Serveur d'exploration sur le chêne en Belgique

Attention, ce site est en cours de développement !
Attention, site généré par des moyens informatiques à partir de corpus bruts.
Les informations ne sont donc pas validées.

Climate, flora and fauna changes in the Sahara over the past 500 million years

Identifieur interne : 000827 ( Istex/Corpus ); précédent : 000826; suivant : 000828

Climate, flora and fauna changes in the Sahara over the past 500 million years

Auteurs : Henry N. Le Houérou

Source :

RBID : ISTEX:D5A385F35E5DB42BC9497438209D9A6F0812DF62

English descriptors

Abstract

The present-day Sahara occupies an area of slightly over 8 million km2in Africa, between latitudes 16 and 32° N, circumscribed within the isohyet of 100 ± 50mm mean annual rainfall. The hyperarid area alternately expanded and shrank on both sides of a seemingly narrow semi-permanent eremitic zone along the Tropic of Cancer during the course of the Quaternary epoch (1·7Ma). The Cenozoic, Mesozoı̈c and Paleozoı̈c Sahara, in turn, has undergone drastic climatic changes as the African continent drifted northward from its Antartic position to reach its present latitudinal situation. But, seemingly the Sahara was never the large desert it now is, with the exception perhaps of the Upper Triassic Lower Liassic epochs. The Pleistocene and Holocene contrasting climate changes induced large variations in flora and fauna distribution, as well as in geomorphic processes. The flora shifted from that of typical desert to tropical savanna and Mediterranean forest or steppe, depending on period and location. Fauna, in turn, changed more in abundance than in nature, since the same groups have been in existence since the Upper Pliocene–Lower Pleistocene. Large mammals, for instance, were mainly of Afro-tropical kinship throughout the Pleistocene and Holocene, while small mammals, in contrast, were predominantly of Mediterranean origin over the same periods. And such is still the case. There were varying large degrees in density of occurrence, but relatively minor fluctuations in nature, in response to such environmental changes as lake and dune expansion and retreat, and even glacier expansion and melting at higher elevations. The present-day man-made expansion of desertic conditions to the north and south actually threaten both flora and fauna alike in the short- and medium-term. Most African large mammals, still present in the desert until the second half of the 19th century, have now become extinct, or are on the very verge of extinction in the Sahara (some may be surviving further south, and/or in the East Africa's parks network). The situation, however, is far less dramatic for the flora, which still includes almost 3000 species of vascular plants, although some species — of economic value or not — are in danger from the man-made destruction of their habitat.

