Palaeoenvironmental and palaeoclimatic implications of the Late‐Quaternary sediment record of Vico volcanic lake (central Italy)
Identifieur interne : 001816 ( Istex/Corpus ); précédent : 001815; suivant : 001817Palaeoenvironmental and palaeoclimatic implications of the Late‐Quaternary sediment record of Vico volcanic lake (central Italy)
Auteurs : Biancamaria NarcisiSource :
- Journal of Quaternary Science [ 0267-8179 ] ; 2001-03.
English descriptors
Abstract
A 15‐m‐long sediment core recovered from the Lago di Vico caldera lake in central Italy has been the subject of macrofacies description and sedimentological (organic carbon content, grain size and mineralogy) investigation. The results have been integrated with the pollen data from the same core in order to provide a regional climatic and environmental history, with inferences on past lake levels and on moisture and temperature regimes. Radiometric (14C and 40Ar/39Ar) dating, biostratigraphical considerations and tephra analyses provide a chronological framework and indicate that the sequence spans the last 90 000 yr. Several moist periods have been identified that were characterised by enhanced weathering by hydrolysis of the catchment rocks. These alternated with relatively dry phases associated with lowering of lake‐levels. The lowest hydrolysis efficiency of the whole record, accompanied by notable aeolian deposition, was attained during the last glacial phase but moisture conditions were such that the lake‐level did not decrease, probably owing to reduced temperatures. Evidence for cool climate also emerges for the early Pleniglacial. The highest available moisture was achieved within the Holocene at 5 kyr BP. The Late Holocene does not show either increase of aridity or degradation of the vegetation cover, until at least Roman times. Copyright © 2001 John Wiley & Sons, Ltd.
Url:
DOI: 10.1002/jqs.594
Links to Exploration step
ISTEX:F300BB34EAADC5698B95598EC9B1E321FC6DDE33Le document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">Palaeoenvironmental and palaeoclimatic implications of the Late‐Quaternary sediment record of Vico volcanic lake (central Italy)</title><author><name sortKey="Narcisi, Biancamaria" sort="Narcisi, Biancamaria" uniqKey="Narcisi B" first="Biancamaria" last="Narcisi">Biancamaria Narcisi</name><affiliation><mods:affiliation>ENEA – C.R. Casaccia, C.P. 2400, 00100 Roma, Italy</mods:affiliation></affiliation><affiliation><mods:affiliation>ENEA‐C.R. Casaccia, PO Box 2400, I‐00100 Rome, Italy.</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:F300BB34EAADC5698B95598EC9B1E321FC6DDE33</idno><date when="2001" year="2001">2001</date><idno type="doi">10.1002/jqs.594</idno><idno type="url">https://api.istex.fr/document/F300BB34EAADC5698B95598EC9B1E321FC6DDE33/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">001816</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">001816</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Palaeoenvironmental and palaeoclimatic implications of the Late‐Quaternary sediment record of Vico volcanic lake (central Italy)</title><author><name sortKey="Narcisi, Biancamaria" sort="Narcisi, Biancamaria" uniqKey="Narcisi B" first="Biancamaria" last="Narcisi">Biancamaria Narcisi</name><affiliation><mods:affiliation>ENEA – C.R. Casaccia, C.P. 2400, 00100 Roma, Italy</mods:affiliation></affiliation><affiliation><mods:affiliation>ENEA‐C.R. Casaccia, PO Box 2400, I‐00100 Rome, Italy.</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Journal of Quaternary Science</title><title level="j" type="sub">Published for the Quaternary Research Association</title><title level="j" type="abbrev">J. Quaternary Sci.</title><idno type="ISSN">0267-8179</idno><idno type="eISSN">1099-1417</idno><imprint><publisher>John Wiley & Sons, Ltd.</publisher><pubPlace>Chichester, UK</pubPlace><date type="published" when="2001-03">2001-03</date><biblScope unit="volume">16</biblScope><biblScope unit="issue">3</biblScope><biblScope unit="page" from="245">245</biblScope><biblScope unit="page" to="255">255</biblScope></imprint><idno type="ISSN">0267-8179</idno></series><idno type="istex">F300BB34EAADC5698B95598EC9B1E321FC6DDE33</idno><idno type="DOI">10.1002/jqs.594</idno><idno type="ArticleID">JQS594</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0267-8179</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Late Quaternary</term><term>central Italy</term><term>lake‐levels</term><term>sediment analysis</term><term>volcanic lake</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">A 15‐m‐long sediment core recovered from the Lago di Vico caldera lake in central Italy has been the subject of macrofacies description and sedimentological (organic carbon content, grain size and mineralogy) investigation. The results have been integrated with the pollen data from the same core in order to provide a regional climatic and environmental history, with inferences on past lake levels and on moisture and temperature regimes. Radiometric (14C and 40Ar/39Ar) dating, biostratigraphical considerations and tephra analyses provide a chronological framework and indicate that the sequence spans the last 90 000 yr. Several moist periods have been identified that were characterised by enhanced weathering by hydrolysis of the catchment rocks. These alternated with relatively dry phases associated with lowering of lake‐levels. The lowest hydrolysis efficiency of the whole record, accompanied by notable aeolian deposition, was attained during the last glacial phase but moisture conditions were such that the lake‐level did not decrease, probably owing to reduced temperatures. Evidence for cool climate also emerges for the early Pleniglacial. The highest available moisture was achieved within the Holocene at 5 kyr BP. The Late Holocene does not show either increase of aridity or degradation of the vegetation cover, until at least Roman times. Copyright © 2001 John Wiley & Sons, Ltd.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>Biancamaria Narcisi</name><affiliations><json:string>ENEA – C.R. Casaccia, C.P. 2400, 00100 Roma, Italy</json:string><json:string>ENEA‐C.R. Casaccia, PO Box 2400, I‐00100 Rome, Italy.