Sedimentology, dating and palaeoclimatic interpretation of A 76.3 ka record from Lago Grande di Monticchio, southern Italy
Identifieur interne : 001888 ( Istex/Corpus ); précédent : 001887; suivant : 001889Sedimentology, dating and palaeoclimatic interpretation of A 76.3 ka record from Lago Grande di Monticchio, southern Italy
Auteurs : Bernd Zolitschka ; Jörg F. W. NegendankSource :
- Quaternary Science Reviews [ 0277-3791 ] ; 1996.
Abstract
Detailed sedimentological and microstratigraphical investigations of lacustrine sediments from Lago Grande di Monticchio (southern Italy) provide a time scale based on rates of sedimentation obtained from annual laminations. Although not annually laminated throughout, a time scale covering the last 76.3 ka is available by interpolation of sedimentation rates. Results of this chronology agree with radiocarbon dates, and with Ar Ar dates on tephra layers from the same lacustrine sediment sequence. Occurrence of varves in combination with physical and geochemical properties are related to variations in the trophic state of the lake and to changing runoff, both controlled by palaeoclimatic conditions. Water depth was relatively shallow with dominating bioturbation and only few varves preserved for most of the Pleniglacial. A marked increase in precipitation and related runoff characterises the early Last Glacial Maximum when water depth reached a maximum and clastic varves were deposited. Subsequently water depth was shallower again. A drastic change towards nutrient rich conditions occurred at the Pleistocene/Holocene transition. During the Holocene organic varves were deposited. Two periods with higher organic productivity were recognised prior to the Last Glacial Maximum around 50 ka and 73 ka. These intervals are interpreted as the result of interstadial conditions. The oldes of the two events shows laminations comparable to those at the Glacial/Holocene transition. The periods with increased minerogenic influx may be characterised as stadial conditions, lasting from 14–40 ka and from 50–73 ka.
Url:
DOI: 10.1016/0277-3791(95)00022-4
Links to Exploration step
ISTEX:765833E9305E27F077BEB6BFC086DB37065854E7Le document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title>Sedimentology, dating and palaeoclimatic interpretation of A 76.3 ka record from Lago Grande di Monticchio, southern Italy</title>
<author><name sortKey="Zolitschka, Bernd" sort="Zolitschka, Bernd" uniqKey="Zolitschka B" first="Bernd" last="Zolitschka">Bernd Zolitschka</name>
<affiliation><mods:affiliation>Fachbereich VI, Geologie, Universität Trier, D-54286 Trier, Germany</mods:affiliation>
</affiliation>
<affiliation><mods:affiliation>GeoForschungsZentrum Postdam, Telegrafenberg A26, D-14473 Potsdam, Germany</mods:affiliation>
</affiliation>
</author>
<author><name sortKey="Negendank, Jorg F W" sort="Negendank, Jorg F W" uniqKey="Negendank J" first="Jörg F. W." last="Negendank">Jörg F. W. Negendank</name>
<affiliation><mods:affiliation>GeoForschungsZentrum Postdam, Telegrafenberg A26, D-14473 Potsdam, Germany</mods:affiliation>
</affiliation>
</author>
</titleStmt>
<publicationStmt><idno type="wicri:source">ISTEX</idno>
<idno type="RBID">ISTEX:765833E9305E27F077BEB6BFC086DB37065854E7</idno>
<date when="1996" year="1996">1996</date>
<idno type="doi">10.1016/0277-3791(95)00022-4</idno>
<idno type="url">https://api.istex.fr/document/765833E9305E27F077BEB6BFC086DB37065854E7/fulltext/pdf</idno>
<idno type="wicri:Area/Istex/Corpus">001888</idno>
<idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">001888</idno>
</publicationStmt>
<sourceDesc><biblStruct><analytic><title level="a">Sedimentology, dating and palaeoclimatic interpretation of A 76.3 ka record from Lago Grande di Monticchio, southern Italy</title>
<author><name sortKey="Zolitschka, Bernd" sort="Zolitschka, Bernd" uniqKey="Zolitschka B" first="Bernd" last="Zolitschka">Bernd Zolitschka</name>
<affiliation><mods:affiliation>Fachbereich VI, Geologie, Universität Trier, D-54286 Trier, Germany</mods:affiliation>
</affiliation>
<affiliation><mods:affiliation>GeoForschungsZentrum Postdam, Telegrafenberg A26, D-14473 Potsdam, Germany</mods:affiliation>
</affiliation>
</author>
<author><name sortKey="Negendank, Jorg F W" sort="Negendank, Jorg F W" uniqKey="Negendank J" first="Jörg F. W." last="Negendank">Jörg F. W. Negendank</name>
<affiliation><mods:affiliation>GeoForschungsZentrum Postdam, Telegrafenberg A26, D-14473 Potsdam, Germany</mods:affiliation>
</affiliation>
</author>
</analytic>
<monogr></monogr>
<series><title level="j">Quaternary Science Reviews</title>
<title level="j" type="abbrev">JQSR</title>