Url:
DOI: 10.1006/jare.1997.0315

Links to Exploration step

ISTEX:D5A385F35E5DB42BC9497438209D9A6F0812DF62

Le document en format XML

<record>
<TEI wicri:istexFullTextTei="biblStruct">
<teiHeader>
<fileDesc>
<titleStmt>
<title xml:lang="en">Climate, flora and fauna changes in the Sahara over the past 500 million years</title>
<author>
<name sortKey="Le Houerou, Henry N" sort="Le Houerou, Henry N" uniqKey="Le Houerou H" first="Henry N." last="Le Houérou">Henry N. Le Houérou</name>
<affiliation>
<mods:affiliation>327, rue de Jussieu, F-34090, Montpellier, France</mods:affiliation>
</affiliation>
</author>
</titleStmt>
<publicationStmt>
<idno type="wicri:source">ISTEX</idno>
<idno type="RBID">ISTEX:D5A385F35E5DB42BC9497438209D9A6F0812DF62</idno>
<date when="1997" year="1997">1997</date>
<idno type="doi">10.1006/jare.1997.0315</idno>
<idno type="url">https://api.istex.fr/document/D5A385F35E5DB42BC9497438209D9A6F0812DF62/fulltext/pdf</idno>
<idno type="wicri:Area/Istex/Corpus">000827</idno>
<idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000827</idno>
</publicationStmt>
<sourceDesc>
<biblStruct>
<analytic>
<title level="a" type="main" xml:lang="en">Climate, flora and fauna changes in the Sahara over the past 500 million years</title>
<author>
<name sortKey="Le Houerou, Henry N" sort="Le Houerou, Henry N" uniqKey="Le Houerou H" first="Henry N." last="Le Houérou">Henry N. Le Houérou</name>
<affiliation>
<mods:affiliation>327, rue de Jussieu, F-34090, Montpellier, France</mods:affiliation>
</affiliation>
</author>
</analytic>
<monogr></monogr>
<series>
<title level="j">Journal of Arid Environments</title>
<title level="j" type="abbrev">YJARE</title>
<idno type="ISSN">0140-1963</idno>
<imprint>
<publisher>ELSEVIER</publisher>
<date type="published" when="1997">1997</date>
<biblScope unit="volume">37</biblScope>
<biblScope unit="issue">4</biblScope>
<biblScope unit="page" from="619">619</biblScope>
<biblScope unit="page" to="647">647</biblScope>
</imprint>
<idno type="ISSN">0140-1963</idno>
</series>
<idno type="istex">D5A385F35E5DB42BC9497438209D9A6F0812DF62</idno>
<idno type="DOI">10.1006/jare.1997.0315</idno>
<idno type="PII">S0140-1963(97)90315-3</idno>
</biblStruct>
</sourceDesc>
<seriesStmt>
<idno type="ISSN">0140-1963</idno>
</seriesStmt>
</fileDesc>
<profileDesc>
<textClass>
<keywords scheme="KwdEn" xml:lang="en">
<term>Sahara</term>
<term>biodiversity</term>
<term>biogeography</term>
<term>climate change</term>
<term>desert</term>
<term>desertification</term>
<term>fauna</term>
<term>flora</term>
<term>natural resources</term>
</keywords>
</textClass>
<langUsage>
<language ident="en">en</language>
</langUsage>
</profileDesc>
</teiHeader>
<front>
<div type="abstract" xml:lang="en">The present-day Sahara occupies an area of slightly over 8 million km2in Africa, between latitudes 16 and 32° N, circumscribed within the isohyet of 100 ± 50mm mean annual rainfall. The hyperarid area alternately expanded and shrank on both sides of a seemingly narrow semi-permanent eremitic zone along the Tropic of Cancer during the course of the Quaternary epoch (1·7Ma). The Cenozoic, Mesozoı̈c and Paleozoı̈c Sahara, in turn, has undergone drastic climatic changes as the African continent drifted northward from its Antartic position to reach its present latitudinal situation. But, seemingly the Sahara was never the large desert it now is, with the exception perhaps of the Upper Triassic Lower Liassic epochs. The Pleistocene and Holocene contrasting climate changes induced large variations in flora and fauna distribution, as well as in geomorphic processes. The flora shifted from that of typical desert to tropical savanna and Mediterranean forest or steppe, depending on period and location. Fauna, in turn, changed more in abundance than in nature, since the same groups have been in existence since the Upper Pliocene–Lower Pleistocene. Large mammals, for instance, were mainly of Afro-tropical kinship throughout the Pleistocene and Holocene, while small mammals, in contrast, were predominantly of Mediterranean origin over the same periods. And such is still the case. There were varying large degrees in density of occurrence, but relatively minor fluctuations in nature, in response to such environmental changes as lake and dune expansion and retreat, and even glacier expansion and melting at higher elevations. The present-day man-made expansion of desertic conditions to the north and south actually threaten both flora and fauna alike in the short- and medium-term. Most African large mammals, still present in the desert until the second half of the 19th century, have now become extinct, or are on the very verge of extinction in the Sahara (some may be surviving further south, and/or in the East Africa's parks network). The situation, however, is far less dramatic for the flora, which still includes almost 3000 species of vascular plants, although some species — of economic value or not — are in danger from the man-made destruction of their habitat.</div>
</front>
</TEI>
<istex>
<corpusName>elsevier</corpusName>
<author>
<json:item>
<name>Henry N. Le Houérou</name>
<affiliations>
<json:string>327, rue de Jussieu, F-34090, Montpellier, France</json:string>
</affiliations>
</json:item>
</author>
<subject>
<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>Sahara</value>
</json:item>
<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>desert</value>
</json:item>
<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>climate change</value>
</json:item>
<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>biogeography</value>
</json:item>
<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>flora</value>
</json:item>
<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>fauna</value>
</json:item>
<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>natural resources</value>
</json:item>
<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>biodiversity</value>
</json:item>
<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>desertification</value>
</json:item>
</subject>
<language>
<json:string>eng</json:string>
</language>
<originalGenre>
<json:string>Full-length article</json:string>
</originalGenre>
<abstract>The present-day Sahara occupies an area of slightly over 8 million km2in Africa, between latitudes 16 and 32° N, circumscribed within the isohyet of 100 ± 50mm mean annual rainfall. The hyperarid area alternately expanded and shrank on both sides of a seemingly narrow semi-permanent eremitic zone along the Tropic of Cancer during the course of the Quaternary epoch (1·7Ma). The Cenozoic, Mesozoı̈c and Paleozoı̈c Sahara, in turn, has undergone drastic climatic changes as the African continent drifted northward from its Antartic position to reach its present latitudinal situation. But, seemingly the Sahara was never the large desert it now is, with the exception perhaps of the Upper Triassic Lower Liassic epochs. The Pleistocene and Holocene contrasting climate changes induced large variations in flora and fauna distribution, as well as in geomorphic processes. The flora shifted from that of typical desert to tropical savanna and Mediterranean forest or steppe, depending on period and location. Fauna, in turn, changed more in abundance than in nature, since the same groups have been in existence since the Upper Pliocene–Lower Pleistocene. Large mammals, for instance, were mainly of Afro-tropical kinship throughout the Pleistocene and Holocene, while small mammals, in contrast, were predominantly of Mediterranean origin over the same periods. And such is still the case. There were varying large degrees in density of occurrence, but relatively minor fluctuations in nature, in response to such environmental changes as lake and dune expansion and retreat, and even glacier expansion and melting at higher elevations. The present-day man-made expansion of desertic conditions to the north and south actually threaten both flora and fauna alike in the short- and medium-term. Most African large mammals, still present in the desert until the second half of the 19th century, have now become extinct, or are on the very verge of extinction in the Sahara (some may be surviving further south, and/or in the East Africa's parks network). The situation, however, is far less dramatic for the flora, which still includes almost 3000 species of vascular plants, although some species — of economic value or not — are in danger from the man-made destruction of their habitat.</abstract>
<qualityIndicators>
<score>8</score>
<pdfVersion>1.2</pdfVersion>
<pdfPageSize>595 x 842 pts (A4)</pdfPageSize>
<refBibsNative>true</refBibsNative>
<keywordCount>9</keywordCount>
<abstractCharCount>2285</abstractCharCount>
<pdfWordCount>10900</pdfWordCount>
<pdfCharCount>70460</pdfCharCount>
<pdfPageCount>29</pdfPageCount>
<abstractWordCount>356</abstractWordCount>
</qualityIndicators>
<title>Climate, flora and fauna changes in the Sahara over the past 500 million years</title>
<pii>
<json:string>S0140-1963(97)90315-3</json:string>
</pii>
<refBibs>
<json:item>
<host>
<author></author>
<title>Préhistoire de l’Afrique</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>C. Arambourg</name>
</json:item>
</author>
<host>
<volume>19</volume>
<pages>
<last>203</last>
<first>195</first>
</pages>
<author></author>
<title>Bulletin de la Société Géologique de France</title>
</host>
<title>Les gisements de vertébrés villafranchiens de l’Afrique du Nord</title>
</json:item>
<json:item>
<host>
<author></author>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>C. Arambourg</name>
</json:item>
<json:item>
<name>R. Coque</name>
</json:item>
</author>
<host>
<volume>8</volume>
<pages>
<last>614</last>
<first>607</first>
</pages>
<author></author>
<title>Bulletin de la Société Géologique de France</title>
</host>
<title>Le gisement Villafranchien de l’Aı̈n Brimba et sa faune</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Préhistoire de l’Afrique du Nord</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Flore de Mauritanie</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Paléobotanique Saharienne</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>A.L. Berger</name>
</json:item>
</author>
<host>
<volume>9</volume>
<pages>
<last>167</last>
<first>139</first>
</pages>
<author></author>
<title>Quaternary Research</title>
</host>
<title>Long term variation of calorific insolation resulting from the earth’s orbital elements</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Climatic Variation and Variability</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Milankovitch and Climate</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Théorie Astronomique des Pluviaux et Interpluviaux du Quaternaire Africain</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>E. Bernard</name>
</json:item>
</author>
<host>
<volume>76</volume>
<pages>
<last>33</last>
<first>13</first>
</pages>
<author></author>
