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Holocene molluscan faunal history and environmental change at Kloster Mühle, Rheinland‐Pfalz, western Germany

Identifieur interne : 003E43 ( Istex/Corpus ); précédent : 003E42; suivant : 003E44

Holocene molluscan faunal history and environmental change at Kloster Mühle, Rheinland‐Pfalz, western Germany

Auteurs : R. A. Meyrick

Source :

RBID : ISTEX:7E1B612734D5DBA92AB80903B4911C62C37BB8F5

English descriptors

Abstract

The Holocene molluscan succession presented here, from a tufa at Kloster Mühle, near Trier, is the most detailed yet published from the German Bundesland of Rheinland‐Pfalz. The base of the sequence, dated at 9720 ± 75 14C yr BP, indicates that the early Holocene was characterised by a moist, open‐ground fauna dominated by Succinea/Oxyloma. The aquatic phase that follows is short lived, bracketed by statistically indistinguishable dates of 9530 ± 60 14C yr BP (below) and 9695 ± 75 14C yr BP (above). The establishment of woodland is indicated by the appearance of Aegopinella nitidula, Vertigo pusilla and especially Carychium tridentatum, which subsequently expands to account for over 40% of the total fauna. Deciduous forest optimum conditions, characterised by the occurrence of Platyla polita and Helicigona lapicida, become established at about 7405 ± 50 14C yr BP. The radiocarbon age of 4384 ± 105 14C yr BP obtained for the uppermost tufa horizon is much younger than expected, both on the basis of the molluscan fauna observed and the implied decline in the rate of sedimentation in the upper part of the deposit, and tufa formation probably ceased much earlier than this date suggests. Copyright © 2002 John Wiley & Sons, Ltd.