<idno type="ISSN">0277-3791</idno>
<imprint><publisher>ELSEVIER</publisher>
<date type="published" when="1996">1996</date>
<biblScope unit="volume">15</biblScope>
<biblScope unit="issue">2–3</biblScope>
<biblScope unit="page" from="101">101</biblScope>
<biblScope unit="page" to="112">112</biblScope>
</imprint>
<idno type="ISSN">0277-3791</idno>
</series>
<idno type="istex">765833E9305E27F077BEB6BFC086DB37065854E7</idno>
<idno type="DOI">10.1016/0277-3791(95)00022-4</idno>
<idno type="PII">0277-3791(95)00022-4</idno>
</biblStruct>
</sourceDesc>
<seriesStmt><idno type="ISSN">0277-3791</idno>
</seriesStmt>
</fileDesc>
<profileDesc><textClass></textClass>
<langUsage><language ident="en">en</language>
</langUsage>
</profileDesc>
</teiHeader>
<front><div type="abstract" xml:lang="en">Detailed sedimentological and microstratigraphical investigations of lacustrine sediments from Lago Grande di Monticchio (southern Italy) provide a time scale based on rates of sedimentation obtained from annual laminations. Although not annually laminated throughout, a time scale covering the last 76.3 ka is available by interpolation of sedimentation rates. Results of this chronology agree with radiocarbon dates, and with Ar Ar dates on tephra layers from the same lacustrine sediment sequence. Occurrence of varves in combination with physical and geochemical properties are related to variations in the trophic state of the lake and to changing runoff, both controlled by palaeoclimatic conditions. Water depth was relatively shallow with dominating bioturbation and only few varves preserved for most of the Pleniglacial. A marked increase in precipitation and related runoff characterises the early Last Glacial Maximum when water depth reached a maximum and clastic varves were deposited. Subsequently water depth was shallower again. A drastic change towards nutrient rich conditions occurred at the Pleistocene/Holocene transition. During the Holocene organic varves were deposited. Two periods with higher organic productivity were recognised prior to the Last Glacial Maximum around 50 ka and 73 ka. These intervals are interpreted as the result of interstadial conditions. The oldes of the two events shows laminations comparable to those at the Glacial/Holocene transition. The periods with increased minerogenic influx may be characterised as stadial conditions, lasting from 14–40 ka and from 50–73 ka.</div>
</front>
</TEI>
<istex><corpusName>elsevier</corpusName>
<author><json:item><name>Bernd Zolitschka</name>
<affiliations><json:string>Fachbereich VI, Geologie, Universität Trier, D-54286 Trier, Germany</json:string>
<json:string>GeoForschungsZentrum Postdam, Telegrafenberg A26, D-14473 Potsdam, Germany</json:string>
</affiliations>
</json:item>
<json:item><name>Jörg F.W. Negendank</name>
<affiliations><json:string>GeoForschungsZentrum Postdam, Telegrafenberg A26, D-14473 Potsdam, Germany</json:string>
</affiliations>
</json:item>
</author>
<language><json:string>eng</json:string>
</language>
<originalGenre><json:string>Full-length article</json:string>
</originalGenre>
<abstract>Detailed sedimentological and microstratigraphical investigations of lacustrine sediments from Lago Grande di Monticchio (southern Italy) provide a time scale based on rates of sedimentation obtained from annual laminations. Although not annually laminated throughout, a time scale covering the last 76.3 ka is available by interpolation of sedimentation rates. Results of this chronology agree with radiocarbon dates, and with Ar Ar dates on tephra layers from the same lacustrine sediment sequence. Occurrence of varves in combination with physical and geochemical properties are related to variations in the trophic state of the lake and to changing runoff, both controlled by palaeoclimatic conditions. Water depth was relatively shallow with dominating bioturbation and only few varves preserved for most of the Pleniglacial. A marked increase in precipitation and related runoff characterises the early Last Glacial Maximum when water depth reached a maximum and clastic varves were deposited. Subsequently water depth was shallower again. A drastic change towards nutrient rich conditions occurred at the Pleistocene/Holocene transition. During the Holocene organic varves were deposited. Two periods with higher organic productivity were recognised prior to the Last Glacial Maximum around 50 ka and 73 ka. These intervals are interpreted as the result of interstadial conditions. The oldes of the two events shows laminations comparable to those at the Glacial/Holocene transition. The periods with increased minerogenic influx may be characterised as stadial conditions, lasting from 14–40 ka and from 50–73 ka.</abstract>
