Paleoclimate reconstruction and mire development in the Eastern Great Hungarian Plain for the last 20,000 years
International audience We present the reconstruction of mire vegetation changes and fire history recorded in a continuous sediment profile that spans the last 20,000 cal yr BP from the Late Pleniglacial to Holocene in North-eastern Hungary. We also aimed to reveal past climate changes by using ecolo...
Published in: | Review of Palaeobotany and Palynology |
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Main Authors: | , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2019
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Subjects: | |
Online Access: | https://hal.archives-ouvertes.fr/hal-02279803 https://hal.archives-ouvertes.fr/hal-02279803/document https://hal.archives-ouvertes.fr/hal-02279803/file/Vincze_etal_RevPalPal_PreProof.pdf https://doi.org/10.1016/j.revpalbo.2019.104112 |
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Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
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English |
topic |
[SDV.SA.SF]Life Sciences [q-bio]/Agricultural sciences/Silviculture forestry [SDV.BV.BOT]Life Sciences [q-bio]/Vegetal Biology/Botanics [SDV.BIBS]Life Sciences [q-bio]/Quantitative Methods [q-bio.QM] [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDE.MCG]Environmental Sciences/Global Changes [SDE.ES]Environmental Sciences/Environmental and Society [SDE.BE]Environmental Sciences/Biodiversity and Ecology |
spellingShingle |
[SDV.SA.SF]Life Sciences [q-bio]/Agricultural sciences/Silviculture forestry [SDV.BV.BOT]Life Sciences [q-bio]/Vegetal Biology/Botanics [SDV.BIBS]Life Sciences [q-bio]/Quantitative Methods [q-bio.QM] [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDE.MCG]Environmental Sciences/Global Changes [SDE.ES]Environmental Sciences/Environmental and Society [SDE.BE]Environmental Sciences/Biodiversity and Ecology Vincze, Ildikó Finsinger, Walter Jakab, Gusztáv Braun, Mihály Hubay, Katalin Veres, Daniel Deli, Tamás Szalai, Zoltán Szabó, Zoltan Magyari, Enikő Paleoclimate reconstruction and mire development in the Eastern Great Hungarian Plain for the last 20,000 years |
topic_facet |
[SDV.SA.SF]Life Sciences [q-bio]/Agricultural sciences/Silviculture forestry [SDV.BV.BOT]Life Sciences [q-bio]/Vegetal Biology/Botanics [SDV.BIBS]Life Sciences [q-bio]/Quantitative Methods [q-bio.QM] [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDE.MCG]Environmental Sciences/Global Changes [SDE.ES]Environmental Sciences/Environmental and Society [SDE.BE]Environmental Sciences/Biodiversity and Ecology |
description |
International audience We present the reconstruction of mire vegetation changes and fire history recorded in a continuous sediment profile that spans the last 20,000 cal yr BP from the Late Pleniglacial to Holocene in North-eastern Hungary. We also aimed to reveal past climate changes by using ecological requirements of specific aquatic plants as summer temperature indicators. Our results suggest the formation of a mesotrophic mire around 20,000 cal yr BP with brown moss, Betula sp. and Selaginella selaginoides cover beside the occurrence of Phragmites australis, Typha latifolia and T. angustifolia suggesting base-rich fen and tundra-like wet-ground habitats on the lakeshore. This community shifted to reed dominated swamp at c. 18,300 cal yr BP with inferred min. July temperatures of 12–15.7°C. Pinus sp., Betula nana, B. pendula/pubescens, Hippuris vulgaris and P. australis dominated until 16,600 cal yr BP pointing to shallow muddy stagnant water and colder climatic conditions than in the preceding interval. The most warmth-demanding species, T. latifolia and T. angustifolia indicated July mean temperatures > 14-15.7°C soon after the LGM. The formation of biogenic carbonate also started at an early stage; major accumulation occurred between 15,200 and 10,000 cal yr BP. In the Early Holocene, environmental indicator species (e.g. Phragmites australis and T. latifolia) pointed to warmer and shallower conditions, while the late Holocene was characterised by strong eutrophication and reed swamp dominance on the lakeshore. Elevated macrocharcoal concentration, wood fragments and remains of Typha species suggested frequent local fires and dry mire surface conditions during the last 1700 years. |