Url:
DOI: 10.1002/jqs.728

Links to Exploration step

ISTEX:7E1B612734D5DBA92AB80903B4911C62C37BB8F5

Le document en format XML

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<term>Environmental change</term>
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<div type="abstract" xml:lang="de">The Holocene molluscan succession presented here, from a tufa at Kloster Mühle, near Trier, is the most detailed yet published from the German Bundesland of Rheinland‐Pfalz. The base of the sequence, dated at 9720 ± 75 14C yr BP, indicates that the early Holocene was characterised by a moist, open‐ground fauna dominated by Succinea/Oxyloma. The aquatic phase that follows is short lived, bracketed by statistically indistinguishable dates of 9530 ± 60 14C yr BP (below) and 9695 ± 75 14C yr BP (above). The establishment of woodland is indicated by the appearance of Aegopinella nitidula, Vertigo pusilla and especially Carychium tridentatum, which subsequently expands to account for over 40% of the total fauna. Deciduous forest optimum conditions, characterised by the occurrence of Platyla polita and Helicigona lapicida, become established at about 7405 ± 50 14C yr BP. The radiocarbon age of 4384 ± 105 14C yr BP obtained for the uppermost tufa horizon is much younger than expected, both on the basis of the molluscan fauna observed and the implied decline in the rate of sedimentation in the upper part of the deposit, and tufa formation probably ceased much earlier than this date suggests. Copyright © 2002 John Wiley & Sons, Ltd.</div>
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<json:string>Devriese, 1976</json:string>
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<json:string>Pfeiffer, 1853</json:string>
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<json:string>Dehm, 1951</json:string>
<json:string>Risso, 1826</json:string>
<json:string>Hor´ cek and Loˇ ek, 1988</json:string>
<json:string>von Proschwitz, 1993</json:string>
<json:string>Muller, 1774</json:string>
<json:string>Draparnaud, 1805</json:string>
<json:string>Kerney et al., 1980</json:string>
<json:string>Meyrick, 1999, 2001, 2002</json:string>
<json:string>Dehm, 1967</json:string>
<json:string>R¨ cke, 1987</json:string>
<json:string>Limondin, 1995</json:string>
<json:string>Torkzadeh, 1972</json:string>
<json:string>Limondine Lozouet, 1997</json:string>
<json:string>Killeen, 1992</json:string>
<json:string>Preece, 1998</json:string>
<json:string>Pokryszko, 1990</json:string>
<json:string>in the Czech Republic and Slovakia (Loˇ ek, 1964, 1982</json:string>
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<json:string>a Meyrick, 1999</json:string>
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<json:string>Strom, 1765</json:string>
<json:string>Meyrick, 2001</json:string>
<json:string>Soens and Gullentops, 1969</json:string>
<json:string>Vogt et al., 1994</json:string>
<json:string>Clapham et al., 1962</json:string>
<json:string>Gittenberger et al. (1998)</json:string>
<json:string>Huntley and Birks (1983)</json:string>
<json:string>Feustel et al., 1971</json:string>
<json:string>Loˇ ek, 1964</json:string>
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<p>The Holocene molluscan succession presented here, from a tufa at Kloster Mühle, near Trier, is the most detailed yet published from the German Bundesland of Rheinland‐Pfalz. The base of the sequence, dated at 9720 ± 75
<sup>14</sup>
C yr BP, indicates that the early Holocene was characterised by a moist, open‐ground fauna dominated by
<i>Succinea</i>
/
<i>Oxyloma</i>
. The aquatic phase that follows is short lived, bracketed by statistically indistinguishable dates of 9530 ± 60
<sup>14</sup>
C yr BP (below) and 9695 ± 75
<sup>14</sup>
C yr BP (above). The establishment of woodland is indicated by the appearance of
<i>Aegopinella nitidula</i>
,
<i>Vertigo pusilla</i>
and especially
<i>Carychium tridentatum</i>
, which subsequently expands to account for over 40% of the total fauna. Deciduous forest optimum conditions, characterised by the occurrence of
<i>Platyla polita</i>
and
<i>Helicigona lapicida</i>
, become established at about 7405 ± 50
<sup>14</sup>
C yr BP. The radiocarbon age of 4384 ± 105
<sup>14</sup>
C yr BP obtained for the uppermost tufa horizon is much younger than expected, both on the basis of the molluscan fauna observed and the implied decline in the rate of sedimentation in the upper part of the deposit, and tufa formation probably ceased much earlier than this date suggests. Copyright © 2002 John Wiley & Sons, Ltd.</p>
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<title>HOLOCENE MOLLUSC SEQUENCE FROM WESTERN GERMANY</title>
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<title>Holocene molluscan faunal history and environmental change at Kloster Mühle, Rheinland‐Pfalz, western Germany</title>
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<namePart type="given">R. A.</namePart>
<namePart type="family">Meyrick</namePart>
<affiliation>Godwin Institute for Quaternary Research, Department of Zoology, University of Cambridge, Downing Street, Cambridge CB2 3EJ, England</affiliation>
<affiliation>E-mail: rich.meyrick@senckenberg.de</affiliation>
<affiliation>Correspondence address: Forschungsstation für Quartärpaläontologie Weimar, Steubenstraße 19a, 99423 Weimar, Germany (current address)</affiliation>
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<abstract lang="de">The Holocene molluscan succession presented here, from a tufa at Kloster Mühle, near Trier, is the most detailed yet published from the German Bundesland of Rheinland‐Pfalz. The base of the sequence, dated at 9720 ± 75 14C yr BP, indicates that the early Holocene was characterised by a moist, open‐ground fauna dominated by Succinea/Oxyloma. The aquatic phase that follows is short lived, bracketed by statistically indistinguishable dates of 9530 ± 60 14C yr BP (below) and 9695 ± 75 14C yr BP (above). The establishment of woodland is indicated by the appearance of Aegopinella nitidula, Vertigo pusilla and especially Carychium tridentatum, which subsequently expands to account for over 40% of the total fauna. Deciduous forest optimum conditions, characterised by the occurrence of Platyla polita and Helicigona lapicida, become established at about 7405 ± 50 14C yr BP. The radiocarbon age of 4384 ± 105 14C yr BP obtained for the uppermost tufa horizon is much younger than expected, both on the basis of the molluscan fauna observed and the implied decline in the rate of sedimentation in the upper part of the deposit, and tufa formation probably ceased much earlier than this date suggests. Copyright © 2002 John Wiley & Sons, Ltd.</abstract>
<note type="funding">Natural Environment Research Council (UK).</note>
<subject lang="en">
<genre>keywords</genre>
<topic>Mollusca</topic>
<topic>tufa</topic>
<topic>Germany</topic>
<topic>Holocene</topic>
<topic>radiocarbon</topic>
</subject>
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<title>Journal of Quaternary Science</title>
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<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>2003</date>
<detail type="volume">
<caption>vol.</caption>
<number>18</number>
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<detail type="issue">
<caption>no.</caption>
<number>2</number>
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<start>121</start>
<end>132</end>
<total>12</total>
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<accessCondition type="use and reproduction" contentType="copyright">Copyright © 2002 John Wiley & Sons, Ltd.</accessCondition>
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