<qualityIndicators><score>7.796</score>
<pdfVersion>1.2</pdfVersion>
<pdfPageSize>591 x 843 pts</pdfPageSize>
<refBibsNative>true</refBibsNative>
<keywordCount>0</keywordCount>
<abstractCharCount>1621</abstractCharCount>
<pdfWordCount>5473</pdfWordCount>
<pdfCharCount>37732</pdfCharCount>
<pdfPageCount>12</pdfPageCount>
<abstractWordCount>233</abstractWordCount>
</qualityIndicators>
<title>Sedimentology, dating and palaeoclimatic interpretation of A 76.3 ka record from Lago Grande di Monticchio, southern Italy</title>
<pii><json:string>0277-3791(95)00022-4</json:string>
</pii>
<refBibs><json:item><author><json:item><name>R.Y. Anderson</name>
</json:item>
<json:item><name>E.B. Nuhfer</name>
</json:item>
<json:item><name>W.E. Dean</name>
</json:item>
</author>
<host><volume>13</volume>
<pages><last>352</last>
<first>348</first>
</pages>
<author></author>
<title>Geology</title>
</host>
<title>Sedimentation in a blast-zone lake at Mount St. Helens, Washington — Implications for varve formation</title>
</json:item>
<json:item><author><json:item><name>J.L.de Beaulieu</name>
</json:item>
<json:item><name>M. Reille</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 Echet, near Lyon, France</title>
</json:item>
<json:item><author><json:item><name>F.P. Bonadonna</name>
</json:item>
<json:item><name>D. Brocchini</name>
</json:item>
<json:item><name>M.A. Laurenzi</name>
</json:item>
<json:item><name>C. Principe</name>
</json:item>
<json:item><name>G. Ferrara</name>
</json:item>
</author>
<host><pages><first>13</first>
</pages>
<author></author>
<title>Symposium — Quaternary Stratigraphy in Volcanic Areas</title>
</host>
<title>Mt. Vulture volcano chronostratigraphy and palaeogeographic implications</title>
</json:item>
<json:item><author><json:item><name>G. Capaldi</name>
</json:item>
<json:item><name>L. Civetta</name>
</json:item>
<json:item><name>P.Y. Gillot</name>
</json:item>
</author>
<host><volume>40</volume>
<pages><last>44</last>
<first>25</first>
</pages>
<author></author>
<title>Rend. Soc. Ital. Min. Petr.</title>
</host>
<title>Geochronology of the Plio-Pleistocene volcanic rocks from southern Italy</title>
</json:item>
<json:item><author><json:item><name>K.M. Creer</name>
</json:item>
</author>
<host><author></author>
<title>Quaternary Proceedings</title>
</host>
<serie><author></author>
<title>Quaternary Proceedings</title>
</serie>
<title>Dating of a maar lake sediment sequence covering the last glacial cycle</title>
</json:item>
<json:item><author><json:item><name>K.M. Creer</name>
</json:item>
<json:item><name>I. Turton</name>
</json:item>
<json:item><name>A. Morris</name>
</json:item>
</author>
<host><volume>15</volume>
<pages><last>188</last>
<first>167</first>
</pages>
<author></author>
<title>Quaternary Science Reviews</title>
</host>
<title>Proxy climate and paleointensity records spanning the last 65 ka from Lago Grande di Monticchio, southern Italy</title>
</json:item>
<json:item><author><json:item><name>W. Dansgaard</name>
</json:item>
<json:item><name>S.J. Johnson</name>
</json:item>
<json:item><name>H.B. Clausen</name>
</json:item>
<json:item><name>D. Dahl-Jensen</name>
</json:item>
<json:item><name>N.S. Gundestrup</name>
</json:item>
<json:item><name>C.U. Hammer</name>
</json:item>
<json:item><name>C.S. Hvidberg</name>
</json:item>
<json:item><name>J.P. Steffensen</name>
</json:item>
<json:item><name>A.E. Sveinbjörnsdottir</name>
</json:item>
<json:item><name>J. Jouzel</name>
</json:item>
<json:item><name>G. Bond</name>
</json:item>
</author>
<host><volume>364</volume>
<pages><last>220</last>
<first>218</first>
</pages>
<author></author>
<title>Nature</title>
</host>
<title>Evidence for general instability of past climate from a 250-kyr ice-core record</title>
</json:item>
<json:item><author><json:item><name>M. De Fino</name>
</json:item>
<json:item><name>L. La Volpe</name>
</json:item>
<json:item><name>A. Peccerillo</name>
</json:item>
<json:item><name>G. Piccarreta</name>
</json:item>
<json:item><name>G. Poli</name>
</json:item>
</author>
<host><volume>92</volume>
<pages><last>145</last>
<first>135</first>
</pages>
<author></author>
<title>Contributions in Mineralogy and Petrography</title>
</host>
<title>Petrogenesis of Mt. Vulture volcano: inferences from mineral chemistry, major and trace element data</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>
<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>49</volume>
<pages><last>108</last>
<first>95</first>
</pages>
<author></author>
<title>Lecture Notes in Earth Sciences</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>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><author><json:item><name>J.E. Guest</name>