</json:string></affiliations></json:item></author><subject><json:item><lang><json:string>eng</json:string></lang><value>central Italy</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>volcanic lake</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>sediment analysis</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>lake‐levels</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Late Quaternary</value></json:item></subject><articleId><json:string>JQS594</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><abstract>A 15‐m‐long sediment core recovered from the Lago di Vico caldera lake in central Italy has been the subject of macrofacies description and sedimentological (organic carbon content, grain size and mineralogy) investigation. The results have been integrated with the pollen data from the same core in order to provide a regional climatic and environmental history, with inferences on past lake levels and on moisture and temperature regimes. Radiometric (14C and 40Ar/39Ar) dating, biostratigraphical considerations and tephra analyses provide a chronological framework and indicate that the sequence spans the last 90 000 yr. Several moist periods have been identified that were characterised by enhanced weathering by hydrolysis of the catchment rocks. These alternated with relatively dry phases associated with lowering of lake‐levels. The lowest hydrolysis efficiency of the whole record, accompanied by notable aeolian deposition, was attained during the last glacial phase but moisture conditions were such that the lake‐level did not decrease, probably owing to reduced temperatures. Evidence for cool climate also emerges for the early Pleniglacial. The highest available moisture was achieved within the Holocene at 5 kyr BP. The Late Holocene does not show either increase of aridity or degradation of the vegetation cover, until at least Roman times. Copyright © 2001 John Wiley & Sons, Ltd.</abstract><qualityIndicators><score>7.508</score><pdfVersion>1.2</pdfVersion><pdfPageSize>598 x 846 pts</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>1402</abstractCharCount><pdfWordCount>7469</pdfWordCount><pdfCharCount>46132</pdfCharCount><pdfPageCount>11</pdfPageCount><abstractWordCount>209</abstractWordCount></qualityIndicators><title>Palaeoenvironmental and palaeoclimatic implications of the Late‐Quaternary sediment record of Vico volcanic lake (central Italy)</title><refBibs><json:item><author><json:item><name>L Barbanti</name></json:item></author><host><volume>25</volume><pages><last>139</last><first>117</first></pages><author></author><title>Memorie dell'Istituto Italiano di Idrobiologia</title></host><title>Lago di Vico: rilevamento batimetrico e note geomorfologiche</title></json:item><json:item><author><json:item><name>F Barberi</name></json:item><json:item><name>G Buonasorte</name></json:item><json:item><name>R Cioni</name></json:item><json:item><name>A Fiordelisi</name></json:item><json:item><name>L Foresi</name></json:item><json:item><name>S Iaccarino</name></json:item><json:item><name>MA Laurenzi</name></json:item><json:item><name>A Sbrana</name></json:item><json:item><name>L Vernia</name></json:item><json:item><name>IM Villa</name></json:item></author><host><volume>49</volume><pages><last>134</last><first>77</first></pages><author></author><title>Memorie Descrittive della Carta Geologica d'Italia</title></host><title>Plio‐Pleistocene geological evolution of the geothermal area of Tuscany and Latium</title></json:item><json:item><author><json:item><name>M Barbieri</name></json:item><json:item><name>A Peccerillo</name></json:item><json:item><name>G Poli</name></json:item><json:item><name>L Tolomeo</name></json:item></author><host><volume>99</volume><pages><last>497</last><first>485</first></pages><author></author><title>Contributions to Mineralogy and Petrology</title></host><title>Major, trace element and Sr isotopic composition of lavas from Vico volcano (Central Italy) and their evolution in an open system</title></json:item><json:item><author><json:item><name>J‐L Beaulieu</name></json:item></author><host><volume>13</volume><pages><last>132</last><first>111</first></pages><author></author><title>Boreas</title></host><title>A long Upper Pleistocene pollen record from Les Echets, near Lyon, France</title></json:item><json:item><author><json:item><name>A Bertagnini</name></json:item><json:item><name>A Sbrana</name></json:item></author><host><volume>35</volume><pages><last>713</last><first>699</first></pages><author></author><title>Memorie della Società Geologica Italiana</title></host><title>Il vulcano di Vico: stratigrafia del complesso vulcanico e sequenze eruttive delle formazioni piroclastiche</title></json:item><json:item><host><author></author><title>Vulcano di Vico</title></host></json:item><json:item><author><json:item><name>P Bertrand</name></json:item><json:item><name>S Brocero</name></json:item><json:item><name>E Lallier‐Verges</name></json:item><json:item><name>N Tribovillard</name></json:item><json:item><name>E Bonifay</name></json:item></author><host><volume>163</volume><pages><last>433</last><first>427</first></pages><author></author><title>Bulletin de la Société géologique de France</title></host><title>Sédimentation organique lacustre et paléoclimats du Pléistocène aux moyennes latitudes: exemple du lac du Bouchet, Haute Loire, France (résultats préliminaires)</title></json:item><json:item><author><json:item><name>E Bonifay</name></json:item><json:item><name>KM Creer</name></json:item><json:item><name>J‐L Beaulieu</name></json:item><json:item><name>G Delibrias</name></json:item><json:item><name>G Perinet</name></json:item><json:item><name>A Pons</name></json:item><json:item><name>M Reille</name></json:item><json:item><name>S Servant</name></json:item><json:item><name>G Smith</name></json:item><json:item><name>N Thouveny</name></json:item><json:item><name>E Truze</name></json:item><json:item><name>P Tucholka</name></json:item></author><host><pages><last>116</last><first>90</first></pages><author></author><title>Climate—History, Periodicity, and Predictability</title></host><title>Study of the Holocene and Late Wurmian sediments of Lac du Bouchet (Haute‐Loire, France): first results</title></json:item><json:item><author><json:item><name>G Borghetti</name></json:item><json:item><name>A