Climatic transfer function from quaternary molluscs in European loess deposits
Identifieur interne : 000536 ( France/Analysis ); précédent : 000535; suivant : 000537Climatic transfer function from quaternary molluscs in European loess deposits
Auteurs : Denis-Didier Rousseau [France]Source :
- Quaternary Research [ 0033-5894 ] ; 1991.
Descripteurs français
English descriptors
- KwdEn :
- Abisko, Achenheim, Achenheim record, Achenheim sequence, Alsace, Analog, Analog climate, Annual precipitation, Assemblage, Atlantic cores, August, August precipitation, August temperatures, Climatic, Climatic cycles, Climatic parameters, Climatic variations, Columella columella, Correspondence analysis, Ecological tolerance, Factor analysis, Fauna, February, Fossil, Fossil assemblages, Global sample, Good agreement, Grande, Grande pile, Guiot, Homogeneous data, Human activities, Imbrie, Initial table, Insolation, Insolation signatures, Interglacial, Interglacial stages, Intermediate fauna, Isotope stages, Last years, Loess, Loess sequence, Lower values, Modern assemblages, Modern data, Modern precipitation regime, Modern value, Mollusc, Molluscan, Molluscan transfer, Multiple correlation coefficient, Multivariate analysis, Oceanic mechanisms, Oceanic results, Other hand, Pleniglacial stages, Pollen data, Precipitation, Precipitation estimates, Puissegur, Quaternary, Quaternary research, Radiometric dates, Second analysis, Specmap chronology, Standard error, Summer estimates, Summer precipitation, Summer temperatures, Summer values, Terrestrial molluscs, Theoretical contribution, Total number, Total variance, Transfer function, Transfer functions, Vertigo genesii, Vosges mountains, Western europe, Western side, Winter deviations, Winter estimates, Winter insolation, Winter precipitation, Winter temperatures.
- Teeft :
- Abisko, Achenheim, Achenheim record, Achenheim sequence, Alsace, Analog, Analog climate, Annual precipitation, Assemblage, Atlantic cores, August, August precipitation, August temperatures, Climatic, Climatic cycles, Climatic parameters, Climatic variations, Columella columella, Correspondence analysis, Ecological tolerance, Factor analysis, Fauna, February, Fossil, Fossil assemblages, Global sample, Good agreement, Grande, Grande pile, Guiot, Homogeneous data, Human activities, Imbrie, Initial table, Insolation, Insolation signatures, Interglacial, Interglacial stages, Intermediate fauna, Isotope stages, Last years, Loess, Loess sequence, Lower values, Modern assemblages, Modern data, Modern precipitation regime, Modern value, Mollusc, Molluscan, Molluscan transfer, Multiple correlation coefficient, Multivariate analysis, Oceanic mechanisms, Oceanic results, Other hand, Pleniglacial stages, Pollen data, Precipitation, Precipitation estimates, Puissegur, Quaternary, Quaternary research, Radiometric dates, Second analysis, Specmap chronology, Standard error, Summer estimates, Summer precipitation, Summer temperatures, Summer values, Terrestrial molluscs, Theoretical contribution, Total number, Total variance, Transfer function, Transfer functions, Vertigo genesii, Vosges mountains, Western europe, Western side, Winter deviations, Winter estimates, Winter insolation, Winter precipitation, Winter temperatures.
Abstract
Abstract: Correspondence and multiple regression analysis of terrestrial molluscs in the loess sections of Achenheim (Alsace, France) has permitted the reconstruction of climatic variations during the last three glacial-interglacial cycles back to 339,000 yr B.P. The sequence has been dated according to the SPECMAP chronology of Imbrie et al. (1984) and the fossil faunas have been calibrated in relation to recent assemblages sampled in defined ecological conditions in Sweden and France. Transfer functions that relate the abundances of different species to climate allow the reconstruction of temperature and precipitation. Estimates for the coldest (February) and warmest (August) months in present-day Alsace were obtained and variations in temperature between −13° and 2°C in winter and 10° and 17°C in summer were determined. These results are consistent with those yielded by transfer functions using other continental fossils. Estimates differ for past precipitation. Summer precipitation is always less than present (with values between 50 and 78 mm, while modern August values are 76 mm higher). Winter estimates are always higher than the present mean (between 76 and 33 mm, while the recent February value is 34 mm). Comparisons between cycles show that the climatic patterns described for one cycle cannot be strictly applied to the others. Comparisons have been made with the pollen stratigraphy of La Grande Pile, the nearest quantified sequence to Achenheim, and with some Atlantic cores in order to study the magnitude of deviations from modern mean values of the climatic parameters.
Url:
DOI: 10.1016/0033-5894(91)90025-Z
Affiliations:
Links toward previous steps (curation, corpus...)