author2 |
Department of Environmental and Landscape Geography Eötvös Loránd University (ELTE) MTA-MTM-ELTE Research Group for Paleontology Eötvös Loránd University (ELTE)-Hungarian Academy of Sciences (MTA) GINOP Sustainable Ecosystem Research Group MTA Centre for Ecological Research Tihany Hungarian Academy of Sciences (MTA)-Hungarian Academy of Sciences (MTA) Institut des Sciences de l'Evolution de Montpellier (UMR ISEM) École pratique des hautes études (EPHE) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Centre National de la Recherche Scientifique (CNRS)-Institut de recherche pour le développement IRD : UR226 Department of Physical Geography and Quaternary Geology Stockholm University School of Chemical Sciences and Engineering, Department of Chemistry, Inorganic Chemistry Royal Institute of Technology Stockholm (KTH ) |
format |
Article in Journal/Newspaper |
author |
Vincze, Ildikó Finsinger, Walter Jakab, Gusztáv Braun, Mihály Hubay, Katalin Veres, Daniel Deli, Tamás Szalai, Zoltán Szabó, Zoltan Magyari, Enikő |
author_facet |
Vincze, Ildikó Finsinger, Walter Jakab, Gusztáv Braun, Mihály Hubay, Katalin Veres, Daniel Deli, Tamás Szalai, Zoltán Szabó, Zoltan Magyari, Enikő |
author_sort |
Vincze, Ildikó |
title |
Paleoclimate reconstruction and mire development in the Eastern Great Hungarian Plain for the last 20,000 years |
title_short |
Paleoclimate reconstruction and mire development in the Eastern Great Hungarian Plain for the last 20,000 years |
title_full |
Paleoclimate reconstruction and mire development in the Eastern Great Hungarian Plain for the last 20,000 years |
title_fullStr |
Paleoclimate reconstruction and mire development in the Eastern Great Hungarian Plain for the last 20,000 years |
title_full_unstemmed |
Paleoclimate reconstruction and mire development in the Eastern Great Hungarian Plain for the last 20,000 years |
title_sort |
paleoclimate reconstruction and mire development in the eastern great hungarian plain for the last 20,000 years |
publisher |
HAL CCSD |
publishDate |
2019 |
url |
https://hal.archives-ouvertes.fr/hal-02279803 https://hal.archives-ouvertes.fr/hal-02279803/document https://hal.archives-ouvertes.fr/hal-02279803/file/Vincze_etal_RevPalPal_PreProof.pdf https://doi.org/10.1016/j.revpalbo.2019.104112 |
genre |
Betula nana Tundra |
genre_facet |
Betula nana Tundra |
op_source |
ISSN: 0034-6667 Review of Palaeobotany and Palynology https://hal.archives-ouvertes.fr/hal-02279803 Review of Palaeobotany and Palynology, Elsevier, 2019, 271, pp.104112. ⟨10.1016/j.revpalbo.2019.104112⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.revpalbo.2019.104112 hal-02279803 https://hal.archives-ouvertes.fr/hal-02279803 https://hal.archives-ouvertes.fr/hal-02279803/document https://hal.archives-ouvertes.fr/hal-02279803/file/Vincze_etal_RevPalPal_PreProof.pdf doi:10.1016/j.revpalbo.2019.104112 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1016/j.revpalbo.2019.104112 |
container_title |
Review of Palaeobotany and Palynology |
container_volume |
271 |
container_start_page |
104112 |
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1766378881893269504 |
spelling |