Sbrana</name></json:item><json:item><name>F Sollevanti</name></json:item></author><host><volume>4</volume><pages><last>254</last><first>253</first></pages><author></author><title>Rendiconti della Società Geologica Italiana</title></host><title>Vulcano‐tettonica dell'area dei Monti Cimini e rapporti cronologici tra vulcanismo cimino e vicano</title></json:item><json:item><author><json:item><name>C Campobasso</name></json:item><json:item><name>R Cioni</name></json:item><json:item><name>L Salvati</name></json:item><json:item><name>A Sbrana</name></json:item></author><host><volume>49</volume><pages><last>290</last><first>277</first></pages><author></author><title>Memorie Descrittive della Carta Geologica d'Italia</title></host><title>Geology and paleogeographic evolution of a peripheral sector of the Vico and Sabatini volcanic complex, between Civita Castellana and Mazzano Romano, (Latium, Italy)</title></json:item><json:item><host><author></author><title>Chamley H. 1989. Clay Sedimentology. Springer‐Verlag: Berlin.</title></host></json:item><json:item><author><json:item><name>R Cioni</name></json:item><json:item><name>A Sbrana</name></json:item><json:item><name>A Bertagnini</name></json:item><json:item><name>G Buonasorte</name></json:item><json:item><name>P Landi</name></json:item><json:item><name>U Rossi</name></json:item><json:item><name>L Salvati</name></json:item></author><host><volume>56</volume><pages><last>155</last><first>137</first></pages><author></author><title>Periodico di Mineralogia</title></host><title>Tephrostratigraphic correlations in the Vulsini, Vico and Sabatini volcanic successions</title></json:item><json:item><author><json:item><name>KM Creer</name></json:item><json:item><name>N Thouveny</name></json:item></author><host><volume>15</volume><pages><last>100</last><first>99</first></pages><author></author><title>The Euromaars Project</title></host><title>Preface</title></json:item><json:item><author><json:item><name>A Cundari</name></json:item></author><host><volume>53</volume><pages><last>144</last><first>129</first></pages><author></author><title>Contributions to Mineralogy and Petrology</title></host><title>Mineral chemistry and petrogenetic aspects of the Vico lavas, Roman volcanic region</title></json:item><json:item><author><json:item><name>A Cundari</name></json:item><json:item><name>G Graziani</name></json:item></author><host><volume>33</volume><pages><last>43</last><first>35</first></pages><author></author><title>Periodico di Mineralogia</title></host><title>Prodotti di alterazione della leucite nelle vulcaniti vicane</title></json:item><json:item><author><json:item><name>A Cundari</name></json:item><json:item><name>PP Mattias</name></json:item></author><host><volume>38</volume><pages><last>114</last><first>98</first></pages><author></author><title>Bulletin Volcanologique</title></host><title>Evolution of the Vico lavas, Roman volcanic Region, Italy</title></json:item><json:item><author><json:item><name>G Digerfeldt</name></json:item><json:item><name>S Olsson</name></json:item><json:item><name>P Sandgren</name></json:item></author><host><volume>158</volume><pages><last>82</last><first>65</first></pages><author></author><title>Palaeogeography, Palaeoclimatology, Palaeoecology</title></host><title>Reconstruction of lake‐level changes in Lake Xinias, central Greece, during the last 40 000 years</title></json:item><json:item><author><json:item><name>M Follieri</name></json:item><json:item><name>D Magri</name></json:item><json:item><name>L Sadori</name></json:item></author><host><volume>30</volume><pages><last>356</last><first>329</first></pages><issue>3–4</issue><author></author><title>Pollen et Spores</title></host><title>250,000‐year pollen record from Valle di Castiglione (Roma)</title></json:item><json:item><author><json:item><name>M Follieri</name></json:item><json:item><name>D Magri</name></json:item><json:item><name>B Narcisi</name></json:item></author><host><volume>45</volume><pages><last>891</last><first>889</first></pages><author></author><title>Memorie della Società Geologica Italiana</title></host><title>A comparison between lithostratigraphy and palynology from the lacustrine sediments of Valle di Castiglione (Roma) over the last 0.25 Ma</title></json:item><json:item><author><json:item><name>M Follieri</name></json:item><json:item><name>D Magri</name></json:item><json:item><name>B Narcisi</name></json:item></author><host><volume>49</volume><pages><last>107</last><first>95</first></pages><author></author><title>Paleolimnology of European Maar Lakes</title></host><title>Palaeoenvironmental investigations on long sediment cores from volcanic lakes of Lazio (central Italy)—an overview</title></json:item><json:item><author><json:item><name>M Follieri</name></json:item><json:item><name>M Giardini</name></json:item><json:item><name>D Magri</name></json:item><json:item><name>L Sadori</name></json:item></author><host><volume>47/48</volume><pages><last>20</last><first>3</first></pages><author></author><title>Quaternary International</title></host><title>Palynostratigraphy of the last glacial period in the volcanic region of Central Italy</title></json:item><json:item><author><json:item><name>P Francus</name></json:item><json:item><name>S Leroy</name></json:item><json:item><name>I Margerai</name></json:item><json:item><name>G Seret</name></json:item><json:item><name>G Wansard</name></json:item></author><host><volume>49</volume><pages><last>304</last><first>289</first></pages><author></author><title>Paleolimnology of European Maar Lakes</title></host><title>A multidisciplinary study of the Vico maar sequence (Latium, Italy): part the last cycle in the Mediterranean area. Preliminary results</title></json:item><json:item><author><json:item><name>AHE Frank</name></json:item></author><host><volume>6</volume><pages><last>85</last><first>67</first></pages><author></author><title>Palaeogeography, Palaeoclimatology, Palaeoecology</title></host><title>Pollen stratigraphy of the Lake of Vico (central Italy)</title></json:item><json:item><author><json:item><name>HE Gaudette</name></json:item><json:item><name>WR Flight</name></json:item><json:item><name>L Toner</name></json:item><json:item><name>DW