The environmental water of the middle Eocene Arctic:Evidence from δD, δ18O and δ13C within specific compounds
The extensive vertical exposure (> 150 m) of terrestrial sediments on Axel Heiberg Island, which contain thick fossiliferous lignites, presents an exceptional opportunity to follow the establishment and re-establishment of Arctic Metasequoia forests during the middle Eocene. We compared δD values...
Published in: | Palaeogeography, Palaeoclimatology, Palaeoecology |
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2009
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Online Access: | https://researchers.mq.edu.au/en/publications/d0d15737-56a2-48ab-9441-97d296246c93 https://doi.org/10.1016/j.palaeo.2008.09.016 http://www.scopus.com/inward/record.url?scp=57749199715&partnerID=8YFLogxK |
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ftmacquarieunicr:oai:https://researchers.mq.edu.au:publications/d0d15737-56a2-48ab-9441-97d296246c93 2024-06-23T07:48:32+00:00 The environmental water of the middle Eocene Arctic:Evidence from δD, δ18O and δ13C within specific compounds Jahren, A. Hope Byrne, Monica C. Graham, Heather V. Sternberg, Leonel S L Summons, Roger E. 2009-01-01 https://researchers.mq.edu.au/en/publications/d0d15737-56a2-48ab-9441-97d296246c93 https://doi.org/10.1016/j.palaeo.2008.09.016 http://www.scopus.com/inward/record.url?scp=57749199715&partnerID=8YFLogxK eng eng info:eu-repo/semantics/restrictedAccess Jahren , A H , Byrne , M C , Graham , H V , Sternberg , L S L & Summons , R E 2009 , ' The environmental water of the middle Eocene Arctic : Evidence from δD, δ18O and δ13C within specific compounds ' , Palaeogeography, Palaeoclimatology, Palaeoecology , vol. 271 , no. 1-2 , pp. 96-103 . https://doi.org/10.1016/j.palaeo.2008.09.016 article 2009 ftmacquarieunicr https://doi.org/10.1016/j.palaeo.2008.09.016 2024-06-12T23:47:21Z The extensive vertical exposure (> 150 m) of terrestrial sediments on Axel Heiberg Island, which contain thick fossiliferous lignites, presents an exceptional opportunity to follow the establishment and re-establishment of Arctic Metasequoia forests during the middle Eocene. We compared δD values in n-alkanes of chain length 23, 25, 27 and 29 with δ 18 O values in phenylglucosazone (P-G) derived from α-cellulose; we also analyzed %-abundance of ferns, gymnosperms and angiosperms using pollen and spores isolated from each lignite. Our results showed that forest composition was altered upon uplift, as gymnosperms became more abundant within the relatively well-drained upland sediments. This was also reflected in the small (1‰), but significant, increase in the δ 13 C value of TOM from lowland to upland environments. However, neither the δD values of n-alkanes nor the δ 18 O in P-G were statistically different in the upland sediments, as compared to the lowland sediments; from this we inferred that the oxygen isotope signature of environmental water available to the forests for plant growth was relatively uniform throughout the time of the fossil forests. The δD value of environmental water implied by both n-alkanes and P-G ranged from - 168 to - 131% and was considerably enriched compared to all environmental water samples available from the modern Arctic region (< - 180%). In addition to indicating a warmer Eocene Arctic, subject to meteoric transport patterns different from today's, these results argue against the presence of an Eocene polar ice cap. Article in Journal/Newspaper Arctic Arctic Axel Heiberg Island Polar Ice Cap Macquarie University Research Portal Arctic Axel Heiberg Island ENVELOPE(-91.001,-91.001,79.752,79.752) Heiberg ENVELOPE(13.964,13.964,66.424,66.424) Palaeogeography, Palaeoclimatology, Palaeoecology 271 1-2 96 103 |
institution |
Open Polar |
collection |
Macquarie University Research Portal |
op_collection_id |
ftmacquarieunicr |
language |
English |
description |