ftccsdartic:oai:HAL:hal-02279803v1 2023-05-15T15:44:30+02:00 Paleoclimate reconstruction and mire development in the Eastern Great Hungarian Plain for the last 20,000 years Vincze, Ildikó Finsinger, Walter Jakab, Gusztáv Braun, Mihály Hubay, Katalin Veres, Daniel Deli, Tamás Szalai, Zoltán Szabó, Zoltan Magyari, Enikő Department of Environmental and Landscape Geography Eötvös Loránd University (ELTE) MTA-MTM-ELTE Research Group for Paleontology Eötvös Loránd University (ELTE)-Hungarian Academy of Sciences (MTA) GINOP Sustainable Ecosystem Research Group MTA Centre for Ecological Research Tihany Hungarian Academy of Sciences (MTA)-Hungarian Academy of Sciences (MTA) Institut des Sciences de l'Evolution de Montpellier (UMR ISEM) École pratique des hautes études (EPHE) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Centre National de la Recherche Scientifique (CNRS)-Institut de recherche pour le développement IRD : UR226 Department of Physical Geography and Quaternary Geology Stockholm University School of Chemical Sciences and Engineering, Department of Chemistry, Inorganic Chemistry Royal Institute of Technology Stockholm (KTH ) 2019 https://hal.archives-ouvertes.fr/hal-02279803 https://hal.archives-ouvertes.fr/hal-02279803/document https://hal.archives-ouvertes.fr/hal-02279803/file/Vincze_etal_RevPalPal_PreProof.pdf https://doi.org/10.1016/j.revpalbo.2019.104112 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.revpalbo.2019.104112 hal-02279803 https://hal.archives-ouvertes.fr/hal-02279803 https://hal.archives-ouvertes.fr/hal-02279803/document https://hal.archives-ouvertes.fr/hal-02279803/file/Vincze_etal_RevPalPal_PreProof.pdf doi:10.1016/j.revpalbo.2019.104112 info:eu-repo/semantics/OpenAccess ISSN: 0034-6667 Review of Palaeobotany and Palynology https://hal.archives-ouvertes.fr/hal-02279803 Review of Palaeobotany and Palynology, Elsevier, 2019, 271, pp.104112. ⟨10.1016/j.revpalbo.2019.104112⟩ [SDV.SA.SF]Life Sciences [q-bio]/Agricultural sciences/Silviculture forestry [SDV.BV.BOT]Life Sciences [q-bio]/Vegetal Biology/Botanics [SDV.BIBS]Life Sciences [q-bio]/Quantitative Methods [q-bio.QM] [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDE.MCG]Environmental Sciences/Global Changes [SDE.ES]Environmental Sciences/Environmental and Society [SDE.BE]Environmental Sciences/Biodiversity and Ecology info:eu-repo/semantics/article Journal articles 2019 ftccsdartic https://doi.org/10.1016/j.revpalbo.2019.104112 2021-11-21T00:35:23Z International audience We present the reconstruction of mire vegetation changes and fire history recorded in a continuous sediment profile that spans the last 20,000 cal yr BP from the Late Pleniglacial to Holocene in North-eastern Hungary. We also aimed to reveal past climate changes by using ecological requirements of specific aquatic plants as summer temperature indicators. Our results suggest the formation of a mesotrophic mire around 20,000 cal yr BP with brown moss, Betula sp. and Selaginella selaginoides cover beside the occurrence of Phragmites australis, Typha latifolia and T. angustifolia suggesting base-rich fen and tundra-like wet-ground habitats on the lakeshore. This community shifted to reed dominated swamp at c. 18,300 cal yr BP with inferred min. July temperatures of 12–15.7°C. Pinus sp., Betula nana, B. pendula/pubescens, Hippuris vulgaris and P. australis dominated until 16,600 cal yr BP pointing to shallow muddy stagnant water and colder climatic conditions than in the preceding interval. The most warmth-demanding species, T. latifolia and T. angustifolia indicated July mean temperatures > 14-15.7°C soon after the LGM. The formation of biogenic carbonate also started at an early stage; major accumulation occurred between 15,200 and 10,000 cal yr BP. In the Early Holocene, environmental indicator species (e.g. Phragmites australis and T. latifolia) pointed to warmer and shallower conditions, while the late Holocene was characterised by strong eutrophication and reed swamp dominance on the lakeshore. Elevated macrocharcoal concentration, wood fragments and remains of Typha species suggested frequent local fires and dry mire surface conditions during the last 1700 years. Article in Journal/Newspaper Betula nana Tundra Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Review of Palaeobotany and Palynology 271 104112 |