Diatom and vegetation responses to Late Glacial and Early Holocene climate changes at Lake Estanya (Southern Pyrenees, NE Spain)

We investigate Lake Estanya's diatom and pollen records from the Late Glacial (LG) to the Early Holocene (EH), in order to compare limnological and vegetation responses to common climate forcing. The biotic changes recognized in this study largely agree with the hydrological evolution of the lake de...

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Authors: Vegas Vilarrúbia, Teresa Elena; Gonzáles-Sanpériz, P.; Morellón, Mario; Gil-Romera, G; Pérez-Sanz, A.; Valero Garcés, Blas Lorenzo
Format: Article
Status:Accepted version
Publication date:2013
Country:España
Institution:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
Repository:Recercat. Dipósit de la Recerca de Catalunya
OAI Identifier:oai:recercat.cat:2445/124935
Online Access:https://hdl.handle.net/2445/124935
Access Level:Open access
Keyword:Diatomees
Canvi climàtic
Plantes aquàtiques
Pirineus
Diatoms
Climatic change
Aquatic plants
Pyrenees
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author Vegas Vilarrúbia, Teresa Elena
author2 Gonzáles-Sanpériz, P.
Morellón, Mario
Gil-Romera, G
Pérez-Sanz, A.
Valero Garcés, Blas Lorenzo
author2_role author
author
author
author
author
author_browse Gil-Romera, G
Gonzáles-Sanpériz, P.
Morellón, Mario
Pérez-Sanz, A.
Valero Garcés, Blas Lorenzo
Vegas Vilarrúbia, Teresa Elena
author_facet Vegas Vilarrúbia, Teresa Elena
Gonzáles-Sanpériz, P.
Morellón, Mario
Gil-Romera, G
Pérez-Sanz, A.
Valero Garcés, Blas Lorenzo
author_role author
collection Recercat. Dipósit de la Recerca de Catalunya
description We investigate Lake Estanya's diatom and pollen records from the Late Glacial (LG) to the Early Holocene (EH), in order to compare limnological and vegetation responses to common climate forcing. The biotic changes recognized in this study largely agree with the hydrological evolution of the lake described previously for the same period. The diatom record shows high sensitivity to fluctuations in both lake level and salinity concentration as consequence of climate shifts. In addition vegetation results indicate that the area could have played an important role as regional vegetation refuge. Shallow lake conditions during the Last Glacial Maximum (LGM) were punctuated by relatively deeper freshwaters between 19.3 and 18.6 cal kyr BP and at 18.0 cal kyr BP, as recorded by diatom shifts. A subsequent increasing aridity trend, coinciding with the Mystery Interval (MI), affected the diatom accumulation rates, which dropped to its minimum values between 17.2 to 14.7 cal kyr BP. Particularly dry and cold conditions during the LGM and MI are supported by the largest values of steppic pollen taxa of the whole sequence, which account for up to 40%. However, relatively high values of Betula during the Heinrich Event 1 suggest a plausible regional vegetation refuge. Abrupt cooling and warming episodes within the LG triggered remarkable ecological threshold crossings in the diatom communities, especially during the stadial/interstadial episodes. At this point, the vegetation reflect the onset of warm conditions during the Bølling/Allerød with the partial substitution of Betula by Marcescent and Evergreen Quercus, what probably indicates the arrival of temperate taxa to the area and the likely migration of birch to higher altitudes. The Younger Dryas Stadial shows a complex ecological response. Diatoms are very poorly preserved, but aquatic taxa reach their highest values. An increase in Marcescent Quercus during this cold stage lends further support to the hypothesis that this is a regional vegetation refuge. Low lake levels recorded during the EH affected the development and preservation of diatom communities. A delay in the onset of humid conditions for the EH is also supported by the vegetation composition, characterized by the maximum expansion of Juniperus.
eu_rights_str_mv openAccess
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institution Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
instname_str Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
network_acronym_str ES
network_name_str España
oai_identifier_str oai:recercat.cat:2445/124935
publishDate 2013
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publisher Elsevier B.V.
publisherStr Elsevier B.V.