- to stream Istex, to step Corpus: 006B10
- to stream Istex, to step Curation: 006B10
- to stream Istex, to step Checkpoint: 005499
- to stream Main, to step Merge: 00BC68
- to stream Main, to step Curation: 00B559
- to stream Main, to step Exploration: 00B559
- to stream France, to step Extraction: 000536
Links to Exploration step
ISTEX:D7F99114E9B37353619ED6B9C69B70C5778DADE6Le document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title>Climatic transfer function from quaternary molluscs in European loess deposits</title><author><name sortKey="Rousseau, Denis Didier" sort="Rousseau, Denis Didier" uniqKey="Rousseau D" first="Denis-Didier" last="Rousseau">Denis-Didier Rousseau</name></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:D7F99114E9B37353619ED6B9C69B70C5778DADE6</idno><date when="1991" year="1991">1991</date><idno type="doi">10.1016/0033-5894(91)90025-Z</idno><idno type="url">https://api.istex.fr/document/D7F99114E9B37353619ED6B9C69B70C5778DADE6/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">006B10</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">006B10</idno><idno type="wicri:Area/Istex/Curation">006B10</idno><idno type="wicri:Area/Istex/Checkpoint">005499</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Checkpoint">005499</idno><idno type="wicri:doubleKey">0033-5894:1991:Rousseau D:climatic:transfer:function</idno><idno type="wicri:Area/Main/Merge">00BC68</idno><idno type="wicri:Area/Main/Curation">00B559</idno><idno type="wicri:Area/Main/Exploration">00B559</idno><idno type="wicri:Area/France/Extraction">000536</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a">Climatic transfer function from quaternary molluscs in European loess deposits</title><author><name sortKey="Rousseau, Denis Didier" sort="Rousseau, Denis Didier" uniqKey="Rousseau D" first="Denis-Didier" last="Rousseau">Denis-Didier Rousseau</name><affiliation wicri:level="3"><country xml:lang="fr">France</country><wicri:regionArea>URA CNRS 157, Centre des Sciences de la Terre, 6 Bd Gabriel, F-21100 Dijon</wicri:regionArea><placeName><region type="region" nuts="2">Bourgogne-Franche-Comté</region><region type="old region" nuts="2">Bourgogne</region><settlement type="city">Dijon</settlement></placeName></affiliation></author></analytic><monogr></monogr><series><title level="j">Quaternary Research</title><title level="j" type="abbrev">YQRES</title><idno type="ISSN">0033-5894</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1991">1991</date><biblScope unit="volume">36</biblScope><biblScope unit="issue">2</biblScope><biblScope unit="page" from="195">195</biblScope><biblScope unit="page" to="209">209</biblScope></imprint><idno type="ISSN">0033-5894</idno></series></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0033-5894</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Abisko</term><term>Achenheim</term><term>Achenheim record</term><term>Achenheim sequence</term><term>Alsace</term><term>Analog</term><term>Analog climate</term><term>Annual precipitation</term><term>Assemblage</term><term>Atlantic cores</term><term>August</term><term>August precipitation</term><term>August temperatures</term><term>Climatic</term><term>Climatic cycles</term><term>Climatic parameters</term><term>Climatic variations</term><term>Columella columella</term><term>Correspondence analysis</term><term>Ecological tolerance</term><term>Factor analysis</term><term>Fauna</term><term>February</term><term>Fossil</term><term>Fossil assemblages</term><term>Global sample</term><term>Good agreement</term><term>Grande</term><term>Grande pile</term><term>Guiot</term><term>Homogeneous data</term><term>Human activities</term><term>Imbrie</term><term>Initial table</term><term>Insolation</term><term>Insolation signatures</term><term>Interglacial</term><term>Interglacial stages</term><term>Intermediate fauna</term><term>Isotope stages</term><term>Last years</term><term>Loess</term><term>Loess sequence</term><term>Lower values</term><term>Modern assemblages</term><term>Modern data</term><term>Modern precipitation regime</term><term>Modern value</term><term>Mollusc</term><term>Molluscan</term><term>Molluscan transfer</term><term>Multiple correlation coefficient</term><term>Multivariate analysis</term><term>Oceanic mechanisms</term><term>Oceanic results</term><term>Other hand</term><term>Pleniglacial stages</term><term>Pollen data</term><term>Precipitation</term><term>Precipitation estimates</term><term>Puissegur</term><term>Quaternary</term><term>Quaternary research</term><term>Radiometric dates</term><term>Second analysis</term><term>Specmap chronology</term><term>Standard error</term><term>Summer estimates</term><term>Summer precipitation</term><term>Summer temperatures</term><term>Summer values</term><term>Terrestrial molluscs</term><term>Theoretical contribution</term><term>Total number</term><term>Total variance</term><term>Transfer function</term><term>Transfer functions</term><term>Vertigo genesii</term><term>Vosges mountains</term><term>Western europe</term><term>Western side</term><term>Winter deviations</term><term>Winter estimates</term><term>Winter insolation</term><term>Winter precipitation</term><term>Winter