The extensive vertical exposure (> 150 m) of terrestrial sediments on Axel Heiberg Island, which contain thick fossiliferous lignites, presents an exceptional opportunity to follow the establishment and re-establishment of Arctic Metasequoia forests during the middle Eocene. We compared δD values in n-alkanes of chain length 23, 25, 27 and 29 with δ 18 O values in phenylglucosazone (P-G) derived from α-cellulose; we also analyzed %-abundance of ferns, gymnosperms and angiosperms using pollen and spores isolated from each lignite. Our results showed that forest composition was altered upon uplift, as gymnosperms became more abundant within the relatively well-drained upland sediments. This was also reflected in the small (1‰), but significant, increase in the δ 13 C value of TOM from lowland to upland environments. However, neither the δD values of n-alkanes nor the δ 18 O in P-G were statistically different in the upland sediments, as compared to the lowland sediments; from this we inferred that the oxygen isotope signature of environmental water available to the forests for plant growth was relatively uniform throughout the time of the fossil forests. The δD value of environmental water implied by both n-alkanes and P-G ranged from - 168 to - 131% and was considerably enriched compared to all environmental water samples available from the modern Arctic region (< - 180%). In addition to indicating a warmer Eocene Arctic, subject to meteoric transport patterns different from today's, these results argue against the presence of an Eocene polar ice cap. |
format |
Article in Journal/Newspaper |
author |
Jahren, A. Hope Byrne, Monica C. Graham, Heather V. Sternberg, Leonel S L Summons, Roger E. |
spellingShingle |
Jahren, A. Hope Byrne, Monica C. Graham, Heather V. Sternberg, Leonel S L Summons, Roger E. The environmental water of the middle Eocene Arctic:Evidence from δD, δ18O and δ13C within specific compounds |
author_facet |
Jahren, A. Hope Byrne, Monica C. Graham, Heather V. Sternberg, Leonel S L Summons, Roger E. |
author_sort |
Jahren, A. Hope |
title |
The environmental water of the middle Eocene Arctic:Evidence from δD, δ18O and δ13C within specific compounds |
title_short |
The environmental water of the middle Eocene Arctic:Evidence from δD, δ18O and δ13C within specific compounds |
title_full |
The environmental water of the middle Eocene Arctic:Evidence from δD, δ18O and δ13C within specific compounds |
title_fullStr |
The environmental water of the middle Eocene Arctic:Evidence from δD, δ18O and δ13C within specific compounds |
title_full_unstemmed |
The environmental water of the middle Eocene Arctic:Evidence from δD, δ18O and δ13C within specific compounds |
title_sort |
environmental water of the middle eocene arctic:evidence from δd, δ18o and δ13c within specific compounds |
publishDate |
2009 |
url |
https://researchers.mq.edu.au/en/publications/d0d15737-56a2-48ab-9441-97d296246c93 https://doi.org/10.1016/j.palaeo.2008.09.016 http://www.scopus.com/inward/record.url?scp=57749199715&partnerID=8YFLogxK |
long_lat |
ENVELOPE(-91.001,-91.001,79.752,79.752) ENVELOPE(13.964,13.964,66.424,66.424) |
geographic |
Arctic Axel Heiberg Island Heiberg |
geographic_facet |
Arctic Axel Heiberg Island Heiberg |
genre |
Arctic Arctic Axel Heiberg Island Polar Ice Cap |
genre_facet |
Arctic Arctic Axel Heiberg Island Polar Ice Cap |
op_source |
Jahren , A H , Byrne , M C , Graham , H V , Sternberg , L S L & Summons , R E 2009 , ' The environmental water of the middle Eocene Arctic : Evidence from δD, δ18O and δ13C within specific compounds ' , Palaeogeography, Palaeoclimatology, Palaeoecology , vol. 271 , no. 1-2 , pp. 96-103 . https://doi.org/10.1016/j.palaeo.2008.09.016 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1016/j.palaeo.2008.09.016 |
container_title |
Palaeogeography, Palaeoclimatology, Palaeoecology |
container_volume |
271 |
container_issue |
1-2 |
container_start_page |
96 |
op_container_end_page |
103 |
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1802638916170285056 |