</json:item>
<json:item><name>A.M. Duncan</name>
</json:item>
<json:item><name>D.K. Chester</name>
</json:item>
</author>
<host><volume>50</volume>
<pages><last>257</last>
<first>244</first>
</pages>
<author></author>
<title>Bulletin of Volcanology</title>
</host>
<title>Monte Vulture volcano (Basilicata, Italy): An analysis of morphology and volcanoclastic facies</title>
</json:item>
<json:item><author><json:item><name>I. Hajdas</name>
</json:item>
<json:item><name>S.D. Ivy</name>
</json:item>
<json:item><name>J. Beer</name>
</json:item>
<json:item><name>G. Bonani</name>
</json:item>
<json:item><name>D. Imboden</name>
</json:item>
<json:item><name>A.F. Lotter</name>
</json:item>
<json:item><name>M. Sturm</name>
</json:item>
<json:item><name>M. Suter</name>
</json:item>
</author>
<host><volume>9</volume>
<pages><last>116</last>
<first>107</first>
</pages>
<author></author>
<title>Climate Dynamics</title>
</host>
<title>AMS radiocarbon dating and varve chronology of Lake Soppensee: 6000 to 12000 14C years BP</title>
</json:item>
<json:item><author><json:item><name>I. Hajdas</name>
</json:item>
<json:item><name>B. Zolitschka</name>
</json:item>
<json:item><name>S.D. Ivy</name>
</json:item>
<json:item><name>J. Beer</name>
</json:item>
<json:item><name>G. Bonani</name>
</json:item>
<json:item><name>S.A.D. Leroy</name>
</json:item>
<json:item><name>J.F.W. Negendank</name>
</json:item>
<json:item><name>M. Ramrath</name>
</json:item>
</author>
<host><volume>14</volume>
<pages><last>143</last>
<first>137</first>
</pages>
<author></author>
<title>Quaternary Science Reviews</title>
</host>
<title>AMS radiocarbon dating of annually laminated sediments from Lake Holzmaar, Germany</title>
</json:item>
<json:item><author><json:item><name>M.A. Laurenzi</name>
</json:item>
<json:item><name>D.I. Brocchini</name>
</json:item>
<json:item><name>C. Principe</name>
</json:item>
<json:item><name>G. Ferrara</name>
</json:item>
</author>
<host><volume>5</volume>
<pages><last>573</last>
<first>572</first>
</pages>
<author></author>
<title>Terra Abstracts</title>
</host>
<title>Mt. Vulture volcano stratigraphy and the effectiveness of dating young phlogopites</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>G. Dai Pra</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 Casiglione crater, Roma</title>
</json:item>
<json:item><author><json:item><name>J.F.W. Negendank</name>
</json:item>
<json:item><name>B. Zolitschka</name>
</json:item>
</author>
<host><author></author>
<title>Lecture Notes in Earth Sciences</title>
</host>
<serie><author></author>
<title>Lecture Notes in Earth Sciences</title>
</serie>
<title>Palaeolimnology of European maar lakes</title>
</json:item>
<json:item><author><json:item><name>J.F.W. Negendank</name>
</json:item>
<json:item><name>B. Zolitschka</name>
</json:item>
</author>
<host><volume>1/94</volume>
<pages><last>75</last>
<first>70</first>
</pages>
<author></author>
<title>Terra Nostra</title>
</host>
<title>The tephra layers of the 76,000 year record of Lago Grande di Monticchio (Basilicata, Italy)</title>
</json:item>
<json:item><author><json:item><name>A. Newton</name>
</json:item>
<json:item><name>A. Dugmore</name>
</json:item>
</author>
<host><volume>49</volume>
<pages><last>348</last>
<first>333</first>
</pages>
<author></author>
<title>Lecture Notes in Earth Sciences</title>
</host>
<title>Tephrochronology of core C from Lago Grande di Monticchio (southern Italy)</title>
</json:item>
<json:item><author><json:item><name>F. Niessen</name>
</json:item>
<json:item><name>A. Lami</name>
</json:item>
<json:item><name>P. Guilizzoni</name>
</json:item>
</author>
<host><volume>49</volume>
<pages><last>148</last>
<first>129</first>
</pages>
<author></author>
<title>Lecture Notes in Earth Sciences</title>
</host>
<title>Climatic and tectonic effects on sedimentation in Central Italian volcano lakes (Latium) — Implications from high resolution seismic profiles</title>
</json:item>
<json:item><author><json:item><name>I.U. Olsson</name>
</json:item>
</author>
<host><volume>214</volume>
<pages><last>34</last>
<first>25</first>
</pages>
<author></author>
<title>Hydrobiologia</title>
</host>
<title>Accuracy and precision in sediment chronology</title>
</json:item>
<json:item><author><json:item><name>H. Pichler</name>
</json:item>
</author>
<host><volume>83</volume>
<pages><first>271</first>
</pages>
<author></author>
<title>Sammlung geologischer Führer</title>
</host>
<title>Italienische Vulkan-Gebiete V.</title>
</json:item>
<json:item><author><json:item><name>M. Reille</name>
</json:item>