<title>Bulletin ASEQUA,Dakar</title>
</host>
<title>Les problèmes du Quaternaire africain vus par la théorie astronomique des climats</title>
</json:item>
<json:item>
<author>
<json:item>
<name>F. Bernard</name>
</json:item>
</author>
<host>
<volume>1</volume>
<pages>
<last>39</last>
<first>29</first>
</pages>
<author></author>
<title>Travaux de l’Institut de Recherches Sahariennes</title>
</host>
<title>Rôle des insectes sociaux dans les terrains du Sahara</title>
</json:item>
<json:item>
<host>
<author></author>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Les grès du Paléozoı̈que inférieur du Sahara. Sédimentation et discontinuités. Evolution structurale d’un craton</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Le Cadre Paléogéographique de la Préhistoire du Maroc Atlantique</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Le Patrimoine Végétal des Provinces Sahariennes du Marco</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>A. Blytt</name>
</json:item>
</author>
<host>
<volume>21</volume>
<pages>
<last>362</last>
<first>279</first>
</pages>
<author></author>
<title>Nyt Magazin fur Naturvidonskapene</title>
</host>
<title>Forsøg til en theorie om indrandringen af Norges: Flora under vekslende regnfulde øg tørre tider</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Essay on the Immigration of Norwegian Flora</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Theorien om dem norske floras invandring under vesklende tørre øg fugtige perioder</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>G. Boudet</name>
</json:item>
</author>
<host>
<volume>12</volume>
<pages>
<last>524</last>
<first>505</first>
</pages>
<author></author>
<title>Adansonia</title>
</host>
<title>Désertification de l’Afrique tropicale sèche</title>
</json:item>
<json:item>
<host>
<author></author>
<title>The Mediterranean element in the floras of Egypt</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Flora of Egypt Checklist</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>T. Broecker</name>
</json:item>
<json:item>
<name>G. Denton</name>
</json:item>
</author>
<host>
<volume>149</volume>
<pages>
<last>71</last>
<first>62</first>
</pages>
<author></author>
<title>Scientific American</title>
</host>
<title>Les cycles glaciaires. Pour la Science</title>
</json:item>
<json:item>
<author>
<json:item>
<name>A. Brun</name>
</json:item>
</author>
<host>
<volume>1</volume>
<pages>
<last>264</last>
<first>247</first>
</pages>
<author></author>
<title>Géologie Méditerrannéenne: ‘La Mer Pélagienne’</title>
</host>
<title>Recherches palynologiques sur les sédiments du Golfe de Gabès. Résultats préliminaires</title>
</json:item>
<json:item>
<author>
<json:item>
<name>A. Brun</name>
</json:item>
</author>
<host>
<volume>25</volume>
<pages>
<last>460</last>
<first>437</first>
</pages>
<author></author>
<title>Pollen & Spores</title>
</host>
<title>Etudes palynologiques des sédiments marins Holocènes de 5 000 B.P. à l’actuel dans le Golfe de Gabès (Mer Pélagienne)</title>
</json:item>
<json:item>
<author>
<json:item>
<name>A. Brun</name>
</json:item>
</author>
<host>
<author></author>
<title>Comptes Rendus Actes du Colloque sur la Palynologie Archéologique</title>
</host>
<title>Apport de la palynologie à l’histoire du peuplement en Tunisie</title>
</json:item>
<json:item>
<author>
<json:item>
<name>A. Brun</name>
</json:item>
</author>
<host>
<volume>1987-1</volume>
<pages>
<last>25</last>
<first>19</first>
</pages>
<author></author>
<title>Bulletin de l’Association Française pour l’Etude du Quaternaire</title>
</host>
<title>Etude palynologique des limons organiques du site de l’oued el Akarit (Sud Tunisien)</title>
</json:item>
<json:item>
<author>
<json:item>
<name>A. Brun</name>
</json:item>
</author>
<host>
<volume>1</volume>
<pages>
<last>33</last>
<first>25</first>
</pages>
<author></author>
<title>Bulletin de la Société Géologique de France</title>
</host>
<title>Micoflores et paléovégétations en Afrique du Nord depuis 30 000 ans</title>
</json:item>
<json:item>
<author>
<json:item>
<name>A. Brun</name>
</json:item>
<json:item>
<name>M. Rouvillois-Brigol</name>
</json:item>
</author>
<host>
<author></author>
<title>Actes du Colloque sur la Palynologie Archéologique</title>
</host>
<title>Apport de la palynologie à l’histoire du peuplement en Tunisie</title>
</json:item>
<json:item>
<author>
<json:item>
<name>Ph Bruneau de Miré</name>
</json:item>
<json:item>
<name>H. Gillet</name>
</json:item>
</author>
<host>
<volume>111</volume>
<pages>
<last>247</last>
<first>221</first>
</pages>
<author></author>
<title>Journal d’Agriculture Tropicale et de Botanique Appliquée</title>
</host>
<title>Contribution à l’étude de la flore du Massif de l’Aı̈r</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Le Mésozoı̈que Saharien. I : L’Extrême-Sud tunisien</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Le Mézozoı̈que saharien. II Essai de synthèse des données des sondages algéro-tunisiens</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>G. Busson</name>
</json:item>
</author>
<host>
<volume>26</volume>
<pages>
<last>442</last>
<first>1</first>
</pages>
<author></author>
<title>Memoires du Museum National d’Histoire naturelle, Nouvelle série, Sciences de la Terre</title>
</host>
<title>Principes, méthodes et résultats d’une étude statigraphique du Mésozoı̈que saharien</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Climatic changes in the arid zones of Africa during early to mid-Holocene times</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>K.W. Butzer</name>
</json:item>
<json:item>
<name>G.L. Isaac</name>
</json:item>
<json:item>
<name>J.L. Richardson</name>
</json:item>
<json:item>
<name>C. Washbourn-Kamau</name>
</json:item>
</author>
<host>
<volume>175</volume>
<pages>
<last>1076</last>
<first>1069</first>
</pages>
<author></author>
<title>Science</title>
</host>
<title>Radiocarbon dating of East African lake levels</title>
</json:item>
<json:item>
<author>
<json:item>
<name>Y. Callot</name>
</json:item>
</author>
<host>
<volume>299</volume>
<pages>
<last>1350</last>
<first>1347</first>
</pages>
<author></author>
<title>Comptes Rendus de l’Académie des Sciences de Paris</title>
</host>
<title>Dépôts lacustres et palustres quaternaires de la bordure nord du grand erg Occidental: (Algérie)</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Géomorphologie et Paléoenvironnements de l’Atlas Saharien au Grand Erg occidental; dynamique éolienne et Paléolacs Holocènes</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Aux Origines de la Berbérie. Massinissa ou les débuts de l’Histoire</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Les Civilisations préhistoriques de l’Afrique du Nord et du Sahara</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Berbères. Aux marges de l’Histoire</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Le Sahara Français</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>P.J. Casselton</name>
</json:item>
</author>
<host>
<author></author>
<title>Sahara Desert</title>
</host>
<title>Breeding birds</title>
</json:item>
<json:item>
<author>
<json:item>
<name>Ch. Causse</name>
</json:item>
<json:item>
<name>G. Conrad</name>
</json:item>
<json:item>
<name>J.Ch. Fontes</name>
</json:item>
<json:item>
<name>F. Gasse</name>
</json:item>
<json:item>
<name>E. Gibert</name>
</json:item>
<json:item>
<name>A. Kassir</name>
</json:item>
</author>
<host>
<volume>306</volume>
<pages>
<last>1464</last>
<first>1459</first>
</pages>
<author></author>
<title>Comptes Rendus de l’Académie des Sciences de Paris</title>
</host>
<title>Le dernier ‘humide’ Pléistocène du Sahara nord-occidental daterait de 80-100 000 ans</title>
</json:item>
<json:item>
<author>
<json:item>
<name>P.C. Chamard</name>
</json:item>
</author>
<host>
<author></author>
<title>La Désertification au Sud du Sahara</title>
</host>
<title>Essai sur les paléoclimats du sud-ouest saharien au Quaternaire récent</title>
</json:item>
<json:item>
<author>
<json:item>
<name>P.C. Chamard</name>
</json:item>
</author>
<host>
<volume>35</volume>
<pages>
<last>243</last>
<first>207</first>
</pages>
<author></author>
<title>Bulletin de l’Institut Fondamental d’Afrique Noire</title>
</host>
<title>Monographie d’une sebkha continentale du sud-ouest saharien: la Sebkha de Chemchane (Adrar de Mauritanie)</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Les Formations Quaternaires du Sahara Nord-occidental</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>G. Choubert</name>
</json:item>
<json:item>
<name>F. Joly</name>
</json:item>
<json:item>
<name>M. Gigout</name>
</json:item>
<json:item>
<name>J. Marçais</name>
</json:item>
<json:item>
<name>J. Margat</name>
</json:item>
<json:item>
<name>R. Raynal</name>
</json:item>
</author>
<host>
<volume>243</volume>
<pages>
<last>506</last>
<first>504</first>
</pages>
<author></author>
<title>Comptes Rendus de l’Académie des Sciences de Paris</title>
</host>
<title>Essai de classification du Quaternaire continental au Maroc</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Biology of Deserts</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Sahara Desert</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>J.L. Cloudsley-Thompson</name>
</json:item>
</author>
<host>
<author></author>
<title>Sahara Desert</title>
</host>
<title>Arachnids</title>
</json:item>
<json:item>
<host>
<author></author>
<title>L’évolution continentale post-hercynienne du Sahara algérien (Saoura, Erg Chech-Tanezrouft, Ahnet-Mouydir)</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>La Tunisie présaharienne, Étude géomorphologique</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Flora e Vegetazione del Fezzan e della Regione di Gât</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>P. Cour</name>
</json:item>
<json:item>
<name>D. Duzer</name>
</json:item>
</author>
<host>
<volume>8</volume>
<pages>
<last>198</last>
<first>175</first>
</pages>
<author></author>
<title>Revue de Géographie Physique et de Géologie Dynamique</title>
</host>
<title>Persistance d’un climat hyper-aride au Sahara Central et Méridional au cours de l’Holocène</title>
</json:item>
<json:item>
<host>
<author></author>
<title>La Vie animale au Sahara</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>J. Dubief</name>
</json:item>
</author>
<host>
<volume>7</volume>
<pages>
<last>189</last>
<first>187</first>
</pages>
<author></author>
<title>Travaux de l’Institut de Recherches Sahariennes</title>
</host>
<title>Alizés, Harmattans et vents étésiens</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Essai sur l’Hydrologie superficielle au Sahara</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Le Climat du Sahara</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Le Climat du Sahara</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>J.C. Duplessy</name>
</json:item>
<json:item>
<name>N. Petit-Maire</name>
</json:item>
<json:item>
<name>J. Guiot</name>