Folger</name></json:item></author><host><volume>44</volume><pages><last>253</last><first>249</first></pages><author></author><title>Journal of Sedimentary Petrology</title></host><title>An inexpensive titration method for the determination of organic carbon in recent sediments</title></json:item><json:item><author><json:item><name>C Giraudi</name></json:item></author><host><volume>70</volume><pages><last>260</last><first>249</first></pages><author></author><title>Palaeogeography, Palaeoclimatology, Palaeoecology</title></host><title>Lake levels and climate for the last 30,000 years in the Fucino area (Abruzzo, Central Italy)_a review</title></json:item><json:item><host><author></author><title>Ricerche paleoclimatiche in ambiente lacustre: Il contributo della Task Force 'Ambiente globale e cambiamenti climatici'</title></host></json:item><json:item><author><json:item><name>S Guerzoni</name></json:item><json:item><name>E Molinaroli</name></json:item><json:item><name>R Chester</name></json:item></author><host><volume>44</volume><pages><last>654</last><first>631</first></pages><issue>3–4</issue><author></author><title>Deep‐Sea Research II</title></host><title>Saharan dust inputs to the western Mediterranean Sea: depositional patterns, geochemistry and sedimentological implications</title></json:item><json:item><author><json:item><name>SP Harrison</name></json:item><json:item><name>G Digerfeldt</name></json:item></author><host><volume>12</volume><pages><last>248</last><first>233</first></pages><author></author><title>Quaternary Science Reviews</title></host><title>European lakes as palaeohydrological and palaeoclimatic indicators</title></json:item><json:item><author><json:item><name>SP Harrison</name></json:item><json:item><name>L Saarse</name></json:item><json:item><name>G Digerfeldt</name></json:item></author><host><volume>6</volume><pages><last>169</last><first>159</first></pages><author></author><title>Evaluation of Climate Proxy Data in Relation to the European Holocene</title></host><title>Holocene changes in lake levels as climate proxy data in Europe</title></json:item><json:item><author><json:item><name>BF Jones</name></json:item><json:item><name>CJ Bowser</name></json:item></author><host><pages><last>235</last><first>179</first></pages><author></author><title>Lakes—Chemistry, Geology, Physics</title></host><title>The mineralogy and related chemistry of lake sediments</title></json:item><json:item><author><json:item><name>N Kallel</name></json:item><json:item><name>M Paterne</name></json:item><json:item><name>L Labeyrie</name></json:item><json:item><name>J‐C Duplessy</name></json:item><json:item><name>M Arnold</name></json:item></author><host><volume>135</volume><pages><last>108</last><first>97</first></pages><author></author><title>Palaeogeography, Palaeoclimatology, Palaeoecology</title></host><title>Temperature and salinity records of the Tyrrhenian Sea during the last 18,000 years</title></json:item><json:item><host><author></author><title>K/Ar chronology of the Vico volcano (Latium, Italy)</title></host></json:item><json:item><author><json:item><name>MA Laurenzi</name></json:item><json:item><name>IM Villa</name></json:item></author><host><volume>56</volume><pages><last>293</last><first>285</first></pages><author></author><title>Periodico di Mineralogia</title></host><title>40Ar/39Ar chronostratigraphy of Vico ignimbrites</title></json:item><json:item><author><json:item><name>B Le</name></json:item><json:item><name>M Le</name></json:item><json:item><name>A Streckeisen</name></json:item><json:item><name>B Zanettin</name></json:item></author><host><volume>27</volume><pages><last>750</last><first>745</first></pages><author></author><title>Journal of Petrology</title></host><title>A chemical classification of volcanic rocks based on the total alkali–silica diagram</title></json:item><json:item><author><json:item><name>SAG Leroy</name></json:item></author><host><volume>101</volume><pages><last>309</last><first>303</first></pages><author></author><title>Bulletin de la Société belge de Géologie</title></host><title>Analyses palynologiques préliminaires d'une phase relativement tempérée (stade isotopique 3) au sein de la dernière période glaciaire, maar de Vico (Latium, Italie)</title></json:item><json:item><author><json:item><name>SAG Leroy</name></json:item><json:item><name>S Giralt</name></json:item><json:item><name>P Francus</name></json:item><json:item><name>G Seret</name></json:item></author><host><volume>15</volume><pages><last>202</last><first>189</first></pages><author></author><title>Quaternary Science Reviews</title></host><title>The high sensitivity of the palynological record in the Vico maar lacustrine sequence (Latium, Italy) highlights the climatic gradient through Europe for the last 90 ka</title></json:item><json:item><author><json:item><name>E Locardi</name></json:item></author><host><volume>72</volume><pages><last>171</last><first>55</first></pages><issue>1</issue><author></author><title>Atti della Società Toscana di Scienze Naturali Series A</title></host><title>Tipi di ignimbriti di magmi mediterranei—Le ignimbriti del Vulcano di Vico</title></json:item><json:item><host><author></author><title>Lulli L, Bidini D, Lorenzoni P, Quantin P, Raglione M. 1990. I suoli caposaldo dell'apparato vulcanico di Vico. Istituto sperimentale per lo studio e la difesa del suolo: Firenze.