Palaeobiodiversity of Knyszyn Forest (NE Poland) Mires Based on the Late Glacial and Holocene Histories of Vascular Plant Species

Peat and lacustrine sediments are a valuable source of knowledge about past biodiversity. Plant macrofossil remains were identified in sediments of mires in northeastern Poland’s Knyszyn Forest. Among them, the remains of species currently absent in this area, such as Potamogeton pusillus, P. friesi...

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Published in:Diversity
Main Author: Danuta Drzymulska
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/d15040502
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spelling ftmdpi:oai:mdpi.com:/1424-2818/15/4/502/ 2023-08-20T04:05:37+02:00 Palaeobiodiversity of Knyszyn Forest (NE Poland) Mires Based on the Late Glacial and Holocene Histories of Vascular Plant Species Danuta Drzymulska agris 2023-04-01 application/pdf https://doi.org/10.3390/d15040502 EN eng Multidisciplinary Digital Publishing Institute Biodiversity Loss & Dynamics https://dx.doi.org/10.3390/d15040502 https://creativecommons.org/licenses/by/4.0/ Diversity; Volume 15; Issue 4; Pages: 502 mire peat plant macrofossil remains Late Glacial Holocene northeastern Poland Text 2023 ftmdpi https://doi.org/10.3390/d15040502 2023-08-01T09:32:02Z Peat and lacustrine sediments are a valuable source of knowledge about past biodiversity. Plant macrofossil remains were identified in sediments of mires in northeastern Poland’s Knyszyn Forest. Among them, the remains of species currently absent in this area, such as Potamogeton pusillus, P. friesii, P. filiformis, Myriophyllum alterniflorum, and Cladium mariscus, have been found. In addition, the history of Betula humilis and its possible correlations with another species of bush birch—Betula nana—were of interest. Radiocarbon dating allowed the presence of the studied species to be placed within a time frame, and it was thus established that aquatic species existed in the area under study during the Late Glacial and the turn of the Holocene. Cladium mariscus occurred during the Greenlandian and Meghalayan stages of the Holocene and then became intolerant of habitat changes that occurred. The coexistence of two species of birch known to exist since the Late Glacial was interrupted in the Northgrippian. B. nana, then disappeared from the area, and B. humilis continued to occur as it was more resistant to the changing environmental conditions. It must be emphasized, however, that these conclusions were made possible by the researchers’ access to undisturbed deposits. The mires present in the area of study remain in good condition, providing important and relevant materials for palaeoecological research. Text Betula nana MDPI Open Access Publishing Diversity 15 4 502
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic mire
peat
plant macrofossil remains
Late Glacial
Holocene
northeastern Poland
spellingShingle mire
peat
plant macrofossil remains
Late Glacial
Holocene
northeastern Poland
Danuta Drzymulska
Palaeobiodiversity of Knyszyn Forest (NE Poland) Mires Based on the Late Glacial and Holocene Histories of Vascular Plant Species
topic_facet mire
peat
plant macrofossil remains
Late Glacial
Holocene
northeastern Poland
description Peat and lacustrine sediments are a valuable source of knowledge about past biodiversity. Plant macrofossil remains were identified in sediments of mires in northeastern Poland’s Knyszyn Forest. Among them, the remains of species currently absent in this area, such as Potamogeton pusillus, P. friesii, P. filiformis, Myriophyllum alterniflorum, and Cladium mariscus, have been found. In addition, the history of Betula humilis and its possible correlations with another species of bush birch—Betula nana—were of interest. Radiocarbon dating allowed the presence of the studied species to be placed within a time frame, and it was thus established that aquatic species existed in the area under study during the Late Glacial and the turn of the Holocene. Cladium mariscus occurred during the Greenlandian and Meghalayan stages of the Holocene and then became intolerant of habitat changes that occurred. The coexistence of two species of birch known to exist since the Late Glacial was interrupted in the Northgrippian. B. nana, then disappeared from the area, and B. humilis continued to occur as it was more resistant to the changing environmental conditions. It must be emphasized, however, that these conclusions were made possible by the researchers’ access to undisturbed deposits. The mires present in the area of study remain in good condition, providing important and relevant materials for palaeoecological research.
format Text
author Danuta Drzymulska
author_facet Danuta Drzymulska
author_sort Danuta Drzymulska
title Palaeobiodiversity of Knyszyn Forest (NE Poland) Mires Based on the Late Glacial and Holocene Histories of Vascular Plant Species
title_short Palaeobiodiversity of Knyszyn Forest (NE Poland) Mires Based on the Late Glacial and Holocene Histories of Vascular Plant Species
title_full Palaeobiodiversity of Knyszyn Forest (NE Poland) Mires Based on the Late Glacial and Holocene Histories of Vascular Plant Species
title_fullStr Palaeobiodiversity of Knyszyn Forest (NE Poland) Mires Based on the Late Glacial and Holocene Histories of Vascular Plant Species
title_full_unstemmed Palaeobiodiversity of Knyszyn Forest (NE Poland) Mires Based on the Late Glacial and Holocene Histories of Vascular Plant Species
title_sort palaeobiodiversity of knyszyn forest (ne poland) mires based on the late glacial and holocene histories of vascular plant species
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/d15040502
op_coverage agris
genre Betula nana
genre_facet Betula nana
op_source Diversity; Volume 15; Issue 4; Pages: 502
op_relation Biodiversity Loss & Dynamics
https://dx.doi.org/10.3390/d15040502
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/d15040502
container_title Diversity
container_volume 15
container_issue 4
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