temperatures</term></keywords><keywords scheme="Teeft" xml:lang="en"><term>Abisko</term><term>Achenheim</term><term>Achenheim record</term><term>Achenheim sequence</term><term>Alsace</term><term>Analog</term><term>Analog climate</term><term>Annual precipitation</term><term>Assemblage</term><term>Atlantic cores</term><term>August</term><term>August precipitation</term><term>August temperatures</term><term>Climatic</term><term>Climatic cycles</term><term>Climatic parameters</term><term>Climatic variations</term><term>Columella columella</term><term>Correspondence analysis</term><term>Ecological tolerance</term><term>Factor analysis</term><term>Fauna</term><term>February</term><term>Fossil</term><term>Fossil assemblages</term><term>Global sample</term><term>Good agreement</term><term>Grande</term><term>Grande pile</term><term>Guiot</term><term>Homogeneous data</term><term>Human activities</term><term>Imbrie</term><term>Initial table</term><term>Insolation</term><term>Insolation signatures</term><term>Interglacial</term><term>Interglacial stages</term><term>Intermediate fauna</term><term>Isotope stages</term><term>Last years</term><term>Loess</term><term>Loess sequence</term><term>Lower values</term><term>Modern assemblages</term><term>Modern data</term><term>Modern precipitation regime</term><term>Modern value</term><term>Mollusc</term><term>Molluscan</term><term>Molluscan transfer</term><term>Multiple correlation coefficient</term><term>Multivariate analysis</term><term>Oceanic mechanisms</term><term>Oceanic results</term><term>Other hand</term><term>Pleniglacial stages</term><term>Pollen data</term><term>Precipitation</term><term>Precipitation estimates</term><term>Puissegur</term><term>Quaternary</term><term>Quaternary research</term><term>Radiometric dates</term><term>Second analysis</term><term>Specmap chronology</term><term>Standard error</term><term>Summer estimates</term><term>Summer precipitation</term><term>Summer temperatures</term><term>Summer values</term><term>Terrestrial molluscs</term><term>Theoretical contribution</term><term>Total number</term><term>Total variance</term><term>Transfer function</term><term>Transfer functions</term><term>Vertigo genesii</term><term>Vosges mountains</term><term>Western europe</term><term>Western side</term><term>Winter deviations</term><term>Winter estimates</term><term>Winter insolation</term><term>Winter precipitation</term><term>Winter temperatures</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Alsace</term><term>Mollusque</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: Correspondence and multiple regression analysis of terrestrial molluscs in the loess sections of Achenheim (Alsace, France) has permitted the reconstruction of climatic variations during the last three glacial-interglacial cycles back to 339,000 yr B.P. The sequence has been dated according to the SPECMAP chronology of Imbrie et al. (1984) and the fossil faunas have been calibrated in relation to recent assemblages sampled in defined ecological conditions in Sweden and France. Transfer functions that relate the abundances of different species to climate allow the reconstruction of temperature and precipitation. Estimates for the coldest (February) and warmest (August) months in present-day Alsace were obtained and variations in temperature between −13° and 2°C in winter and 10° and 17°C in summer were determined. These results are consistent with those yielded by transfer functions using other continental fossils. Estimates differ for past precipitation. Summer precipitation is always less than present (with values between 50 and 78 mm, while modern August values are 76 mm higher). Winter estimates are always higher than the present mean (between 76 and 33 mm, while the recent February value is 34 mm). Comparisons between cycles show that the climatic patterns described for one cycle cannot be strictly applied to the others. Comparisons have been made with the pollen stratigraphy of La Grande Pile, the nearest quantified sequence to Achenheim, and with some Atlantic cores in order to study the magnitude of deviations from modern mean values of the climatic parameters.</div></front></TEI><affiliations><list><country><li>France</li></country><region><li>Bourgogne</li><li>Bourgogne-Franche-Comté</li></region><settlement><li>Dijon</li></settlement></list><tree><country name="France"><region name="Bourgogne-Franche-Comté"><name sortKey="Rousseau, Denis Didier" sort="Rousseau, Denis Didier" uniqKey="Rousseau D" first="Denis-Didier" last="Rousseau">Denis-Didier Rousseau</name></region></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Santé/explor/EdenteV2/Data/France/Analysis
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000536 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/France/Analysis/biblio.hfd -nk 000536 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien
|wiki= Wicri/Santé
|area= EdenteV2
|flux= France
|étape= Analysis
|type= RBID
|clé= ISTEX:D7F99114E9B37353619ED6B9C69B70C5778DADE6
|texte= Climatic transfer function from quaternary molluscs in European loess deposits
}}
| This area was generated with Dilib version V0.6.32. |  |