<json:item><name>Beaulieu J.-L. de</name>
</json:item>
</author>
<host><volume>80</volume>
<pages><last>48</last>
<first>35</first>
</pages>
<author></author>
<title>Palaeogeography, Palaeoclimatology, Palaeoecology</title>
</host>
<title>Pollen analysis of a long upper Pleistocene continental sequence in a Velay maar (Massif Central, France)</title>
</json:item>
<json:item><author><json:item><name>C. Robinson</name>
</json:item>
</author>
<host><author></author>
<title>Ph.D. thesis</title>
</host>
<serie><author></author>
<title>Ph.D. thesis</title>
</serie>
<title>Lago Grande di Monticchio: A palaeoenvironmental reconstruction from sediment geochemistry</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: A long record of environmental change illustrated by sediment geochemistry</title>
</json:item>
<json:item><author><json:item><name>C. Robinson</name>
</json:item>
<json:item><name>G.B. Shimmield</name>
</json:item>
<json:item><name>K.M. Creer</name>
</json:item>
</author>
<host><volume>49</volume>
<pages><last>332</last>
<first>317</first>
</pages>
<author></author>
<title>Lecture Notes in Earth Sciences</title>
</host>
<title>Geochemistry of Lago Grande di Monticchio (southern Italy)</title>
</json:item>
<json:item><author><json:item><name>G.E. Sigvaldason</name>
</json:item>
<json:item><name>K. Annertz</name>
</json:item>
<json:item><name>M. Nilsson</name>
</json:item>
</author>
<host><volume>54</volume>
<pages><last>392</last>
<first>385</first>
</pages>
<author></author>
<title>Bulletin of Volcanology</title>
</host>
<title>Effect of glacier loading/deloading on volcanism: Postglacial volcanic production rate of the Dyngjufjöll area, central Iceland</title>
</json:item>
<json:item><author><json:item><name>N. Thouveny</name>
</json:item>
<json:item><name>J.-L. de Beaulieu</name>
</json:item>
<json:item><name>E. Bonifay</name>
</json:item>
<json:item><name>K.M. Creer</name>
</json:item>
<json:item><name>J. Guiot</name>
</json:item>
<json:item><name>M. Icole</name>
</json:item>
<json:item><name>S. Johnsen</name>
</json:item>
<json:item><name>J. Jouzel</name>
</json:item>
<json:item><name>M. Reille</name>
</json:item>
<json:item><name>T. Williams</name>
</json:item>
<json:item><name>D. Williamson</name>
</json:item>
</author>
<host><volume>371</volume>
<pages><last>506</last>
<first>503</first>
</pages>
<author></author>
<title>Nature</title>
</host>
<title>Climate variations in Europe over the past 140 kyr deduced from rock magnetism</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>Lecture Notes in Earth Sciences</title>
</host>
<title>Sedimentology and palaeoenvironment from the maar Lac du Bouchet for the last climatic cycle, 0–120,000 years (Massif Central, France)</title>
</json:item>
<json:item><author><json:item><name>I. Turton</name>
</json:item>
</author>
<host><author></author>
<title>Ph.D. thesis</title>
</host>
<serie><author></author>
<title>Ph.D. thesis</title>
</serie>
<title>Temporal and spatial variations of the geomagnetic field, up to a timescale of 105 years</title>
</json:item>
<json:item><author><json:item><name>I. Turton</name>
</json:item>
</author>
<host><volume>49</volume>
<pages><last>392</last>
<first>377</first>
</pages>
<author></author>
<title>Lecture Notes in Earth Sciences</title>
</host>
<title>Palaeomagnetic investigations of Lago Grande di Monticchio (southern Italy)</title>
</json:item>
<json:item><author><json:item><name>W.A. Watts</name>
</json:item>
</author>
<host><volume>142</volume>
<pages><last>499</last>
<first>491</first>
</pages>
<author></author>
<title>Journal of the Geological Society of London</title>
</host>
<title>A long pollen record from Laghi di Monticchio, southern Italy; a preliminary account</title>
</json:item>
<json:item><author><json:item><name>W.A. Watts</name>
</json:item>
<json:item><name>J.R.M. Allen</name>
</json:item>
<json:item><name>B. Huntley</name>
</json:item>
</author>
<host><volume>15</volume>
<author></author>
<title>Quaternary Science Reviews</title>
</host>
<title>Vegetation history and climate of the last 15,000 years at Laghi di Monticchio, southern Italy</title>
</json:item>
<json:item><author><json:item><name>W.A. Watts</name>
</json:item>
<json:item><name>J.R.M. Allen</name>
</json:item>
<json:item><name>B. Huntley</name>
</json:item>
</author>
<host><volume>15</volume>
<author></author>
<title>Quaternary Science Reviews</title>
</host>
<title>Vegetation history and climate of the last glacial period (73,000 to 12,000 years before present) at Laghi di Monticchio, southern Italy</title>
</json:item>
<json:item><author><json:item><name>B. Zolitschka</name>
</json:item>
</author>
<host><volume>60</volume>