</json:item>
</author>
<host>
<volume>72</volume>
<pages>
<last>12</last>
<first>11</first>
</pages>
<author></author>
<title>Le Courrier du CNRS</title>
</host>
<title>De la forêt au désert</title>
</json:item>
<json:item>
<author>
<json:item>
<name>J.C. Duplessy</name>
</json:item>
<json:item>
<name>J. Guiot</name>
</json:item>
<json:item>
<name>J. Moyes</name>
</json:item>
<json:item>
<name>N. Petit-Maire</name>
</json:item>
</author>
<host>
<volume>72</volume>
<pages>
<last>12</last>
<first>11</first>
</pages>
<author></author>
<title>Le Courrier du CNRS</title>
</host>
<title>Faunes et flores fossiles témoins des climats</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Etude Géologique, Hydrogéologique et Pédologique des Croûtes en Algérie</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>O. Dutour</name>
</json:item>
</author>
<host>
<volume>14</volume>
<pages>
<last>278</last>
<first>267</first>
</pages>
<author></author>
<title>Cahiers de l’ORSTOM, Série Géologie</title>
</host>
<title>Extension saharienne du type anthropologique de Mechta-Afalou</title>
</json:item>
<json:item>
<author>
<json:item>
<name>O. Dutour</name>
</json:item>
</author>
<host>
<volume>5</volume>
<pages>
<last>256</last>
<first>247</first>
</pages>
<author></author>
<title>Bulletin de la Société d’Anthropologie de Paris</title>
</host>
<title>L’homme de Taforalt au Sahara ou le problème de l’extension saharienne des cromagnoı̈des du Maghreb</title>
</json:item>
<json:item>
<author>
<json:item>
<name>P. Elouard</name>
</json:item>
</author>
<host>
<author></author>
<title>La Désertification au Sud du Sahara</title>
</host>
<title>Oscillations climatiques de l’Holocène à nos jours en Mauritanie atlantique et dans la vallée du Sénégal</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Les Plantes Fossiles dans Leurs Raports avec les Végétaux Vivants</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>J. Fabre</name>
</json:item>
<json:item>
<name>N. Petit-Maire</name>
</json:item>
</author>
<host>
<volume>65</volume>
<pages>
<last>148</last>
<first>133</first>
</pages>
<author></author>
<title>Palaeogeography, Palaeoclimatology & Palaeoecology</title>
</host>
<title>Holocene climatic evolution at 22–23°N from two palaeolakes in the Taoudenni area (Northern Mali)</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Introduction à la Géologie du Sahara Algérien. I : La couverture phanérozoı̈que</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>H. Faure</name>
</json:item>
</author>
<host>
<volume>8</volume>
<pages>
<last>175</last>
<first>167</first>
</pages>
<author></author>
<title>Quaternaria</title>
</host>
<title>Evolution des grands lacs sahariens à l’Holocène</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Global change in Africa during the Quaternary: past, present, future</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>J.Ch. Fontes</name>
</json:item>
<json:item>
<name>F. Gasse</name>
</json:item>
</author>
<host>
<volume>70</volume>
<pages>
<last>398</last>
<first>393</first>
</pages>
<author></author>
<title>Palaeogeography, Palaeoclimatology & Palaeoecology</title>
</host>
<title>On the ages of humid Holocene and late Pleistocene phases in Northern Africa. Remarks on ‘Late Quaternary climatic reconstruction for the Maghreb (North Africa)’ by P. Rognon</title>
</json:item>
<json:item>
<author>
<json:item>
<name>J.Ch. Fontes</name>
</json:item>
<json:item>
<name>F. Gasse</name>
</json:item>
<json:item>
<name>Y. Callot</name>
</json:item>
<json:item>
<name>J.C. Plaziat</name>
</json:item>
<json:item>
<name>P. Carbonnel</name>
</json:item>
<json:item>
<name>P.A. Dupeuble</name>
</json:item>
<json:item>
<name>J. Kaczmarska</name>
</json:item>
</author>
<host>
<volume>317</volume>
<pages>
<last>610</last>
<first>608</first>
</pages>
<author></author>
<title>Nature</title>
</host>
<title>Freshwater to marine-like environments from Holocene lakes in Northern Sahara</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Ekade Ektab die felsbilder Fezzans</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Hadschra Maktuba</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Géologie de l’Afrique</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Le Sahara. Géologie, ressources minérales, mise en valeur</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>F. Gasse</name>
</json:item>
<json:item>
<name>R. Téhet</name>
</json:item>
<json:item>
<name>H. Durand</name>
</json:item>
<json:item>
<name>E. Gibert</name>
</json:item>
<json:item>
<name>J.Ch. Fontes</name>
</json:item>
</author>
<host>
<volume>346</volume>
<pages>
<last>146</last>
<first>141</first>
</pages>
<author></author>
<title>Nature</title>
</host>
<title>The arid-humid transition in the Sahara and the Sahel during the last deglaciation</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Le Peuplement Vvégétal du Massif de l’Ennedi (Tchad)</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Water resources in the Arab, Middle East and North Africa</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>M. Gruet</name>
</json:item>
</author>
<host>
<volume>VI-VII</volume>
<pages>
<last>126</last>
<first>79</first>
</pages>
<author></author>
<title>Libyca</title>
</host>
<title>Le gisement d’El Guettar et sa flore</title>
</json:item>
<json:item>
<host>
<author></author>
<title>El Sahara Español</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>P. Guinet</name>
</json:item>
</author>
<host>
<volume>III</volume>
<pages>
<last>96</last>
<first>21</first>
</pages>
<author></author>
<title>Bulletin de la Carte Phytogéographique,(Série A)</title>
</host>
<title>Carte et notice détaillée de la feuille de Béni-Abbès au 1/200.000</title>
</json:item>
<json:item>
<author>
<json:item>
<name>P. Guinet</name>
</json:item>
<json:item>
<name>C. Sauvage</name>
</json:item>
</author>
<host>
<author></author>
<title>Les Hammadas Sud-Marocaines</title>
</host>
<title>Botanique</title>
</json:item>
<json:item>
<author>
<json:item>
<name>R. Guiraud</name>
</json:item>
</author>
<host>
<volume>31</volume>
<pages>
<last>87</last>
<first>85</first>
</pages>
<author></author>
<title>Annales de la Faculté des Sciences de Dakar</title>
</host>
<title>Le Continental Intercalaire en Algérie</title>
</json:item>
<json:item>
<author>
<json:item>
<name>R. Guiraud</name>
</json:item>
</author>
<host>
<volume>7</volume>
<pages>
<last>543</last>
<first>519</first>
</pages>
<author></author>
<title>Journal of African Earth Science</title>
</host>
<title>L’Hydrogéologie de l’Afrique</title>
</json:item>
<json:item>
<author>
<json:item>
<name>R. Guiraud</name>
</json:item>
</author>
<host>
<volume>42</volume>
<pages>
<last>203</last>
<first>157</first>
</pages>
<author></author>
<title>World Map Commission Bulletin</title>
</host>
<title>Review of the Hydrogeology of Africa</title>
</json:item>
<json:item>
<author>
<json:item>
<name>R. Guiraud</name>
</json:item>
<json:item>
<name>Y. Bellion</name>
</json:item>
</author>
<host>
<author></author>
<title>The Oceanic Basins and Margins</title>
</host>
<title>Late Carboniferous to recent geodynamic evolution of the west Gondwanian cratonic, Tethyan margins</title>
</json:item>
<json:item>
<author>
<json:item>
<name>R. Guiraud</name>
</json:item>
<json:item>
<name>B. Ousmane</name>
</json:item>
</author>
<host>
<author></author>
<title>Proceedings of the International Geological Correlation Project 127</title>
</host>
<title>L’Hydrogéologie du Continental Terminal en Afrique</title>
</json:item>
<json:item>
<host>
<author></author>
<title>L’Hydrogéologie de l’Afrique de l’Ouest</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>An Illustrated Guide to the Plants of Erkowit.</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>L. Hebrard</name>
</json:item>
</author>
<host>
<volume>14</volume>
<pages>
<last>227</last>
<first>193</first>
</pages>
<author></author>
<title>Bulletin de l’ASEQUA,</title>
</host>
<title>Un épisode quaternaire en Mauritanie à la fin du Nouakchottien: le Tafolien 4000-2000 ans avant le présent</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Biogéographie des Mammifères et des Oiseaux de l’Afrique du Nord</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Le Sahara avant le Désert</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Land and Water Use Survey in the Kordofan Province of the Republic of Sudan</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>L. Joleaud</name>
</json:item>
</author>
<host>
<volume>26</volume>
<pages>
<last>39</last>
<first>23</first>
</pages>
<author></author>
<title>Bulletin de la Société d’Histoire Naturelle de l’Afrique du Nord</title>
</host>
<title>Gisements de vertébrés quaternaires du Sahara</title>
</json:item>
<json:item>
<author>
<json:item>
<name>M. Kassas</name>
</json:item>
</author>
<host>
<volume>44</volume>
<pages>
<last>194</last>
<first>180</first>
</pages>
<author></author>
<title>Journal of Ecology</title>
</host>
<title>The mist oasis of Erkwit</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Au Hoggar. Mission 1922</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>C. Kilian</name>
</json:item>
</author>
<host>
<volume>191</volume>
<pages>
<last>1138</last>
<first>1137</first>
</pages>
<author></author>
<title>Comptes Rendus de l’Académie des Sciences de Paris</title>
</host>
<title>Un élément de décision pour la controverse relative à la mer intérieure saharienne plio-pléistocène</title>
</json:item>
<json:item>
<author>
<json:item>
<name>C. Kilian</name>
</json:item>
</author>
<host>
<volume>9</volume>
<pages>
<last>111</last>
<first>110</first>
</pages>
<author></author>
<title>Comptes Rendus Sommaires de la Société Géologique de France</title>
</host>
<title>Une variation de climat dans la période historique. Le dessèchement progressif du Sahara depuis l’époque précameline et des Garamantes</title>
</json:item>
<json:item>
<author>
<json:item>
<name>C. Kilian</name>
</json:item>
</author>
<host>
<volume>58</volume>
<pages>
<first>21, .22</first>
</pages>
<author></author>
<title>Chronique des Mines et de la Colonisation</title>
</host>
<title>Esquisse géologique du Sahara français à l’est du 6ème degré de longitude</title>
</json:item>
<json:item>
<author>
<json:item>
<name>J.E. Kutzbach</name>
</json:item>
</author>
<host>
<volume>214</volume>
<pages>
<last>61</last>
<first>59</first>
</pages>
<author></author>
<title>Science</title>
</host>
<title>Monsoon climates of the early Holocene: climate experiment with the earth’s orbital parameters for 9,000 years ago</title>
</json:item>
<json:item>
<author>
<json:item>
<name>J.E. Kutzbach</name>
</json:item>
</author>
<host>
<pages>
<last>268</last>
<first>247</first>
</pages>
<author></author>
<title>Monsoons,</title>
</host>
<title>The changing pulse of the monsoon</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Climate: past, present, future</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>M.R.K. Lambert</name>
