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Long-term forest dynamics at Gribskov, eastern Denmark with early-Holocene evidence for thermophilous broadleaved tree species

Overballe-Petersen, Mette Venas ; Nielsen, Anne Birgitte LU orcid ; Hannon, Gina E. ; Halsall, Karen and Bradshaw, Richard H. W. (2013) In The Holocene 23(2). p.243-254
Abstract
We report on a full-Holocene pollen, charcoal and macrofossil record from a small forest hollow in Gribskov, eastern Denmark. The Fagus sylvatica pollen record suggests the establishment of a small Fagus population at Gribskov in the early Holocene together with early establishment of other thermophilous broadleaved trees, including Quercus sp., Tilia sp. and Ulmus sp. The macrofossils contribute to the vegetation reconstruction with evidence for local presence of species with low pollen productivity or easily degraded pollen types such as Populus. The charcoal record shows frequent burning during two periods of the early Holocene and from c. 3000 cal. BP to present. The early-Holocene part of the record indicates a highly disturbed forest... (More)
We report on a full-Holocene pollen, charcoal and macrofossil record from a small forest hollow in Gribskov, eastern Denmark. The Fagus sylvatica pollen record suggests the establishment of a small Fagus population at Gribskov in the early Holocene together with early establishment of other thermophilous broadleaved trees, including Quercus sp., Tilia sp. and Ulmus sp. The macrofossils contribute to the vegetation reconstruction with evidence for local presence of species with low pollen productivity or easily degraded pollen types such as Populus. The charcoal record shows frequent burning during two periods of the early Holocene and from c. 3000 cal. BP to present. The early-Holocene part of the record indicates a highly disturbed forest ecosystem with frequent fires and abundant macrofossils of particularly Betula sp. and Populus sp. The sediment stratigraphy and age-depth relationships give no clear indication of post-depositional disturbance, although a possible short-lived hiatus occurs around 6500 cal. BP. The early pollen record from thermophilous trees could indicate that there may have been some downwash following sediment desiccation through wood peat layers deposited between c. 6500 and 10,000 cal. BP, but the overall biostratigraphy is consistent with other Danish small hollow records. (Less)
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author
; ; ; and
organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
broadleaved trees, charcoal, Denmark, forest history, macrofossils, pollen analysis
in
The Holocene
volume
23
issue
2
pages
243 - 254
publisher
SAGE Publications
external identifiers
  • wos:000313980100008
  • scopus:84872903771
ISSN
0959-6836
DOI
10.1177/0959683612455549
language
English
LU publication?
yes
id
ada371c7-c2c8-41a8-9bd1-893241633655 (old id 3591093)
date added to LUP
2016-04-01 10:16:32
date last changed
2022-04-27 20:27:58
@article{ada371c7-c2c8-41a8-9bd1-893241633655,
  abstract     = {{We report on a full-Holocene pollen, charcoal and macrofossil record from a small forest hollow in Gribskov, eastern Denmark. The Fagus sylvatica pollen record suggests the establishment of a small Fagus population at Gribskov in the early Holocene together with early establishment of other thermophilous broadleaved trees, including Quercus sp., Tilia sp. and Ulmus sp. The macrofossils contribute to the vegetation reconstruction with evidence for local presence of species with low pollen productivity or easily degraded pollen types such as Populus. The charcoal record shows frequent burning during two periods of the early Holocene and from c. 3000 cal. BP to present. The early-Holocene part of the record indicates a highly disturbed forest ecosystem with frequent fires and abundant macrofossils of particularly Betula sp. and Populus sp. The sediment stratigraphy and age-depth relationships give no clear indication of post-depositional disturbance, although a possible short-lived hiatus occurs around 6500 cal. BP. The early pollen record from thermophilous trees could indicate that there may have been some downwash following sediment desiccation through wood peat layers deposited between c. 6500 and 10,000 cal. BP, but the overall biostratigraphy is consistent with other Danish small hollow records.}},
  author       = {{Overballe-Petersen, Mette Venas and Nielsen, Anne Birgitte and Hannon, Gina E. and Halsall, Karen and Bradshaw, Richard H. W.}},
  issn         = {{0959-6836}},
  keywords     = {{broadleaved trees; charcoal; Denmark; forest history; macrofossils; pollen analysis}},
  language     = {{eng}},
  number       = {{2}},
  pages        = {{243--254}},
  publisher    = {{SAGE Publications}},
  series       = {{The Holocene}},
  title        = {{Long-term forest dynamics at Gribskov, eastern Denmark with early-Holocene evidence for thermophilous broadleaved tree species}},
  url          = {{http://dx.doi.org/10.1177/0959683612455549}},
  doi          = {{10.1177/0959683612455549}},
  volume       = {{23}},
  year         = {{2013}},
}