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Is palynology a credible climate proxy in the Subantarctic?

Nathalie Van der Putten, Cyriel Verbruggen UGent, Svante Björck, Jacques-Louis de Beaulieu, Chris J Barrow and Yves Frenot (2012) HOLOCENE. 22(10). p.1113-1121
abstract
Pollen and spore analysis is the most successfully used palaeobotanical discipline for reconstructing Holocene vegetation and climate history throughout the world. Subantarctic islands are very specific areas. They are located in the circum-Antarctic Southern Ocean in latitudes that are under strong influence of the southern westerly winds, and are characterised by a treeless, phanerogam-poor flora. Palynological research on many of these islands has resulted in diverging conclusions about how to infer climate history from pollen data. In this study we compare pollen data with macrofossil data on the one hand, and the palaeoenvironmental history based on a multiproxy record on the other hand, of two peat sequences from two different subantarctic islands, South Georgia and Île de la Possession (Îles Crozet). We conclude that palynology must be used with caution as a proxy for climate change on these islands, especially when no other proxy data are available. The upland–lowland principle, as it has been applied in pollen studies in the South Indian Ocean islands, results in erroneous conclusions about climate change on Île de la Possession. More palaeoclimatic multiproxy and pollen studies, in combination with pollen–vegetation relationship studies, can, however, contribute to a more reliable model of how to interpret pollen data in the Subantarctic. We want to stress that our conclusions are only based on Holocene records. Consequently, the question remains if palynology can be used as a palaeoclimatic proxy when climatic changes were more pronounced such as during the last glacial–interglacial transition.
Please use this url to cite or link to this publication:
author
organization
year
type
journalArticle (original)
publication status
published
subject
keyword
palynology, Îles Crozet, Holocene, Subantarctic, plant macrofossil analysis, South Georgia, CAL KYR BP, KERGUELEN ISLANDS, HOLOCENE, PEAT, CALIBRATION, HISTORY, RECORD
journal title
HOLOCENE
Holocene
volume
22
issue
10
pages
1113 - 1121
Web of Science type
Article
Web of Science id
000308883300004
JCR category
GEOSCIENCES, MULTIDISCIPLINARY
JCR impact factor
3.218 (2012)
JCR rank
22/170 (2012)
JCR quartile
1 (2012)
ISSN
0959-6836
DOI
10.1177/0959683612441804
language
English
UGent publication?
yes
classification
A1
copyright statement
I have transferred the copyright for this publication to the publisher
id
2141050
handle
http://hdl.handle.net/1854/LU-2141050
date created
2012-06-12 18:08:27
date last changed
2013-07-15 15:41:48
@article{2141050,
  abstract     = {Pollen and spore analysis is the most successfully used palaeobotanical discipline for reconstructing Holocene vegetation and climate history throughout the world. Subantarctic islands are very specific areas. They are located in the circum-Antarctic Southern Ocean in latitudes that are under strong influence of the southern westerly winds, and are characterised by a treeless, phanerogam-poor flora. Palynological research on many of these islands has resulted in diverging conclusions about how to infer climate history from pollen data. In this study we compare pollen data with macrofossil data on the one hand, and the palaeoenvironmental history based on a multiproxy record on the other hand, of two peat sequences from two different subantarctic islands, South Georgia and {\^I}le de la Possession ({\^I}les Crozet). We conclude that palynology must be used with caution as a proxy for climate change on these islands, especially when no other proxy data are available. The upland--lowland principle, as it has been applied in pollen studies in the South Indian Ocean islands, results in erroneous conclusions about climate change on {\^I}le de la Possession. More palaeoclimatic multiproxy and pollen studies, in combination with pollen--vegetation relationship studies, can, however, contribute to a more reliable model of how to interpret pollen data in the Subantarctic. We want to stress that our conclusions are only based on Holocene records. Consequently, the question remains if palynology can be used as a palaeoclimatic proxy when climatic changes were more pronounced such as during the last glacial--interglacial transition.},
  author       = {Van der Putten, Nathalie and Verbruggen, Cyriel and Bj{\"o}rck, Svante and de Beaulieu, Jacques-Louis and Barrow, Chris J and Frenot, Yves},
  issn         = {0959-6836},
  journal      = {HOLOCENE},
  keyword      = {palynology,{\^I}les Crozet,Holocene,Subantarctic,plant macrofossil analysis,South Georgia,CAL KYR BP,KERGUELEN ISLANDS,HOLOCENE,PEAT,CALIBRATION,HISTORY,RECORD},
  language     = {eng},
  number       = {10},
  pages        = {1113--1121},
  title        = {Is palynology a credible climate proxy in the Subantarctic?},
  url          = {http://dx.doi.org/10.1177/0959683612441804},
  volume       = {22},
  year         = {2012},
}

Chicago
Van der Putten, Nathalie, Cyriel Verbruggen, Svante Björck, Jacques-Louis de Beaulieu, Chris J Barrow, and Yves Frenot. 2012. “Is Palynology a Credible Climate Proxy in the Subantarctic?” Holocene 22 (10): 1113–1121.
APA
Van der Putten, N., Verbruggen, C., Björck, S., de Beaulieu, J.-L., Barrow, C. J., & Frenot, Y. (2012). Is palynology a credible climate proxy in the Subantarctic? HOLOCENE, 22(10), 1113–1121.
Vancouver
1.
Van der Putten N, Verbruggen C, Björck S, de Beaulieu J-L, Barrow CJ, Frenot Y. Is palynology a credible climate proxy in the Subantarctic? HOLOCENE. 2012;22(10):1113–21.
MLA
Van der Putten, Nathalie, Cyriel Verbruggen, Svante Björck, et al. “Is Palynology a Credible Climate Proxy in the Subantarctic?” HOLOCENE 22.10 (2012): 1113–1121. Print.