</json:item>
</author>
<host>
<author></author>
<title>Sahara Desert</title>
</host>
<title>Amphibians and reptiles</title>
</json:item>
<json:item>
<author>
<json:item>
<name>J. Lang</name>
</json:item>
<json:item>
<name>C. Kogbe</name>
</json:item>
<json:item>
<name>S. Alidou</name>
</json:item>
<json:item>
<name>K.A. Alzouma</name>
</json:item>
<json:item>
<name>G. Bellion</name>
</json:item>
<json:item>
<name>D. Dubois</name>
</json:item>
<json:item>
<name>A. Durand</name>
</json:item>
<json:item>
<name>R. Guiraud</name>
</json:item>
<json:item>
<name>A. Houessou</name>
</json:item>
<json:item>
<name>F. De Klasz</name>
</json:item>
<json:item>
<name>E. Romann</name>
</json:item>
<json:item>
<name>M. Salard-Cheboldaeff</name>
</json:item>
<json:item>
<name>J. Trichet</name>
</json:item>
</author>
<host>
<volume>10</volume>
<pages>
<last>99</last>
<first>79</first>
</pages>
<author></author>
<title>Journal of African Earth Sciences</title>
</host>
<title>The continental terminal in West Africa</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Les Vertébrés du Sahara</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Faune du Sahara, Vol. I: poissons, amphibiens et reptiles; Vol. II: Mammifères</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Eléments pour un Atlas des Plantes Vasculaires de l ’Afrique Ssèche,Vol. I</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>J.Ph. Lefranc</name>
</json:item>
<json:item>
<name>R. Guiraud</name>
</json:item>
</author>
<host>
<volume>10</volume>
<pages>
<last>77</last>
<first>27</first>
</pages>
<author></author>
<title>Journal of African Earth Sciences</title>
</host>
<title>The Continental Intercalaire of Northwestern Sahara and its equivalents in the neighbouring regions</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Recherche Écologiques et Floristiques sur la Végétation de la Tunisie Méridionale</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Etude préliminaire sur la compatibilité des flores nord-africaine et palestinienne</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>H.N. Le Houérou</name>
</json:item>
</author>
<host>
<author></author>
<title>Hot Deserts and Arid Shrublands,Vol. B</title>
</host>
<title>The desert and arid zones of Northern Africa</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Considérations biogéographiques sur les steppes nord-africaines. Comptes Rendus du Colloque International de l’Association Française de Géographie Physique: Biogéographie, Environnement et Aménagement</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>H.N. Le Houérou</name>
</json:item>
</author>
<host>
<volume>1,2</volume>
<pages>
<last>259</last>
<first>246</first>
</pages>
<author></author>
<title>Sècheresse</title>
</host>
<title>Le Sahara du point de vue bioclimatique: définitions et limites</title>
</json:item>
<json:item>
<author>
<json:item>
<name>H.N. Le Houérou</name>
</json:item>
</author>
<host>
<volume>XV</volume>
<pages>
<last>144</last>
<first>95</first>
</pages>
<author></author>
<title>Comptes Rendus de la Conférence Internationale sur la Désertisation</title>
</host>
<title>Classification écoclimatique des zones arides (s.1.) de l’Afrique du Nord. 80 pp</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Recherches Écoclimatiques et Biogéographiques sur les Zones Arides (s.l.) de l’Afrique du Nord</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>H.N. Le Houérou</name>
</json:item>
</author>
<host>
<volume>22</volume>
<pages>
<last>30</last>
<first>3</first>
</pages>
<author></author>
<title>Journal of Arid Environments</title>
</host>
<title>Outline of the biological history of the Sahara</title>
</json:item>
<json:item>
<author>
<json:item>
<name>H.N. Le Houérou</name>
</json:item>
</author>
<host>
<volume>10</volume>
<pages>
<last>396</last>
<first>1</first>
</pages>
<author></author>
<title>Options méditerranéennes, B</title>
</host>
<title>Bioclimatologie et biogéographie des steppes arides du nord de l’Afrique</title>
</json:item>
<json:item>
<author>
<json:item>
<name>H.N. Le Houérou</name>
</json:item>
</author>
<host>
<volume>4(1)</volume>
<pages>
<last>16</last>
<first>1</first>
</pages>
<author></author>
<title>Annals of Ar. Zone</title>
</host>
<title>The Sahara from the bioclimatic viewpoint: definition and limits</title>
</json:item>
<json:item>
<author>
<json:item>
<name>H.N. Le Houérou</name>
</json:item>
<json:item>
<name>H. Gillet</name>
</json:item>
</author>
<host>
<author></author>
<title>Conservation Biology: the science of scarcity and diversity</title>
</host>
<title>Conservation vs desertization in African Arid Lands</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Agro-Bioclimatic Classification of Africa.Agrometorology series, no 6</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Etude étologique et phytogéographique du Tassili N’Ajjer</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>A. Leroi-Gourhan</name>
</json:item>
</author>
<host>
<volume>55</volume>
<pages>
<first>9</first>
</pages>
<author></author>
<title>Bulletin de la Société de Préhistoire de France</title>
</host>
<title>Résultats de l’analyse pollinique du gisement d’El Guettar, Tunisie</title>
</json:item>
<json:item>
<author>
<json:item>
<name>M. Leroux</name>
</json:item>
</author>
<host>
<author></author>
<title>La Désertification au Sud du Sahara</title>
</host>
<title>La circulation atmosphérique générale et les oscillations climatiques tropicales</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Le Climat de l’Afrique Tropicale</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>A la Découverte des Fresques du Tassili</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>W.F. Libby</name>
</json:item>
<json:item>
<name>E.C. Anderson</name>
</json:item>
<json:item>
<name>J.R. Arnold</name>
</json:item>
</author>
<host>
<volume>109</volume>
<pages>
<first>227</first>
</pages>
<author></author>
<title>Science</title>
</host>
<title>Age determination by radiocarbon</title>
</json:item>
<json:item>
<author>
<json:item>
<name>C. Lorius</name>
</json:item>
</author>
<host>
<volume>72</volume>
<pages>
<last>13</last>
<first>12</first>
</pages>
<author></author>
<title>Le Courrier du CNRS</title>
</host>
<title>Les archives glaciaires</title>
</json:item>
<json:item>
<author>
<json:item>
<name>C. Lorius</name>
</json:item>
<json:item>
<name>J. Jouzel</name>
</json:item>
<json:item>
<name>C. Ritz</name>
</json:item>
<json:item>
<name>T. Merlivat</name>
</json:item>
<json:item>
<name>N. Barkov</name>
</json:item>
<json:item>
<name>Y. Kootkevich</name>
</json:item>
<json:item>
<name>V. Kolyatkov</name>
</json:item>
</author>
<host>
<volume>316</volume>
<pages>
<last>596</last>
<first>591</first>
</pages>
<author></author>
<title>Nature</title>
</host>
<title>A 150,000 years climatic record from Antartic ice</title>
</json:item>
<json:item>
<author>
<json:item>
<name>J.F. McCauley</name>
</json:item>
<json:item>
<name>G.G. Shaber</name>
</json:item>
<json:item>
<name>C.S. Breed</name>
</json:item>
<json:item>
<name>M.J. Grolier</name>
</json:item>
<json:item>
<name>C.V. Haynes</name>
</json:item>
<json:item>
<name>B. Issawi</name>
</json:item>
<json:item>
<name>C. Elachi</name>
</json:item>
<json:item>
<name>R. Blom</name>
</json:item>
</author>
<host>
<volume>218</volume>
<pages>
<last>1020</last>
<first>1004</first>
</pages>
<author></author>
<title>Science</title>
</host>
<title>Subsurface valleys and geoarchaeology of the Eastern Sahara revealed by shuttle radar</title>
</json:item>
<json:item>
<author>
<json:item>
<name>J.F. McCauley</name>
</json:item>
<json:item>
<name>C.S. Breed</name>
</json:item>
<json:item>
<name>G.G. Shaber</name>
</json:item>
<json:item>
<name>W.P. McHugh</name>
</json:item>
<json:item>
<name>B. Issawi</name>
</json:item>
<json:item>
<name>C.V. Haynes</name>
</json:item>
<json:item>
<name>M.J. Grolier</name>
</json:item>
<json:item>
<name>A. El Kilani</name>
</json:item>
</author>
<host>
<volume>GE 4</volume>
<pages>
<last>648</last>
<first>624</first>
</pages>
<author></author>
<title>IEEE Transactions on Geosciences and RemoteSensing</title>
</host>
<title>Palaeodrainages of the Eastern Sahara—the radar rivers revisited (Sir-Alb Implications for a mid-Tertiary trans-African drainage system)</title>
</json:item>
<json:item>
<author>
<json:item>
<name>M. Mainguet</name>
</json:item>
</author>
<host>
<volume>20</volume>
<pages>
<last>296</last>
<first>275</first>
</pages>
<author></author>
<title>Zonal Geomorphologie, N.F.</title>
</host>
<title>Propositions pour une nouvelle classification des édifices sableux éoliens d’après les images satellites Lansat, Gemini et NOAA 3</title>
</json:item>
<json:item>
<author>
<json:item>
<name>M. Mainguet</name>
</json:item>
</author>
<host>
<volume>56</volume>
<pages>
<last>92</last>
<first>79</first>
</pages>
<author></author>
<title>Würtzburger Geographische Arbeiten</title>
</host>
<title>Les dunes d’érosion: signification morphodynamique et climatique de leur existence</title>
</json:item>
<json:item>
<author>
<json:item>
<name>M. Mainguet</name>
</json:item>
</author>
<host>
<volume>Bd.45</volume>
<pages>
<last>285</last>
<first>265</first>
</pages>
<author></author>
<title>Zonal Geomorphologie(N.F.Suppl.)</title>
</host>
<title>Dunes vives, dunes fixées, dune vêtues: une dassification selon le bilan d’alimentation, le régime éolien et la dynamique des édifices sableux</title>
</json:item>
<json:item>
<author>
<json:item>
<name>M. Mainguet</name>
</json:item>
</author>
<host>
<author></author>
<title>Deserts and Arid Lands</title>
</host>
<title>A dassification of dunes based on aeolian dynamics and the sand budget</title>
</json:item>
<json:item>
<author>
<json:item>
<name>J. Maley</name>
</json:item>
</author>
<host>
<volume>14</volume>
<pages>
<last>227</last>
<first>193</first>
</pages>
<author></author>
<title>Palaeogeography, Palaeoclimatology, Palaeoecology</title>
</host>
<title>Mécanismes des changements climatiques aux basses latitudes</title>
</json:item>
<json:item>
<author>
<json:item>
<name>J. Maley</name>
</json:item>
</author>
<host>
<author></author>
<title>The Sahara and the Nile</title>
</host>
<title>Les changements climatiques de la fin du Tertiaire en Afrique: leurs conséquences sur l’apparition du Sahara et de sa végétation</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Etudes Palynologiques dans le Bassin du Lac Tchad et Paléoclimatologie de l’Afrique Nord-tropicale de 30 000 Ans à l’Époque Actuelle</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>J. Mangerud</name>
</json:item>
<json:item>
<name>S.T. Andersen</name>
</json:item>
<json:item>
<name>B.E. Berglund</name>
</json:item>
<json:item>
<name>J.J. Donner</name>
</json:item>
</author>
<host>
<volume>3</volume>
<pages>
<last>128</last>
<first>109</first>
</pages>
<author></author>
<title>Boreas</title>
</host>
<title>Quaternary stratigraphy of Norden, a proposed for terminology and classification</title>
