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Saulnier-Talbot, Émilie, Leng, Melanie J, Pienitz, Reinhard (2007) Recent climate and stable isotopes in modern surface waters of northernmost Ungava Peninsula, Canada. Canadian Journal of Earth Sciences, 44 (2) 171-180 doi:10.1139/e06-089

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Reference TypeJournal (article/letter/editorial)
TitleRecent climate and stable isotopes in modern surface waters of northernmost Ungava Peninsula, Canada
JournalCanadian Journal of Earth Sciences
AuthorsSaulnier-Talbot, ÉmilieAuthor
Leng, Melanie JAuthor
Pienitz, ReinhardAuthor
Year2007 (February 1)Volume44
Issue2
PublisherCanadian Science Publishing
DOIdoi:10.1139/e06-089Search in ResearchGate
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Mindat Ref. ID484274Long-form Identifiermindat:1:5:484274:7
GUID0
Full ReferenceSaulnier-Talbot, Émilie, Leng, Melanie J, Pienitz, Reinhard (2007) Recent climate and stable isotopes in modern surface waters of northernmost Ungava Peninsula, Canada. Canadian Journal of Earth Sciences, 44 (2) 171-180 doi:10.1139/e06-089
Plain TextSaulnier-Talbot, Émilie, Leng, Melanie J, Pienitz, Reinhard (2007) Recent climate and stable isotopes in modern surface waters of northernmost Ungava Peninsula, Canada. Canadian Journal of Earth Sciences, 44 (2) 171-180 doi:10.1139/e06-089
In(2007, February) Canadian Journal of Earth Sciences Vol. 44 (2) Canadian Science Publishing
Abstract/Notes The isotope composition (δ18O and δD) of surface waters was measured over a 26-month period near three localities situated along the northern coast of Ungava Peninsula, Quebec, Canada. To characterize the present-day local hydrological settings, the oxygen and hydrogen isotope ratios were measured from precipitation and were compared to local and regional climate data. We show that the modern surface waters contain information on climate and that this relationship is likely to be transferred to biotic components within the lakes. These components, once sedimented, are therefore likely to form an archive of climate change. The new data presented here show the possibility of isotope paleoclimatic investigation based on lake sediments in the northern coastal region of Ungava Peninsula.


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