<pages><last>226</last>
<first>1</first>
</pages>
<author></author>
<title>Documenta Naturae</title>
</host>
<title>Spätquartäre jahreszeitlich geschichtete Seesedimente ausgewählter Eifelmaare</title>
</json:item>
<json:item><author><json:item><name>B. Zolitschka</name>
</json:item>
</author>
<host><volume>214</volume>
<pages><last>61</last>
<first>59</first>
</pages>
<author></author>
<title>Hydrobiologia</title>
</host>
<title>Absolute dating of late Quaternary sediments by high resolution varve chronology</title>
</json:item>
<json:item><author><json:item><name>B. Zolitschka</name>
</json:item>
<json:item><name>J.F.W. Negendank</name>
</json:item>
</author>
<host><volume>49</volume>
<pages><last>288</last>
<first>277</first>
</pages>
<author></author>
<title>Lecture Notes in Earth Sciences</title>
</host>
<title>Lago Grande di Monticchio (southern Italy) — A high resolution sedimentary record of the last 70,000 years</title>
</json:item>
<json:item><author><json:item><name>B. Zolitschka</name>
</json:item>
<json:item><name>J.F.W. Negendank</name>
</json:item>
</author>
<host><volume>1/49</volume>
<pages><last>69</last>
<first>64</first>
</pages>
<author></author>
<title>Terra Nostra</title>
</host>
<title>Sedimentological studies on lacustrine sediments from Lago Grande di Monticchio (Italy) as a source of palaeoclimatic proxy data for the last 76,000 years</title>
</json:item>
</refBibs>
<genre><json:string>research-article</json:string>
</genre>
<serie><volume>1</volume>
<pages><last>87</last>
<first>75</first>
</pages>
<language><json:string>unknown</json:string>
</language>
<title>Quaternary Proceedings</title>
</serie>
<host><volume>15</volume>
<pii><json:string>S0277-3791(00)X0001-7</json:string>
</pii>
<pages><last>112</last>
<first>101</first>
</pages>
<issn><json:string>0277-3791</json:string>
</issn>
<issue>2–3</issue>
<genre><json:string>journal</json:string>
</genre>
<language><json:string>unknown</json:string>
</language>
<title>Quaternary Science Reviews</title>
<publicationDate>1996</publicationDate>
</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>1996</publicationDate>
<copyrightDate>1996</copyrightDate>
<doi><json:string>10.1016/0277-3791(95)00022-4</json:string>
</doi>
<id>765833E9305E27F077BEB6BFC086DB37065854E7</id>
<score>0.5972127</score>
<fulltext><json:item><extension>pdf</extension>
<original>true</original>
<mimetype>application/pdf</mimetype>
<uri>https://api.istex.fr/document/765833E9305E27F077BEB6BFC086DB37065854E7/fulltext/pdf</uri>
</json:item>
<json:item><extension>zip</extension>
<original>false</original>
<mimetype>application/zip</mimetype>
<uri>https://api.istex.fr/document/765833E9305E27F077BEB6BFC086DB37065854E7/fulltext/zip</uri>
</json:item>
<istex:fulltextTEI uri="https://api.istex.fr/document/765833E9305E27F077BEB6BFC086DB37065854E7/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a">Sedimentology, dating and palaeoclimatic interpretation of A 76.3 ka record from Lago Grande di Monticchio, southern Italy</title>
</titleStmt>
<publicationStmt><authority>ISTEX</authority>
<publisher>ELSEVIER</publisher>
<availability><p>ELSEVIER</p>
</availability>
<date>1996</date>
</publicationStmt>
<sourceDesc><biblStruct type="inbook"><analytic><title level="a">Sedimentology, dating and palaeoclimatic interpretation of A 76.3 ka record from Lago Grande di Monticchio, southern Italy</title>
<author xml:id="author-1"><persName><forename type="first">Bernd</forename>
<surname>Zolitschka</surname>
</persName>
<affiliation>Fachbereich VI, Geologie, Universität Trier, D-54286 Trier, Germany</affiliation>
<affiliation>GeoForschungsZentrum Postdam, Telegrafenberg A26, D-14473 Potsdam, Germany</affiliation>
</author>
<author xml:id="author-2"><persName><forename type="first">Jörg F.W.</forename>
<surname>Negendank</surname>
</persName>
<affiliation>GeoForschungsZentrum Postdam, Telegrafenberg A26, D-14473 Potsdam, Germany</affiliation>
</author>
</analytic>
<monogr><title level="j">Quaternary Science Reviews</title>
<title level="j" type="abbrev">JQSR</title>
<idno type="pISSN">0277-3791</idno>
<idno type="PII">S0277-3791(00)X0001-7</idno>
<imprint><publisher>ELSEVIER</publisher>
<date type="published" when="1996"></date>
<biblScope unit="volume">15</biblScope>
<biblScope unit="issue">2–3</biblScope>
<biblScope unit="page" from="101">101</biblScope>
<biblScope unit="page" to="112">112</biblScope>
</imprint>
</monogr>
<idno type="istex">765833E9305E27F077BEB6BFC086DB37065854E7</idno>
<idno type="DOI">10.1016/0277-3791(95)00022-4</idno>
<idno type="PII">0277-3791(95)00022-4</idno>
</biblStruct>
</sourceDesc>
</fileDesc>
<profileDesc><creation><date>1996</date>
