Southern Baffin Island mean annual precipitation isotopes modulated by summer and autumn moisture source changes during the past 5800 years

• Published in: Journal of Quaternary Science
• Main Authors: Gorbey, Devon B., Thomas, Elizabeth K., Crump, Sarah E., Hollister, Kayla V., Raynolds, Martha K., Raberg, Jonathan H., de Wet, Gregory, Sepúlveda, Julio, Miller, Gifford H.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2021
• Subjects: Paleontology; Earth and Planetary Sciences (miscellaneous); Arts and Humanities (miscellaneous); Arctic; Baffin Island; Baffin; Labrador Sea; Nunavut
• Online Access: http://dx.doi.org/10.1002/jqs.3390; https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3390; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/jqs.3390

ABSTRACT Paleo water isotope records can elucidate how the Arctic water cycle responded to past climate changes. We analyze the hydrogen isotope composition (δ 2 H) of plant‐derived n ‐alkanoic acids (waxes) from Lake Qaupat, Baffin Island, Nunavut, Canada, to assess moisture sources and seasonality during the past 5.8 ka. We compare this record to a sedimentary ancient DNA ( sed aDNA)‐inferred vascular plant record from the same lake, aiming to overcome the uncertainty of plant community impacts on leaf waxes. As the sed aDNA record reveals a stable plant community after the colonization of Betula sp. at 6.1 ka, we interpret plant wax δ 2 H values to reflect climate, specifically mean annual precipitation δ 2 H. However, the distributions of n ‐alkanoic acid homologs suggest that aquatic mosses, which are not represented in the sed aDNA record, may become more abundant towards the present. Therefore, we cannot exclude the possibility that changes in the plant community cause changes in the plant wax δ 2 H record, particularly long‐chain waxes, which become less abundant through this record. We find that Lake Qaupat mid‐chain plant wax δ 2 H is enriched coincident with high Labrador Sea summer surface temperature, which suggests that local moisture sources in summer and early autumn have the greatest impact on precipitation isotopes in this region.