</title></host></json:item><json:item><author><json:item><name>FJH Mackereth</name></json:item></author><host><volume>161</volume><pages><last>309</last><first>295</first></pages><author></author><title>Proceedings of the Royal Society of London, Series B</title></host><title>Chemical investigation of lake sediments and their interpretation</title></json:item><json:item><author><json:item><name>D Magri</name></json:item><json:item><name>L Sadori</name></json:item></author><host><volume>8</volume><pages><last>260</last><first>247</first></pages><author></author><title>Vegetation History and Archaeobotany</title></host><title>Late Pleistocene and Holocene pollen stratigraphy at Lago di Vico (central Italy)</title></json:item><json:item><author><json:item><name>FG Margaritora</name></json:item></author><host><volume>50</volume><pages><last>336</last><first>319</first></pages><author></author><title>Limnology in Italy</title></host><title>Limnology in Latium: the volcanic lakes</title></json:item><json:item><author><json:item><name>PP Mattias</name></json:item><json:item><name>U Ventriglia</name></json:item></author><host><volume>9</volume><pages><last>384</last><first>331</first></pages><author></author><title>Memorie della Società Geologica Italiana</title></host><title>La regione vulcanica dei Monti Sabatini e Cimini</title></json:item><json:item><author><json:item><name>B Narcisi</name></json:item></author><host><volume>12</volume><pages><last>78</last><first>69</first></pages><author></author><title>Il Quaternario</title></host><title>Nuovi ritrovamenti del tephra tardiglaciale etneo in Italia Centrale</title></json:item><json:item><author><json:item><name>B Narcisi</name></json:item></author><host><volume>54</volume><pages><last>252</last><first>246</first></pages><author></author><title>Quaternary Research</title></host><title>Late Quaternary eolian deposition in Central Italy</title></json:item><json:item><author><json:item><name>B Narcisi</name></json:item><json:item><name>B Anselmi</name></json:item><json:item><name>F Catalano</name></json:item><json:item><name>P Dai</name></json:item><json:item><name>G Magri</name></json:item></author><host><volume>11</volume><pages><last>362</last><first>353</first></pages><author></author><title>Quaternary Science Reviews</title></host><title>Lithostratigraphy of the 250,000 year record of lacustrine sediments from the Valle di Castiglione crater, Roma</title></json:item><json:item><author><json:item><name>B Narcisi</name></json:item><json:item><name>L Vezzoli</name></json:item></author><host><volume>21</volume><pages><last>50</last><first>31</first></pages><author></author><title>Global and Planetary Change</title></host><title>Quaternary stratigraphy of distal tephra layers in the Mediterranean—an overview</title></json:item><json:item><author><json:item><name>M Nicoletti</name></json:item></author><host><volume>38</volume><pages><last>20</last><first>1</first></pages><author></author><title>Periodico di Mineralogia</title></host><title>Datazioni argon potassio di alcune vulcaniti delle Regioni vulcaniche Cimina e Vicana</title></json:item><json:item><host><author></author><title>Etude géologique et géochimique du volcanisme du Latium Italie: exemple du Vico et des Vulsini</title></host></json:item><json:item><author><json:item><name>G Perini</name></json:item></author><host><volume>17</volume><pages><last>178</last><first>173</first></pages><author></author><title>Plinius</title></host><title>The magmatological evolution of Vico volcano</title></json:item><json:item><author><json:item><name>G Perini</name></json:item><json:item><name>S Conticelli</name></json:item><json:item><name>L Francalanci</name></json:item></author><host><volume>40</volume><pages><last>93</last><first>67</first></pages><author></author><title>Mineralogica et Petrografica Acta</title></host><title>Inferences on the volcanic history of the Vico volcano, Roman Magmatic Province, Central Italy: stratigraphic, petrographic and geochemical data</title></json:item><json:item><author><json:item><name>G Perini</name></json:item><json:item><name>S Conticelli</name></json:item><json:item><name>L Francalanci</name></json:item><json:item><name>JP Davidson</name></json:item></author><host><volume>95</volume><pages><last>272</last><first>247</first></pages><author></author><title>Journal of Volcanology and Geothermal Research</title></host><title>The relationship between potassic and calc‐alkaline post‐orogenic magmatism at Vico volcano, central Italy</title></json:item><json:item><author><json:item><name>IC Prentice</name></json:item><json:item><name>J Guiot</name></json:item><json:item><name>SP Harrison</name></json:item></author><host><volume>360</volume><pages><last>660</last><first>658</first></pages><author></author><title>Nature</title></host><title>Mediterranean vegetation, lake levels and paleoclimate at Last Glacial Maximum</title></json:item><json:item><author><json:item><name>P Quantin</name></json:item><json:item><name>B Dabin</name></json:item><json:item><name>A Bouleau</name></json:item><json:item><name>L Lulli</name></json:item><json:item><name>D Bidini</name></json:item></author><host><volume>7</volume><pages><last>117</last><first>99</first></pages><author></author><title>Volcanic Soils: Weathering and Landscape Relationship of Soils on Tephra and Basalt</title></host><title>Characteristics and genesis of two andosols in Central Italy</title></json:item><json:item><author><json:item><name>P Quantin</name></json:item><json:item><name>P Lorenzoni</name></json:item></author><host><volume>35‐A</volume><pages><last>296</last><first>289</first></pages><author></author><title>Mineralogica et Petrografica Acta</title></host><title>Weathering of leucite to clay minerals in tephrites of the Vico volcano</title></json:item><json:item><author><json:item><name>M Raglione</name></json:item></author><host><pages><last>34</last><first>25</first></pages><author></author><title>I suoli caposaldo dell'apparato vulcanico di Vico</title></host><title>Notizie geografiche</title></json:item><json:item><author><json:item><name>B Rein</name></json:item><json:item><name>JFW Negendank</name></json:item></author><host><volume>49</volume><pages><last>171</last><first>164</first></pages><author></author><title>Paleolimnology of European Maar Lakes</title></host><title>Organic carbon contents of sediments from Lake Schalkenmehrener maar: a paleoclimate indicator</title></json:item><json:item><author><json:item><name>C Robinson</name></json:item></author><host><volume>118</volume><pages><last>254</last><first>235</first></pages><author></author><title>Chemical Geology</title></host><title>Lago Grande di Monticchio, southern Italy: a long record of environmental change illustrated by sediment geochemistry</title></json:item><json:item><author><json:item><name>M Saarnisto</name></json:item></author><host><pages><last>369</last><first>343</first></pages><author></author><title>Handbook of Holocene Palaeoecology and Palaeohydrology</title></host><title>Annually laminated lake sediments</title></json:item><json:item><author><json:item><name>A