</creation>
<langUsage><language ident="en">en</language>
</langUsage>
<abstract xml:lang="en"><p>Detailed sedimentological and microstratigraphical investigations of lacustrine sediments from Lago Grande di Monticchio (southern Italy) provide a time scale based on rates of sedimentation obtained from annual laminations. Although not annually laminated throughout, a time scale covering the last 76.3 ka is available by interpolation of sedimentation rates. Results of this chronology agree with radiocarbon dates, and with Ar Ar dates on tephra layers from the same lacustrine sediment sequence. Occurrence of varves in combination with physical and geochemical properties are related to variations in the trophic state of the lake and to changing runoff, both controlled by palaeoclimatic conditions. Water depth was relatively shallow with dominating bioturbation and only few varves preserved for most of the Pleniglacial. A marked increase in precipitation and related runoff characterises the early Last Glacial Maximum when water depth reached a maximum and clastic varves were deposited. Subsequently water depth was shallower again. A drastic change towards nutrient rich conditions occurred at the Pleistocene/Holocene transition. During the Holocene organic varves were deposited. Two periods with higher organic productivity were recognised prior to the Last Glacial Maximum around 50 ka and 73 ka. These intervals are interpreted as the result of interstadial conditions. The oldes of the two events shows laminations comparable to those at the Glacial/Holocene transition. The periods with increased minerogenic influx may be characterised as stadial conditions, lasting from 14–40 ka and from 50–73 ka.</p>
</abstract>
</profileDesc>
<revisionDesc><change when="1996">Published</change>
</revisionDesc>
</teiHeader>
</istex:fulltextTEI>
<json:item><extension>txt</extension>
<original>false</original>
<mimetype>text/plain</mimetype>
<uri>https://api.istex.fr/document/765833E9305E27F077BEB6BFC086DB37065854E7/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"><item-info><jid>JQSR</jid>
<aid>95000224</aid>
<ce:pii>0277-3791(95)00022-4</ce:pii>
<ce:doi>10.1016/0277-3791(95)00022-4</ce:doi>
<ce:copyright type="unknown" year="1996"></ce:copyright>
</item-info>
<head><ce:title>Sedimentology, dating and palaeoclimatic interpretation of A 76.3 ka record from Lago Grande di Monticchio, southern Italy</ce:title>
<ce:author-group><ce:author><ce:given-name>Bernd</ce:given-name>
<ce:surname>Zolitschka</ce:surname>
<ce:cross-ref refid="AFF1"><ce:sup>∗</ce:sup>
</ce:cross-ref>
<ce:cross-ref refid="AFF2"><ce:sup>†</ce:sup>
</ce:cross-ref>
</ce:author>
<ce:author><ce:given-name>Jörg F.W.</ce:given-name>
<ce:surname>Negendank</ce:surname>
<ce:cross-ref refid="AFF2"><ce:sup>†</ce:sup>
</ce:cross-ref>
</ce:author>
<ce:affiliation id="AFF1"><ce:label>a</ce:label>
<ce:textfn>Fachbereich VI, Geologie, Universität Trier, D-54286 Trier, Germany</ce:textfn>
</ce:affiliation>
<ce:affiliation id="AFF2"><ce:label>b</ce:label>
<ce:textfn>GeoForschungsZentrum Postdam, Telegrafenberg A26, D-14473 Potsdam, Germany</ce:textfn>
</ce:affiliation>
</ce:author-group>
<ce:abstract><ce:section-title>Abstract</ce:section-title>
<ce:abstract-sec><ce:simple-para>Detailed sedimentological and microstratigraphical investigations of lacustrine sediments from Lago Grande di Monticchio (southern Italy) provide a time scale based on rates of sedimentation obtained from annual laminations. Although not annually laminated throughout, a time scale covering the last 76.3 ka is available by interpolation of sedimentation rates. Results of this chronology agree with radiocarbon dates, and with <math altimg="si1.gif"><fr shape="sol"><nu><rm>Ar</rm>
</nu>
<de><rm>Ar</rm>
</de>
</fr>
</math>
dates on tephra layers from the same lacustrine sediment sequence. Occurrence of varves in combination with physical and geochemical properties are related to variations in the trophic state of the lake and to changing runoff, both controlled by palaeoclimatic conditions.</ce:simple-para>
<ce:simple-para>Water depth was relatively shallow with dominating bioturbation and only few varves preserved for most of the Pleniglacial. A marked increase in precipitation and related runoff characterises the early Last Glacial Maximum when water depth reached a maximum and clastic varves were deposited. Subsequently water depth was shallower again. A drastic change towards nutrient rich conditions occurred at the Pleistocene/Holocene transition. During the Holocene organic varves were deposited. Two periods with higher organic productivity were recognised prior to the Last Glacial Maximum around 50 ka and 73 ka. These intervals are interpreted as the result of interstadial conditions. The oldes of the two events shows laminations comparable to those at the Glacial/Holocene transition. The periods with increased minerogenic influx may be characterised as stadial conditions, lasting from 14–40 ka and from 50–73 ka.</ce:simple-para>
