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Cited by 324

The DOI matches its Crossref record; 14 of the 14 references it cites were found in a registry or an index.

Radiocarbon Geochemistry of Modern and Ancient Arctic Lake Systems, Baffin Island, Canada

Abbott, Mark B., Stafford, Thomas W.·1996·Quaternary Research

Abstract

The accuracy of Arctic lake chronologies has been assessed by measuring the 14 C activities of modern carbon sources and applying these isotopic mass balances to dating fossil lake materials. Small (<1 km 2) shallow (<25 m) Arctic lakes with watersheds <12 km 2 have soil and peat stratigraphic sections with 14 C activities ranging from 98 to 51% Modern. The 14 C activity of particulate organic carbon, dissolved organic carbon, and dissolved inorganic carbon from lake and stream waters ranges from 121 to 95% Modern. The sediment–water interface of the studied lakes shows consistent 14 C ages of ∼1000 14 C yr, although the 14 C activity of living aquatic vegetation is 115% Modern. Radiocarbon measurements of components of the lacustrine carbon pool imply that the ∼1000 14 C yr age of the sediment–water interface results from deposition of 14 C-depleted organic matter derived from the watershed.

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Crossref · 10.1006/qres.1996.0031

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Metadata

Authors
Abbott, M. B., & Stafford, T. W.
Venue
Quaternary Research
Published
1996-05
Volume
45
Issue
3
Pages
300-311
ISSN
  • 0033-5894 (ISSN-L)
  • 1096-0287
OpenAlex
W2016895904
Cited by
324
References
14
FWCI
6.02
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Radiocarbon Geochemistry of Modern and Ancient Arctic Lake Systems, Baffin Island, Canada. https://app.cochat.ai/papers/10.1006/qres.1996.0031
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Abbott, M. B., & Stafford, T. W. (1996). Radiocarbon Geochemistry of Modern and Ancient Arctic Lake Systems, Baffin Island, Canada. Quaternary Research. https://doi.org/10.1006/qres.1996.0031

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