Scoppola</name></json:item></author><host><pages><last>79</last><first>73</first></pages><author></author><title>L'ambiente nella Tuscia laziale—Aree protette e di interesse naturalistico della provincia di Viterbo</title></host><title>La vegetazione della Riserva Naturale Regionale Lago di Vico</title></json:item><json:item><host><author></author><title>La vegetazione della Caldera del Lago di Vico</title></host></json:item><json:item><author><json:item><name>F Simmi</name></json:item></author><host><pages><last>65</last><first>61</first></pages><author></author><title>L'ambiente nella Tuscia laziale_Aree protette e di interesse naturalistico della provincia di Viterbo</title></host><title>Aspetti di tutela e di gestione della Riserva Naturale Regionale Lago di Vico</title></json:item><json:item><author><json:item><name>F Simmi</name></json:item><json:item><name>M Zapparoli</name></json:item></author><host><pages><last>90</last><first>81</first></pages><author></author><title>L'ambiente nella Tuscia laziale—Aree protette e di interesse naturalistico della provincia di Viterbo</title></host><title>Aspetti faunistici della Riserva Naturale Regionale Lago di Vico</title></json:item><json:item><author><json:item><name>F Sollevanti</name></json:item></author><host><volume>17</volume><pages><last>217</last><first>203</first></pages><author></author><title>Journal of Volcanology and Geothermal Research</title></host><title>Geologic, volcanologic and tectonic setting of the Vico–Cimino area, Italy</title></json:item><json:item><author><json:item><name>E Truze</name></json:item><json:item><name>K Kelts</name></json:item></author><host><volume>49</volume><pages><last>275</last><first>237</first></pages><author></author><title>Paleolimnology of European Maar Lakes</title></host><title>Sedimentology and paleoenvironment from the maar Lac du Bouchet from the last climatic cycle, 0–120,000 years (Massif Central, France)</title></json:item><json:item><author><json:item><name>JM Verstraten</name></json:item><json:item><name>J Sevink</name></json:item></author><host><volume>21</volume><pages><last>285</last><first>271</first></pages><author></author><title>Geoderma</title></host><title>Clay soils on limestone in South Limburg, The Netherlands, 3. Soil formation</title></json:item><json:item><author><json:item><name>B Villemant</name></json:item><json:item><name>C Fléhoc</name></json:item></author><host><volume>91</volume><pages><last>326</last><first>312</first></pages><author></author><title>Earth and Planetary Science Letters</title></host><title>U–Th fractionation by fluids in K‐rich magma genesis: the Vico volcano, central Italy</title></json:item><json:item><host><author></author><title>Watson EV. 1981. British Mosses and Liverworts. Cambridge University Press: Cambridge.</title></host></json:item></refBibs><genre><json:string>article</json:string></genre><host><volume>16</volume><publisherId><json:string>JQS</json:string></publisherId><pages><total>11</total><last>255</last><first>245</first></pages><issn><json:string>0267-8179</json:string></issn><issue>3</issue><subject><json:item><value>Research Article</value></json:item></subject><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1099-1417</json:string></eissn><title>Journal of Quaternary Science</title><doi><json:string>10.1002/(ISSN)1099-1417</json:string></doi></host><categories><wos><json:string>science</json:string><json:string>geosciences, multidisciplinary</json:string><json:string>geography, physical</json:string></wos><scienceMetrix><json:string>natural sciences</json:string><json:string>earth & environmental sciences</json:string><json:string>paleontology</json:string></scienceMetrix></categories><publicationDate>2001</publicationDate><copyrightDate>2001</copyrightDate><doi><json:string>10.1002/jqs.594</json:string></doi><id>F300BB34EAADC5698B95598EC9B1E321FC6DDE33</id><score>0.019739822</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/F300BB34EAADC5698B95598EC9B1E321FC6DDE33/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/F300BB34EAADC5698B95598EC9B1E321FC6DDE33/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/F300BB34EAADC5698B95598EC9B1E321FC6DDE33/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Palaeoenvironmental and palaeoclimatic implications of the Late‐Quaternary sediment record of Vico volcanic lake (central Italy)</title></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>John Wiley & Sons, Ltd.</publisher><pubPlace>Chichester, UK</pubPlace><availability><p>Copyright © 2001 John Wiley & Sons, Ltd.</p></availability><date>2001</date></publicationStmt><notesStmt><note>European Union ARIDUSEUROMED Project - No. ENV4‐CT95‐0062;</note><note>European Commission EUROMAARS Project</note></notesStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Palaeoenvironmental and palaeoclimatic implications of the Late‐Quaternary sediment record of Vico volcanic lake (central Italy)</title><author xml:id="author-1"><persName><forename type="first">Biancamaria</forename><surname>Narcisi</surname></persName><affiliation>ENEA – C.R. Casaccia, C.P. 2400, 00100 Roma, Italy</affiliation><affiliation>ENEA‐C.R. Casaccia, PO Box 2400, I‐00100 Rome, Italy.</affiliation></author></analytic><monogr><title level="j">Journal of Quaternary Science</title><title level="j" type="sub">Published for the Quaternary Research Association</title><title level="j" type="abbrev">J. Quaternary Sci.</title><idno type="pISSN">0267-8179</idno><idno type="eISSN">1099-1417</idno><idno type="DOI">10.1002/(ISSN)1099-1417</idno><imprint><publisher>John Wiley & Sons, Ltd.