Patterns of land-snail succession in Central Europe over the last 15,000 years: main changes along environmental, spatial and temporal gradients

Land snail shell assemblages have been used since the pioneering days of palaeoecology to describe Quaternary environmental changes. Despite the many advantages of this proxy, it has recently been rather overlooked. There are more than 300 mollusc successions from localities throughout the Czech and...

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Published inQuaternary science reviews Vol. 93; pp. 155 - 166
Main Authors Juřičková, Lucie, Horsák, Michal, Horáčková, Jitka, Abraham, Vojtěch, Ložek, Vojen
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 01.06.2014
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Online AccessGet full text
ISSN0277-3791
1873-457X
DOI10.1016/j.quascirev.2014.03.019

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Abstract Land snail shell assemblages have been used since the pioneering days of palaeoecology to describe Quaternary environmental changes. Despite the many advantages of this proxy, it has recently been rather overlooked. There are more than 300 mollusc successions from localities throughout the Czech and Slovak Republics, making this a globally unique archive. We selected 91 of these successions for radiocarbon dating and further detailed processing. Based on analyses of 828 mollusc assemblages we found a significant increase in both total species richness and number of forest species since the Lateglacial, with a decrease in both after the Middle Holocene. In contrast, the opposite response was found for open-country species and the proportion of xerophilous species. The proportion of forest and open-country species reversed at the Pleistocene/Holocene transition (approx. 11,500 cal yrs BP). Changes in species richness were rather stable across the study area and at different elevation, contrary to changes in species composition. MDS ordination based on presence/absence data show four main patterns of species composition associated with the number of forest species in a sample, position of site along the west–east direction, the proportion of hygrophilous species and, finally, with the age of the mollusc assemblage. The number of forest species indicates the main pattern of changes in the composition of Central European land snail assemblages from the Lateglacial to the present. We confirmed the application and temporal stability of ecological groups of snails as a useful tool for reconstruction of the terrestrial palaeoenvironment. •The proportion of forest and open country species reversed 11,500 cal yrs. BP.•The peak of forest species richness was estimated about 5000 cal yrs. BP.•The number of forest species indicates the main pattern of assemblage changes.•Other patterns are west–east gradient, proportion of hygrophilous species and age.•Snail ecological groups are useful tool for reconstruction of palaeoenvironment.
AbstractList Land snail shell assemblages have been used since the pioneering days of palaeoecology to describe Quaternary environmental changes. Despite the many advantages of this proxy, it has recently been rather overlooked. There are more than 300 mollusc successions from localities throughout the Czech and Slovak Republics, making this a globally unique archive. We selected 91 of these successions for radiocarbon dating and further detailed processing. Based on analyses of 828 mollusc assemblages we found a significant increase in both total species richness and number of forest species since the Lateglacial, with a decrease in both after the Middle Holocene. In contrast, the opposite response was found for open-country species and the proportion of xerophilous species. The proportion of forest and open-country species reversed at the Pleistocene/Holocene transition (approx. 11,500 cal yrs BP). Changes in species richness were rather stable across the study area and at different elevation, contrary to changes in species composition. MDS ordination based on presence/absence data show four main patterns of species composition associated with the number of forest species in a sample, position of site along the west–east direction, the proportion of hygrophilous species and, finally, with the age of the mollusc assemblage. The number of forest species indicates the main pattern of changes in the composition of Central European land snail assemblages from the Lateglacial to the present. We confirmed the application and temporal stability of ecological groups of snails as a useful tool for reconstruction of the terrestrial palaeoenvironment. •The proportion of forest and open country species reversed 11,500 cal yrs. BP.•The peak of forest species richness was estimated about 5000 cal yrs. BP.•The number of forest species indicates the main pattern of assemblage changes.•Other patterns are west–east gradient, proportion of hygrophilous species and age.•Snail ecological groups are useful tool for reconstruction of palaeoenvironment.
Land snail shell assemblages have been used since the pioneering days of palaeoecology to describe Quaternary environmental changes. Despite the many advantages of this proxy, it has recently been rather overlooked. There are more than 300 mollusc successions from localities throughout the Czech and Slovak Republics, making this a globally unique archive. We selected 91 of these successions for radiocarbon dating and further detailed processing. Based on analyses of 828 mollusc assemblages we found a significant increase in both total species richness and number of forest species since the Lateglacial, with a decrease in both after the Middle Holocene. In contrast, the opposite response was found for open-country species and the proportion of xerophilous species. The proportion of forest and open-country species reversed at the Pleistocene/Holocene transition (approx. 11,500 cal yrs BP). Changes in species richness were rather stable across the study area and at different elevation, contrary to changes in species composition. MDS ordination based on presence/absence data show four main patterns of species composition associated with the number of forest species in a sample, position of site along the west-east direction, the proportion of hygrophilous species and, finally, with the age of the mollusc assemblage. The number of forest species indicates the main pattern of changes in the composition of Central European land snail assemblages from the Lateglacial to the present. We confirmed the application and temporal stability of ecological groups of snails as a useful tool for reconstruction of the terrestrial palaeoenvironment.
Author Juřičková, Lucie
Horáčková, Jitka
Ložek, Vojen
Horsák, Michal
Abraham, Vojtěch
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  givenname: Jitka
  surname: Horáčková
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  surname: Ložek
  fullname: Ložek, Vojen
  organization: Department of Zoology, Faculty of Science, Charles University in Prague, Viničná 7, CZ-128 44 Prague 2, Czech Republic
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Keywords Mollusc succession
Forest species
Lateglacial
Central European refugia
Holocene
Palaeoenvironment reconstruction
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Snippet Land snail shell assemblages have been used since the pioneering days of palaeoecology to describe Quaternary environmental changes. Despite the many...
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crossref
elsevier
SourceType Aggregation Database
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Index Database
Publisher
StartPage 155
SubjectTerms Central European refugia
Forest species
Holocene
Lateglacial
Mollusc succession
Palaeoenvironment reconstruction
Title Patterns of land-snail succession in Central Europe over the last 15,000 years: main changes along environmental, spatial and temporal gradients
URI https://dx.doi.org/10.1016/j.quascirev.2014.03.019
https://www.proquest.com/docview/1805503821
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