</ce:abstract-sec>
</ce:abstract>
</head>
</converted-article>
</istex:document>
</istex:metadataXml>
<mods version="3.6"><titleInfo><title>Sedimentology, dating and palaeoclimatic interpretation of A 76.3 ka record from Lago Grande di Monticchio, southern Italy</title>
</titleInfo>
<titleInfo type="alternative" contentType="CDATA"><title>Sedimentology, dating and palaeoclimatic interpretation of A 76.3 ka record from Lago Grande di Monticchio, southern Italy</title>
</titleInfo>
<name type="personal"><namePart type="given">Bernd</namePart>
<namePart type="family">Zolitschka</namePart>
<affiliation>Fachbereich VI, Geologie, Universität Trier, D-54286 Trier, Germany</affiliation>
<affiliation>GeoForschungsZentrum Postdam, Telegrafenberg A26, D-14473 Potsdam, Germany</affiliation>
<role><roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal"><namePart type="given">Jörg F.W.</namePart>
<namePart type="family">Negendank</namePart>
<affiliation>GeoForschungsZentrum Postdam, Telegrafenberg A26, D-14473 Potsdam, Germany</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">1996</dateIssued>
<copyrightDate encoding="w3cdtf">1996</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">Detailed sedimentological and microstratigraphical investigations of lacustrine sediments from Lago Grande di Monticchio (southern Italy) provide a time scale based on rates of sedimentation obtained from annual laminations. Although not annually laminated throughout, a time scale covering the last 76.3 ka is available by interpolation of sedimentation rates. Results of this chronology agree with radiocarbon dates, and with Ar Ar dates on tephra layers from the same lacustrine sediment sequence. Occurrence of varves in combination with physical and geochemical properties are related to variations in the trophic state of the lake and to changing runoff, both controlled by palaeoclimatic conditions. Water depth was relatively shallow with dominating bioturbation and only few varves preserved for most of the Pleniglacial. A marked increase in precipitation and related runoff characterises the early Last Glacial Maximum when water depth reached a maximum and clastic varves were deposited. Subsequently water depth was shallower again. A drastic change towards nutrient rich conditions occurred at the Pleistocene/Holocene transition. During the Holocene organic varves were deposited. Two periods with higher organic productivity were recognised prior to the Last Glacial Maximum around 50 ka and 73 ka. These intervals are interpreted as the result of interstadial conditions. The oldes of the two events shows laminations comparable to those at the Glacial/Holocene transition. The periods with increased minerogenic influx may be characterised as stadial conditions, lasting from 14–40 ka and from 50–73 ka.</abstract>
<relatedItem type="host"><titleInfo><title>Quaternary Science Reviews</title>
</titleInfo>
<titleInfo type="abbreviated"><title>JQSR</title>
</titleInfo>
<genre type="journal">journal</genre>
<originInfo><dateIssued encoding="w3cdtf">1996</dateIssued>
</originInfo>
<identifier type="ISSN">0277-3791</identifier>
<identifier type="PII">S0277-3791(00)X0001-7</identifier>
<part><date>1996</date>
<detail type="volume"><number>15</number>
<caption>vol.</caption>
</detail>
<detail type="issue"><number>2–3</number>
<caption>no.</caption>
</detail>
<extent unit="issue pages"><start>99</start>
<end>245</end>
</extent>
<extent unit="pages"><start>101</start>
<end>112</end>
</extent>
</part>
</relatedItem>
<identifier type="istex">765833E9305E27F077BEB6BFC086DB37065854E7</identifier>
<identifier type="DOI">10.1016/0277-3791(95)00022-4</identifier>
<identifier type="PII">0277-3791(95)00022-4</identifier>
<recordInfo><recordContentSource>ELSEVIER</recordContentSource>
</recordInfo>
</mods>
</metadata>
</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 001888 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/Istex/Corpus/biblio.hfd -nk 001888 | 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:765833E9305E27F077BEB6BFC086DB37065854E7 |texte= Sedimentology, dating and palaeoclimatic interpretation of A 76.3 ka record from Lago Grande di Monticchio, southern Italy }}
![]() | This area was generated with Dilib version V0.6.31. | ![]() |