</publisher><pubPlace>Chichester, UK</pubPlace><date type="published" when="2001-03"></date><biblScope unit="volume">16</biblScope><biblScope unit="issue">3</biblScope><biblScope unit="page" from="245">245</biblScope><biblScope unit="page" to="255">255</biblScope></imprint></monogr><idno type="istex">F300BB34EAADC5698B95598EC9B1E321FC6DDE33</idno><idno type="DOI">10.1002/jqs.594</idno><idno type="ArticleID">JQS594</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>2001</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>A 15‐m‐long sediment core recovered from the Lago di Vico caldera lake in central Italy has been the subject of macrofacies description and sedimentological (organic carbon content, grain size and mineralogy) investigation. The results have been integrated with the pollen data from the same core in order to provide a regional climatic and environmental history, with inferences on past lake levels and on moisture and temperature regimes. Radiometric (14C and 40Ar/39Ar) dating, biostratigraphical considerations and tephra analyses provide a chronological framework and indicate that the sequence spans the last 90 000 yr. Several moist periods have been identified that were characterised by enhanced weathering by hydrolysis of the catchment rocks. These alternated with relatively dry phases associated with lowering of lake‐levels. The lowest hydrolysis efficiency of the whole record, accompanied by notable aeolian deposition, was attained during the last glacial phase but moisture conditions were such that the lake‐level did not decrease, probably owing to reduced temperatures. Evidence for cool climate also emerges for the early Pleniglacial. The highest available moisture was achieved within the Holocene at 5 kyr BP. The Late Holocene does not show either increase of aridity or degradation of the vegetation cover, until at least Roman times. Copyright © 2001 John Wiley & Sons, Ltd.</p></abstract><textClass xml:lang="en"><keywords scheme="keyword"><list><head>keywords</head><item><term>central Italy</term></item><item><term>volcanic lake</term></item><item><term>sediment analysis</term></item><item><term>lake‐levels</term></item><item><term>Late Quaternary</term></item></list></keywords></textClass><textClass><keywords scheme="Journal Subject"><list><head>article-category</head><item><term>Research Article</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="2000-06-01">Received</change><change when="2000-10-05">Registration</change><change when="2001-03">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/F300BB34EAADC5698B95598EC9B1E321FC6DDE33/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Wiley, elements deleted: body"><istex:xmlDeclaration>version="1.0" encoding="UTF-8" standalone="yes"</istex:xmlDeclaration><istex:document><component version="2.0" type="serialArticle" xml:lang="en"><header><publicationMeta level="product"><publisherInfo><publisherName>John Wiley & Sons, Ltd.</publisherName><publisherLoc>Chichester, UK</publisherLoc></publisherInfo><doi registered="yes">10.1002/(ISSN)1099-1417</doi><issn type="print">0267-8179</issn><issn type="electronic">1099-1417</issn><idGroup><id type="product" value="JQS"></id></idGroup><titleGroup><title type="main" xml:lang="en" sort="JOURNAL OF QUATERNARY SCIENCE">Journal of Quaternary Science</title><title type="subtitle">Published for the Quaternary Research Association</title><title type="short">J. Quaternary Sci.</title></titleGroup></publicationMeta><publicationMeta level="part" position="30"><doi origin="wiley" registered="yes">10.1002/jqs.v16:3</doi><numberingGroup><numbering type="journalVolume" number="16">16</numbering><numbering type="journalIssue">3</numbering></numberingGroup><coverDate startDate="2001-03">March 2001</coverDate></publicationMeta><publicationMeta level="unit" type="article" position="4" status="forIssue"><doi origin="wiley" registered="yes">10.1002/jqs.594</doi><idGroup><id type="unit" value="JQS594"></id></idGroup><countGroup><count type="pageTotal" number="11"></count></countGroup><titleGroup><title type="articleCategory">Research Article</title><title type="tocHeading1">Research Articles</title></titleGroup><copyright ownership="publisher">Copyright © 2001 John Wiley & Sons, Ltd.</copyright><eventGroup><event type="manuscriptReceived" date="2000-06-01"></event><event type="manuscriptRevised" date="2000-10-03"></event><event type="manuscriptAccepted" date="2000-10-05"></event><event type="firstOnline" date="2001-04-24"></event><event type="publishedOnlineFinalForm" date="2001-04-24"></event><event type="xmlConverted" agent="Converter:JWSART34_TO_WML3G version:2.3.2 mode:FullText source:HeaderRef result:HeaderRef" date="2010-03-15"></event><event type="xmlConverted" agent="Converter:WILEY_ML3G_TO_WILEY_ML3GV2 version:3.8.8" date="2014-02-01"></event><event type="xmlConverted" agent="Converter:WML3G_To_WML3G version:4.1.7 mode:FullText,remove_FC" date="2014-10-30"></event></eventGroup><numberingGroup><numbering type="pageFirst">245</numbering><numbering type="pageLast">255</numbering></numberingGroup><correspondenceTo>ENEA‐C.R. Casaccia, PO Box 2400, I‐00100 Rome, Italy.</correspondenceTo><linkGroup><link type="toTypesetVersion" href="file:JQS.JQS594.pdf"></link></linkGroup></publicationMeta><contentMeta><countGroup><count type="figureTotal" number="5"></count><count type="tableTotal" number="0"></count><count type="referenceTotal" number="67"></count></countGroup><titleGroup><title type="main" xml:lang="en">Palaeoenvironmental and palaeoclimatic implications of the Late‐Quaternary sediment record of Vico volcanic lake (central Italy)</title><title type="short" xml:lang="en">LAGO DI VICO (ITALY) SEDIMENT RECORD</title></titleGroup><creators><creator xml:id="au1" creatorRole="author" affiliationRef="#af1" corresponding="yes"><personName><givenNames>Biancamaria</givenNames><familyName>Narcisi</familyName></personName><contactDetails><email>narcisi@casaccia.enea,it</email></contactDetails></creator></creators><affiliationGroup><affiliation xml:id="af1" countryCode="IT" type="organization"><unparsedAffiliation>ENEA – C.R. Casaccia, C.P. 2400, 00100 Roma, Italy</unparsedAffiliation></affiliation></affiliationGroup><keywordGroup xml:lang="en" type="author"><keyword xml:id="kwd1">central Italy</keyword><keyword xml:id="kwd2">volcanic lake</keyword><keyword xml:id="kwd3">sediment analysis</keyword><keyword xml:id="kwd4">lake‐levels</keyword><keyword xml:id="kwd5">Late Quaternary</keyword></keywordGroup><fundingInfo><fundingAgency>European Union ARIDUSEUROMED Project</fundingAgency><fundingNumber>ENV4‐CT95‐0062</fundingNumber></fundingInfo><fundingInfo><fundingAgency>European Commission EUROMAARS Project</fundingAgency></fundingInfo><abstractGroup><abstract type="main" xml:lang="en"><title type="main">Abstract</title><p>A 15‐m‐long sediment core recovered from the Lago di Vico