</json:item>
<json:item>
<host>
<author></author>
<title>L’eau dans le Bassin Méditerranéen: situation et prospective</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>J. Mathez</name>
</json:item>
<json:item>
<name>Ch. Sauvage</name>
</json:item>
</author>
<host>
<pages>
<first>117.195, 253, 257</first>
</pages>
<author></author>
<title>Travaux de l’Institut Scientifique Chérifien et de la Faculté des Sciences de Rabat,Série Générale no. 3,</title>
</host>
<title>Catalogue des végétaux vasculaires de la province de Tarfaya</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Les Bassins des Fleuves Sénégal et Gambie, Etude Géomorphologique</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>M. Milankovitch</name>
</json:item>
</author>
<host>
<author></author>
<title>Handbuch der Klimatologie</title>
</host>
<title>Mathematische klimalehre und astronomische theorie der klima- schwankungen</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Kanon der erbstrahlung und seine anwendung auf das eiszeitenproblem</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Méhavées</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Phanérogames</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Majabat al Koubrâ. Contribution à l’étude de l’ “Empty Quarter” ouest saharien</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Les Déserts</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Tadrart Acacus. Arte rupestre e culture del Sahara preistorico</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>K. Neuman</name>
</json:item>
</author>
<host>
<volume>18</volume>
<pages>
<last>188</last>
<first>179</first>
</pages>
<author></author>
<title>Palaeoecology of Africa</title>
</host>
<title>Middle Holocene vegetation of the Gilf Kebir, SW Egypt a reconstruction</title>
</json:item>
<json:item>
<author>
<json:item>
<name>K. Neuman</name>
</json:item>
<json:item>
<name>E. Schulz</name>
</json:item>
</author>
<host>
<volume>18</volume>
<pages>
<last>166</last>
<first>163</first>
</pages>
<author></author>
<title>Palaeoecology of Africa</title>
</host>
<title>Middle Holocene savanna vegetation in the Central Sahara. Preliminary report</title>
</json:item>
<json:item>
<author>
<json:item>
<name>H.J. Pachur</name>
</json:item>
<json:item>
<name>S. Krëpelin</name>
</json:item>
</author>
<host>
<volume>237</volume>
<pages>
<last>300</last>
<first>298</first>
</pages>
<author></author>
<title>Science</title>
</host>
<title>Wadi Howar: palaeoclimatic evidence from an extinct river system in the South Eastern Sahara</title>
</json:item>
<json:item>
<author>
<json:item>
<name>P. Pallas</name>
</json:item>
</author>
<host>
<author></author>
<title>The Geology of Libya</title>
</host>
<title>Water resources of the Socialist People’s Libyan Jamahiria</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Die Alpen im Eiszeitalter</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Le Sahara Adantique à l’Holocene: peuplement et ecologie</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Le Shati, lac Pléistocene du Fezzan</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>N. Petit-Maire</name>
</json:item>
</author>
<host>
<volume>9</volume>
<pages>
<last>16</last>
<first>7</first>
</pages>
<author></author>
<title>Episodes</title>
</host>
<title>Palaeoclimates in the Sahara of Mali. A multidisciplinary study</title>
</json:item>
<json:item>
<author>
<json:item>
<name>N. Petit-Maire</name>
</json:item>
</author>
<host>
<author></author>
<title>Current Research in African Earth Science</title>
</host>
<title>Local responses to recent climatic change: hyperarid central Sahara and Coastal Sahara</title>
</json:item>
<json:item>
<author>
<json:item>
<name>N. Petit-Maire</name>
</json:item>
</author>
<host>
<author></author>
<title>Paleoclimatology and Paleometeorology: modern and past patterns of global atmospheric transport</title>
</host>
<title>Interglacial environments in presently hyperarid Sahara: paleoclimatic implications</title>
</json:item>
<json:item>
<author>
<json:item>
<name>N. Petit-Maire</name>
</json:item>
</author>
<host>
<author></author>
<title>Palaeoclimatology & Palaeometeorology: modern and past patterns of global atmospheric transport</title>
</host>
<title>Interglacial environments in presently hyperarid Sahara: palaeoclimatic implications</title>
</json:item>
<json:item>
<author>
<json:item>
<name>N. Petit-Maire</name>
</json:item>
<json:item>
<name>O. Dutour</name>
</json:item>
</author>
<host>
<author></author>
<title>Prehistory of Arid North Africa</title>
</host>
<title>Holocene populations of the Western and Southern Sahara: Mechtoı̈ds and Palaeoclimates</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Sahara ou Sahel? Quaternaire récent du Bassin de Taoudennin (Mali)</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>A. Pons</name>
</json:item>
<json:item>
<name>P. Quézel</name>
</json:item>
</author>
<host>
<volume>243</volume>
<pages>
<last>658</last>
<first>656</first>
</pages>
<author></author>
<title>Comptes Rendus de l’Académie des Sciences de Paris</title>
</host>
<title>Premiers résultats de l’analyse palynologique de quelques paléosols sahariens</title>
</json:item>
<json:item>
<author>
<json:item>
<name>A. Pons</name>
</json:item>
<json:item>
<name>P. Quézel</name>
</json:item>
</author>
<host>
<volume>14</volume>
<pages>
<last>40</last>
<first>15</first>
</pages>
<author></author>
<title>Travaux de l’Institut de Recherches Sahariennes</title>
</host>
<title>Première étude palynologique de quelques paléosols sahariens</title>
</json:item>
<json:item>
<author>
<json:item>
<name>A. Pons</name>
</json:item>
<json:item>
<name>P. Quézel</name>
</json:item>
</author>
<host>
<volume>244</volume>
<pages>
<last>90</last>
<first>22</first>
</pages>
<author></author>
<title>Comptes Rendus de l’Académie des Sciences de Paris</title>
</host>
<title>Premières remarques sur l’étude palynologique d’un guano fossile du Hoggar</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Etude Écologique des Biotopes du Criquet PèlerinSchistocerca gregaria</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Contribution à l’Étude de la Flore et de la Végétation du Hoggar</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>P. Quézel</name>
</json:item>
</author>
<host>
<volume>15</volume>
<pages>
<last>57</last>
<first>43</first>
</pages>
<author></author>
<title>Travaux de l’Institut de Recherches Sahariennes</title>
</host>
<title>Les groupements végétaux du massif de la Tefedest</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Mission botanique au Tibesti</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>P. Quézel</name>
</json:item>
</author>
<host>
<volume>22</volume>
<pages>
<last>359</last>
<first>353</first>
</pages>
<author></author>
<title>Bulletin de l’Institut Fondamental d’Afrique Noire</title>
</host>
<title>Flore et palynologie saharienne</title>
</json:item>
<json:item>
<host>
<author></author>
<title>La Végétation du Sahara du Tchad à la Mauritanie</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>P. Quézel</name>
</json:item>
</author>
<host>
<volume>65</volume>
<pages>
<last>534</last>
<first>479</first>
</pages>
<author></author>
<title>Annals of Missouri Botanical Garden</title>
</host>
<title>Analysis of the flora of Mediterranean and Saharan Africa</title>
</json:item>
<json:item>
<author>
<json:item>
<name>P. Quézel</name>
</json:item>
<json:item>
<name>C. Martinez</name>
</json:item>
</author>
<host>
<volume>49</volume>
<pages>
<last>244</last>
<first>230</first>
</pages>
<author></author>
<title>Bulletin de la Société d’Histoire Naturelle de l’Afrique du Nord</title>
</host>
<title>Etude palynologique de deux diatomites du Borkou</title>
</json:item>
<json:item>
<author>
<json:item>
<name>P. Quézel</name>
</json:item>
<json:item>
<name>C. Martinez</name>
</json:item>
</author>
<host>
<volume>6-7</volume>
<pages>
<last>228</last>
<first>211</first>
</pages>
<author></author>
<title>Libyca</title>
</host>
<title>Le dernier interpluvial au Sahara Central. Essai de chronologie palynologique et paléoclimatique</title>
</json:item>
<json:item>
<author>
<json:item>
<name>J.C. Ritchie</name>
</json:item>
<json:item>
<name>C.H. Eyles</name>
</json:item>
<json:item>
<name>C.V. Haynes</name>
</json:item>
</author>
<host>
<volume>314</volume>
<pages>
<last>355</last>
<first>352</first>
</pages>
<author></author>
<title>Nature</title>
</host>
<title>Sediment and pollen evidence for an early to mid-Holocene humid period in the Eastern Sahara</title>
</json:item>
<json:item>
<author>
<json:item>
<name>H. Rodhenburg</name>
</json:item>
<json:item>
<name>H. Sabelberg</name>
</json:item>
</author>
<host>
<author></author>
<title>Palaeoecology of Africa and the Surrounding Islands</title>
</host>
<title>Northwestern Sahara margin: terrestrial stratigraphy of the upper Quaternary and some palaeoclimatic implications</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Le Massif de l’Atakor et ses Bordures (Sahara Central)</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>P. Rognon</name>
</json:item>
</author>
<host>
<volume>18</volume>
<pages>
<last>282</last>
<first>251</first>
</pages>
<author></author>
<title>Revue de Géographie Physique & de Géologie Dynamique</title>
</host>
<title>Essai d’interprétation climatique au sahara depuis 40 000 ans</title>
</json:item>
<json:item>
<author>
<json:item>
<name>P. Rognon</name>
</json:item>
</author>
<host>
<volume>18</volume>
<pages>
<last>156</last>
<first>147</first>
</pages>
<author></author>
<title>Revue de Géographie Physique et de Géologie Dynamique</title>
</host>
<title>Les oscillations du climat saharien depuis 40 millénaires. Introduction à un vieux débat</title>
</json:item>
<json:item>
<author>
<json:item>
<name>P. Rognon</name>
</json:item>
</author>
<host>
<volume>22</volume>
<pages>
<last>328</last>
<first>313</first>
</pages>
<author></author>
<title>Revue de Géographie Physique et de Géologie Dynamique</title>
</host>
<title>Une extension des déserts (Sahara et Moyen Orient) au cours du tardiglaciaire (18000-10 000 ans B.P.)</title>
</json:item>
<json:item>
<author>
<json:item>
<name>P. Rognon</name>
</json:item>
</author>
<host>
<volume>1</volume>
<pages>
<last>20</last>
<first>13</first>
</pages>
<author></author>
<title>Bulletin de la Sociëté Géologique de France</title>
</host>
<title>Variations de l’aridité au Sahara depuis 125 000 B.P. en relation avec les ‘contraintes’ orbitales et glaciaires</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Biographie d’un Désert</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>P. Rognon</name>
</json:item>
<json:item>
<name>B. Biju Duval</name>
</json:item>
<json:item>
<name>O. De Charpal</name>
</json:item>
</author>
<host>
<volume>2, XIV, 5</volume>
<pages>
<last>528</last>
<first>507</first>
</pages>
<author></author>
<title>Revue de Geograpie Physique et de Géologie Dynamique</title>