reponame_str Recercat. Dipósit de la Recerca de Catalunya
spelling Diatom and vegetation responses to Late Glacial and Early Holocene climate changes at Lake Estanya (Southern Pyrenees, NE Spain) Vegas Vilarrúbia, Teresa Elena Gonzáles-Sanpériz, P. Morellón, Mario Gil-Romera, G Pérez-Sanz, A. Valero Garcés, Blas Lorenzo Diatomees Canvi climàtic Plantes aquàtiques Pirineus Diatoms Climatic change Aquatic plants Pyrenees We investigate Lake Estanya's diatom and pollen records from the Late Glacial (LG) to the Early Holocene (EH), in order to compare limnological and vegetation responses to common climate forcing. The biotic changes recognized in this study largely agree with the hydrological evolution of the lake described previously for the same period. The diatom record shows high sensitivity to fluctuations in both lake level and salinity concentration as consequence of climate shifts. In addition vegetation results indicate that the area could have played an important role as regional vegetation refuge. Shallow lake conditions during the Last Glacial Maximum (LGM) were punctuated by relatively deeper freshwaters between 19.3 and 18.6 cal kyr BP and at 18.0 cal kyr BP, as recorded by diatom shifts. A subsequent increasing aridity trend, coinciding with the Mystery Interval (MI), affected the diatom accumulation rates, which dropped to its minimum values between 17.2 to 14.7 cal kyr BP. Particularly dry and cold conditions during the LGM and MI are supported by the largest values of steppic pollen taxa of the whole sequence, which account for up to 40%. However, relatively high values of Betula during the Heinrich Event 1 suggest a plausible regional vegetation refuge. Abrupt cooling and warming episodes within the LG triggered remarkable ecological threshold crossings in the diatom communities, especially during the stadial/interstadial episodes. At this point, the vegetation reflect the onset of warm conditions during the Bølling/Allerød with the partial substitution of Betula by Marcescent and Evergreen Quercus, what probably indicates the arrival of temperate taxa to the area and the likely migration of birch to higher altitudes. The Younger Dryas Stadial shows a complex ecological response. Diatoms are very poorly preserved, but aquatic taxa reach their highest values. An increase in Marcescent Quercus during this cold stage lends further support to the hypothesis that this is a regional vegetation refuge. Low lake levels recorded during the EH affected the development and preservation of diatom communities. A delay in the onset of humid conditions for the EH is also supported by the vegetation composition, characterized by the maximum expansion of Juniperus. Elsevier B.V. https://hdl.handle.net/2445/124935
spellingShingle Diatom and vegetation responses to Late Glacial and Early Holocene climate changes at Lake Estanya (Southern Pyrenees, NE Spain)
Vegas Vilarrúbia, Teresa Elena
Diatomees
Canvi climàtic
Plantes aquàtiques
Pirineus
Diatoms
Climatic change
Aquatic plants
Pyrenees
status_str acceptedVersion
title Diatom and vegetation responses to Late Glacial and Early Holocene climate changes at Lake Estanya (Southern Pyrenees, NE Spain)
title_full Diatom and vegetation responses to Late Glacial and Early Holocene climate changes at Lake Estanya (Southern Pyrenees, NE Spain)
title_fullStr Diatom and vegetation responses to Late Glacial and Early Holocene climate changes at Lake Estanya (Southern Pyrenees, NE Spain)
title_full_unstemmed Diatom and vegetation responses to Late Glacial and Early Holocene climate changes at Lake Estanya (Southern Pyrenees, NE Spain)
title_short Diatom and vegetation responses to Late Glacial and Early Holocene climate changes at Lake Estanya (Southern Pyrenees, NE Spain)
title_sort Diatom and vegetation responses to Late Glacial and Early Holocene climate changes at Lake Estanya (Southern Pyrenees, NE Spain)
topic Diatomees
Canvi climàtic
Plantes aquàtiques
Pirineus
Diatoms
Climatic change
Aquatic plants
Pyrenees
topic_facet Diatomees
Canvi climàtic
Plantes aquàtiques
Pirineus
Diatoms
Climatic change
Aquatic plants
Pyrenees
url https://hdl.handle.net/2445/124935