caldera lake in central Italy has been the subject of macrofacies description and sedimentological (organic carbon content, grain size and mineralogy) investigation. The results have been integrated with the pollen data from the same core in order to provide a regional climatic and environmental history, with inferences on past lake levels and on moisture and temperature regimes. Radiometric (<sup>14</sup>C and <sup>40</sup>Ar/<sup>39</sup>Ar) dating, biostratigraphical considerations and tephra analyses provide a chronological framework and indicate that the sequence spans the last 90 000 yr. Several moist periods have been identified that were characterised by enhanced weathering by hydrolysis of the catchment rocks. These alternated with relatively dry phases associated with lowering of lake‐levels. The lowest hydrolysis efficiency of the whole record, accompanied by notable aeolian deposition, was attained during the last glacial phase but moisture conditions were such that the lake‐level did not decrease, probably owing to reduced temperatures. Evidence for cool climate also emerges for the early Pleniglacial. The highest available moisture was achieved within the Holocene at 5 kyr BP. The Late Holocene does not show either increase of aridity or degradation of the vegetation cover, until at least Roman times. Copyright © 2001 John Wiley & Sons, Ltd.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Palaeoenvironmental and palaeoclimatic implications of the Late‐Quaternary sediment record of Vico volcanic lake (central Italy)</title></titleInfo><titleInfo type="abbreviated" lang="en"><title>LAGO DI VICO (ITALY) SEDIMENT RECORD</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Palaeoenvironmental and palaeoclimatic implications of the Late‐Quaternary sediment record of Vico volcanic lake (central Italy)</title></titleInfo><name type="personal"><namePart type="given">Biancamaria</namePart><namePart type="family">Narcisi</namePart><affiliation>ENEA – C.R. Casaccia, C.P. 2400, 00100 Roma, Italy</affiliation><affiliation>ENEA‐C.R. Casaccia, PO Box 2400, I‐00100 Rome, Italy.</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>John Wiley & Sons, Ltd.</publisher><place><placeTerm type="text">Chichester, UK</placeTerm></place><dateIssued encoding="w3cdtf">2001-03</dateIssued><dateCaptured encoding="w3cdtf">2000-06-01</dateCaptured><dateValid encoding="w3cdtf">2000-10-05</dateValid><copyrightDate encoding="w3cdtf">2001</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType><extent unit="figures">5</extent><extent unit="references">67</extent></physicalDescription><abstract lang="en">A 15‐m‐long sediment core recovered from the Lago di Vico caldera lake in central Italy has been the subject of macrofacies description and sedimentological (organic carbon content, grain size and mineralogy) investigation. The results have been integrated with the pollen data from the same core in order to provide a regional climatic and environmental history, with inferences on past lake levels and on moisture and temperature regimes. Radiometric (14C and 40Ar/39Ar) dating, biostratigraphical considerations and tephra analyses provide a chronological framework and indicate that the sequence spans the last 90 000 yr. Several moist periods have been identified that were characterised by enhanced weathering by hydrolysis of the catchment rocks. These alternated with relatively dry phases associated with lowering of lake‐levels. The lowest hydrolysis efficiency of the whole record, accompanied by notable aeolian deposition, was attained during the last glacial phase but moisture conditions were such that the lake‐level did not decrease, probably owing to reduced temperatures. Evidence for cool climate also emerges for the early Pleniglacial. The highest available moisture was achieved within the Holocene at 5 kyr BP. The Late Holocene does not show either increase of aridity or degradation of the vegetation cover, until at least Roman times. Copyright © 2001 John Wiley & Sons, Ltd.</abstract><note type="funding">European Union ARIDUSEUROMED Project - No. ENV4‐CT95‐0062; </note><note type="funding">European Commission EUROMAARS Project</note><subject lang="en"><genre>keywords</genre><topic>central Italy</topic><topic>volcanic lake</topic><topic>sediment analysis</topic><topic>lake‐levels</topic><topic>Late Quaternary</topic></subject><relatedItem type="host"><titleInfo><title>Journal of Quaternary Science</title><subTitle>Published for the Quaternary Research Association</subTitle></titleInfo><titleInfo type="abbreviated"><title>J. Quaternary Sci.</title></titleInfo><genre type="journal">journal</genre><subject><genre>article-category</genre><topic>Research Article</topic></subject><identifier type="ISSN">0267-8179</identifier><identifier type="eISSN">1099-1417</identifier><identifier type="DOI">10.1002/(ISSN)1099-1417</identifier><identifier type="PublisherID">JQS</identifier><part><date>2001</date><detail type="volume"><caption>vol.</caption><number>16</number></detail><detail type="issue"><caption>no.</caption><number>3</number></detail><extent unit="pages"><start>245</start><end>255</end><total>11</total></extent></part></relatedItem><identifier type="istex">F300BB34EAADC5698B95598EC9B1E321FC6DDE33</identifier><identifier type="DOI">10.1002/jqs.594</identifier><identifier type="ArticleID">JQS594</identifier><accessCondition type="use and reproduction" contentType="copyright">Copyright © 2001 John Wiley & Sons, Ltd.</accessCondition><recordInfo><recordContentSource>WILEY</recordContentSource><recordOrigin>John Wiley & Sons, Ltd.</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Rhénanie/explor/UnivTrevesV1/Data/Istex/Corpus
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 001816 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/Istex/Corpus/biblio.hfd -nk 001816 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien
|wiki= Wicri/Rhénanie
|area= UnivTrevesV1
|flux= Istex
|étape= Corpus
|type= RBID
|clé= ISTEX:F300BB34EAADC5698B95598EC9B1E321FC6DDE33
|texte= Palaeoenvironmental and palaeoclimatic implications of the Late‐Quaternary sediment record of Vico volcanic lake (central Italy)
}}
| This area was generated with Dilib version V0.6.31. |  |