</host>
<title>Modelé glaciaire dans l’Ordovicien supérieur saharien: phases d’érosion et glacio-tectonique sur la bordure des Eglab</title>
</json:item>
<json:item>
<author>
<json:item>
<name>S. Santa</name>
</json:item>
</author>
<host>
<volume>6-7</volume>
<pages>
<last>77</last>
<first>37</first>
</pages>
<author></author>
<title>Libyca</title>
</host>
<title>Essai de reconstitution de paysages végétaux quaternaires d’Afrique du Nord</title>
</json:item>
<json:item>
<author>
<json:item>
<name>M. Sarnthein</name>
</json:item>
</author>
<host>
<volume>272</volume>
<pages>
<last>46</last>
<first>43</first>
</pages>
<author></author>
<title>Nature</title>
</host>
<title>Sand deserts during glacial maximum and climatic optimum</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Die Sahara und ihre Randgebeite</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>E. Schulz</name>
</json:item>
</author>
<host>
<author></author>
<title>Palaeoecology of Africa</title>
</host>
<title>Der Holozäne vegetation der zentralen Sahara</title>
</json:item>
<json:item>
<author>
<json:item>
<name>E. Schulz</name>
</json:item>
</author>
<host>
<volume>69</volume>
<pages>
<last>161</last>
<first>143</first>
</pages>
<author></author>
<title>Würzburger Geographische Arbeiten</title>
</host>
<title>Der sudrand der Sahara</title>
</json:item>
<json:item>
<author>
<json:item>
<name>R. Sernander</name>
</json:item>
</author>
<host>
<volume>30</volume>
<pages>
<last>478</last>
<first>465</first>
</pages>
<author></author>
<title>Geologie Fören</title>
</host>
<title>On the evidence of postglacial changes of climate furnished by the peat mosses of Northern Europe</title>
</json:item>
<json:item>
<author>
<json:item>
<name>R. Sernander</name>
</json:item>
</author>
<host>
<author></author>
<title>Geologie Fören</title>
</host>
<title>Dis schwedischen torf moore als zeugen postglazialer klimmaschankungen</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Séquences continentales et variations climatiques, évolution du bassin du Tchad au Cénozoı̈que Supérieur</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>M. Servant</name>
</json:item>
<json:item>
<name>S. Servant-Vildary</name>
</json:item>
</author>
<host>
<author></author>
<title>The Sahara and the Nile</title>
</host>
<title>L’environnement quaternaire du Bassin du Tchad</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Etude des Diatomées et Paléo-limnologie du Bassin Tchadien au Cénozoı̈que Supérieur</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>R. Stein</name>
</json:item>
<json:item>
<name>M. Sarnthein</name>
</json:item>
</author>
<host>
<volume>16</volume>
<pages>
<last>36</last>
<first>9</first>
</pages>
<author></author>
<title>Palaeoecology of Africa</title>
</host>
<title>Late Neogene events of atmospheric and oceanic circulation offshore North-West Africa. High resolution record from deep sea sediments</title>
</json:item>
<json:item>
<host>
<author></author>
<title>Student’s Flora of Egypt</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Etude des ressources en eau du Sahara septentrional. Algérie-Tunisie</title>
</host>
</json:item>
<json:item>
<host>
<author></author>
<title>Analyse pollinique des dépots würmiens d’El Guettar (Tunisie)</title>
</host>
</json:item>
<json:item>
<author>
<json:item>
<name>M. Van Campo</name>
</json:item>
</author>
<host>
<author></author>
<title>Problems in Prehistory: North Africa and the Levant</title>
</host>
<title>Pollen analysis in the Sahara</title>
</json:item>
<json:item>
<author>
<json:item>
<name>M. Van Campo</name>
</json:item>
<json:item>
<name>R. Coque</name>
</json:item>
</author>
<host>
<volume>11</volume>
<pages>
<last>284</last>
<first>275</first>
</pages>
<author></author>
<title>Pollen & Spores</title>
</host>
<title>Palynologie et géomorphologie dans le Sud tunisien</title>
</json:item>
<json:item>
<author>
<json:item>
<name>W. Van Zeist</name>
</json:item>
<json:item>
<name>S. Bottema</name>
</json:item>
</author>
<host>
<volume>16</volume>
<pages>
<last>69</last>
<first>36</first>
</pages>
<author></author>
<title>Striae</title>
</host>
<title>Reflection on a Holocene subdivision of the Near East. In: Mangerud, J., Birks, H. J. B. & Juger, K. D. (Eds),Chronostratigraphic subdivisions of the Holocene</title>
</json:item>
<json:item>
<author>
<json:item>
<name>B. Van Zinderen Bakker</name>
</json:item>
<json:item>
<name>J. Maley</name>
</json:item>
</author>
<host>
<volume>10-11</volume>
<pages>
<last>104</last>
<first>83</first>
</pages>
<author></author>
<title>Palaeoecology of Africa</title>
</host>
<title>Late Quaternary palaeoenvironments of the Saharan region</title>
</json:item>
<json:item>
<author>
<json:item>
<name>F. Wendorf</name>
</json:item>
<json:item>
<name>A.E. Close</name>
</json:item>
<json:item>
<name>A. Gautier</name>
</json:item>
<json:item>
<name>R. Child</name>
</json:item>
</author>
<host>
<volume>21</volume>
<pages>
<last>445</last>
<first>436</first>
</pages>
<author></author>
<title>La Recherche</title>
</host>
<title>Les débuts du pastoralisme en Egypte</title>
</json:item>
<json:item>
<author>
<json:item>
<name>G.E. Wickens</name>
</json:item>
</author>
<host>
<volume>24 a</volume>
<pages>
<last>65</last>
<first>43</first>
</pages>
<author></author>
<title>Boissiera</title>
</host>
<title>Changes in climate and vegetation of the Sudan since 20,000 B.P</title>
</json:item>
</refBibs>
<genre>
<json:string>research-article</json:string>
</genre>
<host>
<volume>37</volume>
<pii>
<json:string>S0140-1963(00)X0043-2</json:string>
</pii>
<pages>
<last>647</last>
<first>619</first>
</pages>
<issn>
<json:string>0140-1963</json:string>
</issn>
<issue>4</issue>
<genre>
<json:string>journal</json:string>
</genre>
<language>
<json:string>unknown</json:string>
</language>
<title>Journal of Arid Environments</title>
<publicationDate>1997</publicationDate>
</host>
<categories>
<wos>
<json:string>science</json:string>
<json:string>environmental sciences</json:string>
<json:string>ecology</json:string>
</wos>
<scienceMetrix>
<json:string>natural sciences</json:string>
<json:string>biology</json:string>
<json:string>ecology</json:string>
</scienceMetrix>
</categories>
<publicationDate>1997</publicationDate>
<copyrightDate>1997</copyrightDate>
<doi>
<json:string>10.1006/jare.1997.0315</json:string>
</doi>
<id>D5A385F35E5DB42BC9497438209D9A6F0812DF62</id>
<score>1</score>
<fulltext>
<json:item>
<extension>pdf</extension>
<original>true</original>
<mimetype>application/pdf</mimetype>
<uri>https://api.istex.fr/document/D5A385F35E5DB42BC9497438209D9A6F0812DF62/fulltext/pdf</uri>
</json:item>
<json:item>
<extension>zip</extension>
<original>false</original>
<mimetype>application/zip</mimetype>
<uri>https://api.istex.fr/document/D5A385F35E5DB42BC9497438209D9A6F0812DF62/fulltext/zip</uri>
</json:item>
<istex:fulltextTEI uri="https://api.istex.fr/document/D5A385F35E5DB42BC9497438209D9A6F0812DF62/fulltext/tei">
<teiHeader>
<fileDesc>
<titleStmt>
<title level="a" type="main" xml:lang="en">Climate, flora and fauna changes in the Sahara over the past 500 million years</title>
</titleStmt>
<publicationStmt>
<authority>ISTEX</authority>
<publisher>ELSEVIER</publisher>
<availability>
<p>©1997 Academic Press</p>
</availability>
<date>1997</date>
</publicationStmt>
<notesStmt>
<note>Sawyer, J. S.</note>
<note type="content">Section title: Regular Article</note>
</notesStmt>
<sourceDesc>
<biblStruct type="inbook">
<analytic>
<title level="a" type="main" xml:lang="en">Climate, flora and fauna changes in the Sahara over the past 500 million years</title>
<author xml:id="author-1">
<persName>
<forename type="first">Henry N.</forename>
<surname>Le Houérou</surname>
</persName>
<affiliation>327, rue de Jussieu, F-34090, Montpellier, France</affiliation>
</author>
</analytic>
<monogr>
<title level="j">Journal of Arid Environments</title>
<title level="j" type="abbrev">YJARE</title>
<idno type="pISSN">0140-1963</idno>
<idno type="PII">S0140-1963(00)X0043-2</idno>
<imprint>
<publisher>ELSEVIER</publisher>
<date type="published" when="1997"></date>
<biblScope unit="volume">37</biblScope>
<biblScope unit="issue">4</biblScope>
<biblScope unit="page" from="619">619</biblScope>
<biblScope unit="page" to="647">647</biblScope>
</imprint>
</monogr>
<idno type="istex">D5A385F35E5DB42BC9497438209D9A6F0812DF62</idno>
<idno type="DOI">10.1006/jare.1997.0315</idno>
<idno type="PII">S0140-1963(97)90315-3</idno>
</biblStruct>
</sourceDesc>
</fileDesc>
<profileDesc>
<creation>
<date>1997</date>
</creation>
<langUsage>
<language ident="en">en</language>
</langUsage>
<abstract xml:lang="en">
<p>The present-day Sahara occupies an area of slightly over 8 million km2in Africa, between latitudes 16 and 32° N, circumscribed within the isohyet of 100 ± 50mm mean annual rainfall. The hyperarid area alternately expanded and shrank on both sides of a seemingly narrow semi-permanent eremitic zone along the Tropic of Cancer during the course of the Quaternary epoch (1·7Ma). The Cenozoic, Mesozoı̈c and Paleozoı̈c Sahara, in turn, has undergone drastic climatic changes as the African continent drifted northward from its Antartic position to reach its present latitudinal situation. But, seemingly the Sahara was never the large desert it now is, with the exception perhaps of the Upper Triassic Lower Liassic epochs. The Pleistocene and Holocene contrasting climate changes induced large variations in flora and fauna distribution, as well as in geomorphic processes. The flora shifted from that of typical desert to tropical savanna and Mediterranean forest or steppe, depending on period and location. Fauna, in turn, changed more in abundance than in nature, since the same groups have been in existence since the Upper Pliocene–Lower Pleistocene. Large mammals, for instance, were mainly of Afro-tropical kinship throughout the Pleistocene and Holocene, while small mammals, in contrast, were predominantly of Mediterranean origin over the same periods. And such is still the case. There were varying large degrees in density of occurrence, but relatively minor fluctuations in nature, in response to such environmental changes as lake and dune expansion and retreat, and even glacier expansion and melting at higher elevations. The present-day man-made expansion of desertic conditions to the north and south actually threaten both flora and fauna alike in the short- and medium-term. Most African large mammals, still present in the desert until the second half of the 19th century, have now become extinct, or are on the very verge of extinction in the Sahara (some may be surviving further south, and/or in the East Africa's parks network). The situation, however, is far less dramatic for the flora, which still includes almost 3000 species of vascular plants, although some species — of economic value or not — are in danger from the man-made destruction of their habitat.</p>
</abstract>
<textClass xml:lang="en">
<keywords scheme="keyword">
<list>
<head>Keywords</head>
<item>
<term>Sahara</term>
</item>
<item>
<term>desert</term>
</item>
<item>
<term>climate change</term>
</item>
<item>
<term>biogeography</term>
</item>
<item>
<term>flora</term>
</item>
<item>
<term>fauna</term>
</item>
<item>
<term>natural resources</term>
</item>
<item>
<term>biodiversity</term>
</item>
<item>
<term>desertification</term>
</item>
</list>
</keywords>
</textClass>
</profileDesc>
<revisionDesc>
<change when="1997">Published</change>
</revisionDesc>
</teiHeader>
</istex:fulltextTEI>
<json:item>
<extension>txt</extension>
<original>false</original>
<mimetype>text/plain</mimetype>
<uri>https://api.istex.fr/document/D5A385F35E5DB42BC9497438209D9A6F0812DF62/fulltext/txt</uri>
</json:item>
</fulltext>
<metadata>
<istex:metadataXml wicri:clean="Elsevier, elements deleted: tail">
<istex:xmlDeclaration>version="1.0" encoding="utf-8"</istex:xmlDeclaration>
<istex:docType PUBLIC="-//ES//DTD journal article DTD version 4.5.2//EN//XML" URI="art452.dtd" name="istex:docType"></istex:docType>
<istex:document>
<converted-article version="4.5.2" docsubtype="fla" xml:lang="en">
<item-info>
<jid>YJARE</jid>
<aid>90315</aid>
<ce:pii>S0140-1963(97)90315-3</ce:pii>
<ce:doi>10.1006/jare.1997.0315</ce:doi>
<ce:copyright type="full-transfer" year="1997">Academic Press</ce:copyright>
</item-info>
<head>
<ce:article-footnote>
<ce:label></ce:label>
<ce:note-para>Sawyer, J. S.</ce:note-para>
</ce:article-footnote>
<ce:dochead>
<ce:textfn>Regular Article</ce:textfn>
</ce:dochead>
<ce:title>Climate, flora and fauna changes in the Sahara over the past 500 million years</ce:title>
<ce:author-group>
<ce:author>
<ce:given-name>Henry N.</ce:given-name>
<ce:surname>Le Houérou</ce:surname>
</ce:author>
<ce:affiliation>
<ce:textfn>327, rue de Jussieu, F-34090, Montpellier, France</ce:textfn>
</ce:affiliation>
</ce:author-group>
<ce:date-received day="22" month="7" year="1997"></ce:date-received>
<ce:date-accepted day="10" month="8" year="1997"></ce:date-accepted>
<ce:abstract>
<ce:section-title>Abstract</ce:section-title>
<ce:abstract-sec>
<ce:simple-para>The present-day Sahara occupies an area of slightly over 8 million km
<ce:sup>2</ce:sup>
in Africa, between latitudes 16 and 32° N, circumscribed within the isohyet of 100 ± 50
<ce:hsp sp="0.25"></ce:hsp>
mm mean annual rainfall. The hyperarid area alternately expanded and shrank on both sides of a seemingly narrow semi-permanent eremitic zone along the Tropic of Cancer during the course of the Quaternary epoch (1·7
<ce:hsp sp="0.25"></ce:hsp>
Ma). The Cenozoic, Mesozoı̈c and Paleozoı̈c Sahara, in turn, has undergone drastic climatic changes as the African continent drifted northward from its Antartic position to reach its present latitudinal situation. But, seemingly the Sahara was never the large desert it now is, with the exception perhaps of the Upper Triassic Lower Liassic epochs. The Pleistocene and Holocene contrasting climate changes induced large variations in flora and fauna distribution, as well as in geomorphic processes.</ce:simple-para>
<ce:simple-para>The flora shifted from that of typical desert to tropical savanna and Mediterranean forest or steppe, depending on period and location. Fauna, in turn, changed more in abundance than in nature, since the same groups have been in existence since the Upper Pliocene–Lower Pleistocene. Large mammals, for instance, were mainly of Afro-tropical kinship throughout the Pleistocene and Holocene, while small mammals, in contrast, were predominantly of Mediterranean origin over the same periods. And such is still the case. There were varying large degrees in density of occurrence, but relatively minor fluctuations in nature, in response to such environmental changes as lake and dune expansion and retreat, and even glacier expansion and melting at higher elevations. The present-day man-made expansion of desertic conditions to the north and south actually threaten both flora and fauna alike in the short- and medium-term. Most African large mammals, still present in the desert until the second half of the 19th century, have now become extinct, or are on the very verge of extinction in the Sahara (some may be surviving further south, and/or in the East Africa's parks network). The situation, however, is far less dramatic for the flora, which still includes almost 3000 species of vascular plants, although some species — of economic value or not — are in danger from the man-made destruction of their habitat.</ce:simple-para>
</ce:abstract-sec>
</ce:abstract>
<ce:keywords>
<ce:section-title>Keywords</ce:section-title>
<ce:keyword>
<ce:text>Sahara</ce:text>
</ce:keyword>
<ce:keyword>
<ce:text>desert</ce:text>
</ce:keyword>
<ce:keyword>
<ce:text>climate change</ce:text>
</ce:keyword>
<ce:keyword>
<ce:text>biogeography</ce:text>
</ce:keyword>
<ce:keyword>
<ce:text>flora</ce:text>
</ce:keyword>
<ce:keyword>
<ce:text>fauna</ce:text>
</ce:keyword>
<ce:keyword>
<ce:text>natural resources</ce:text>
</ce:keyword>
<ce:keyword>
<ce:text>biodiversity</ce:text>
</ce:keyword>
<ce:keyword>
<ce:text>desertification</ce:text>
</ce:keyword>
</ce:keywords>
</head>
</converted-article>
</istex:document>
</istex:metadataXml>
<mods version="3.6">
<titleInfo lang="en">
<title>Climate, flora and fauna changes in the Sahara over the past 500 million years</title>
</titleInfo>
<titleInfo type="alternative" lang="en" contentType="CDATA">
<title>Climate, flora and fauna changes in the Sahara over the past 500 million years</title>
</titleInfo>
<name type="personal">
<namePart type="given">Henry N.</namePart>
<namePart type="family">Le Houérou</namePart>
<affiliation>327, rue de Jussieu, F-34090, Montpellier, France</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<typeOfResource>text</typeOfResource>
<genre type="research-article" displayLabel="Full-length article"></genre>
<originInfo>
<publisher>ELSEVIER</publisher>
<dateIssued encoding="w3cdtf">1997</dateIssued>
<copyrightDate encoding="w3cdtf">1997</copyrightDate>
</originInfo>
<language>
<languageTerm type="code" authority="iso639-2b">eng</languageTerm>
<languageTerm type="code" authority="rfc3066">en</languageTerm>
</language>
<physicalDescription>
<internetMediaType>text/html</internetMediaType>
</physicalDescription>
<abstract lang="en">The present-day Sahara occupies an area of slightly over 8 million km2in Africa, between latitudes 16 and 32° N, circumscribed within the isohyet of 100 ± 50mm mean annual rainfall. The hyperarid area alternately expanded and shrank on both sides of a seemingly narrow semi-permanent eremitic zone along the Tropic of Cancer during the course of the Quaternary epoch (1·7Ma). The Cenozoic, Mesozoı̈c and Paleozoı̈c Sahara, in turn, has undergone drastic climatic changes as the African continent drifted northward from its Antartic position to reach its present latitudinal situation. But, seemingly the Sahara was never the large desert it now is, with the exception perhaps of the Upper Triassic Lower Liassic epochs. The Pleistocene and Holocene contrasting climate changes induced large variations in flora and fauna distribution, as well as in geomorphic processes. The flora shifted from that of typical desert to tropical savanna and Mediterranean forest or steppe, depending on period and location. Fauna, in turn, changed more in abundance than in nature, since the same groups have been in existence since the Upper Pliocene–Lower Pleistocene. Large mammals, for instance, were mainly of Afro-tropical kinship throughout the Pleistocene and Holocene, while small mammals, in contrast, were predominantly of Mediterranean origin over the same periods. And such is still the case. There were varying large degrees in density of occurrence, but relatively minor fluctuations in nature, in response to such environmental changes as lake and dune expansion and retreat, and even glacier expansion and melting at higher elevations. The present-day man-made expansion of desertic conditions to the north and south actually threaten both flora and fauna alike in the short- and medium-term. Most African large mammals, still present in the desert until the second half of the 19th century, have now become extinct, or are on the very verge of extinction in the Sahara (some may be surviving further south, and/or in the East Africa's parks network). The situation, however, is far less dramatic for the flora, which still includes almost 3000 species of vascular plants, although some species — of economic value or not — are in danger from the man-made destruction of their habitat.</abstract>
<note>Sawyer, J. S.</note>
<note type="content">Section title: Regular Article</note>
<subject lang="en">
<genre>Keywords</genre>
<topic>Sahara</topic>
<topic>desert</topic>
<topic>climate change</topic>
<topic>biogeography</topic>
<topic>flora</topic>
<topic>fauna</topic>
<topic>natural resources</topic>
<topic>biodiversity</topic>
<topic>desertification</topic>
</subject>
<relatedItem type="host">
<titleInfo>
<title>Journal of Arid Environments</title>
</titleInfo>
<titleInfo type="abbreviated">
<title>YJARE</title>
</titleInfo>
<genre type="journal">journal</genre>
<originInfo>
<dateIssued encoding="w3cdtf">199712</dateIssued>
</originInfo>
<identifier type="ISSN">0140-1963</identifier>
<identifier type="PII">S0140-1963(00)X0043-2</identifier>
<part>
<date>199712</date>
<detail type="volume">
<number>37</number>
<caption>vol.</caption>
</detail>
<detail type="issue">
<number>4</number>
<caption>no.</caption>
</detail>
<extent unit="issue pages">
<start>575</start>
<end>721</end>
</extent>
<extent unit="pages">
<start>619</start>
<end>647</end>
</extent>
</part>
</relatedItem>
<identifier type="istex">D5A385F35E5DB42BC9497438209D9A6F0812DF62</identifier>
<identifier type="DOI">10.1006/jare.1997.0315</identifier>
<identifier type="PII">S0140-1963(97)90315-3</identifier>
<accessCondition type="use and reproduction" contentType="copyright">©1997 Academic Press</accessCondition>
<recordInfo>
<recordContentSource>ELSEVIER</recordContentSource>
<recordOrigin>Academic Press, ©1997</recordOrigin>
</recordInfo>
</mods>
</metadata>
<serie></serie>
</istex>
</record>

Pour manipuler ce document sous Unix (Dilib)

EXPLOR_STEP=$WICRI_ROOT/Wicri/Bois/explor/CheneBelgiqueV2/Data/Istex/Corpus
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000827 | SxmlIndent | more

Ou

HfdSelect -h $EXPLOR_AREA/Data/Istex/Corpus/biblio.hfd -nk 000827 | SxmlIndent | more

Pour mettre un lien sur cette page dans le réseau Wicri

{{Explor lien
   |wiki=    Wicri/Bois
   |area=    CheneBelgiqueV2
   |flux=    Istex
   |étape=   Corpus
   |type=    RBID
   |clé=     ISTEX:D5A385F35E5DB42BC9497438209D9A6F0812DF62
   |texte=   Climate, flora and fauna changes in the Sahara over the past 500 million years
}}

Wicri

This area was generated with Dilib version V0.6.27.
Data generation: Wed Mar 22 20:06:11 2017. Site generation: Wed Mar 6 16:09:04 2024