Multi-proxy evidence for millennial-scale changes in North Pacific Holocene hydroclimate from the Kenai Peninsula lowlands, south-central Alaska

QUATERNARY SCIENCE REVIEWS

卷:241

Article

Broadman, Ellie¹  Kaufman, Darrell S.¹  Henderson, Andrew C. G.²  Berg, Edward E.³  Anderson, R. Scott¹  Leng, Melanie J.^4,5  Stahnke, Sean A.¹  Munoz, Samuel E.⁶ 

[1] No Arizona Univ, Sch Earth & Sustainabil, Flagstaff, AZ 86011 USA

[2] Newcastle Univ, Sch Geog Polit & Sociol, Newcastle Upon Tyne, Tyne & Wear, England

[3] US Fish & Wildlife Serv, Kenai Natl Wildlife Refuge, Soldotna, AK USA

[4] British Geol Survey, Natl Environm Isotope Facil, Isotope Geosci Facil, Nottingham, England

[5] Univ Nottingham, Ctr Environm Geochem, Sch Biosci, Nottingham, England

[6] Northeastern Univ, Marine Sci Ctr, Dept Marine & Environm Sci, Nahant, MA USA

关键词: Diatom oxygen isotopes;    Biogenic silica;    Kenai lowlands;    Aleutian Low;    Hydroclimate;    South-central Alaska;    Holocene;   

DOI  :  10.1016/j.quascirev.2020.106420

来源: Elsevier

【 摘 要 】

The Holocene hydroclimate of south-central Alaska has been studied extensively, but conflicting interpretations between oxygen isotope paleoclimate datasets are seemingly as common as converging reconstructions, in part due to the challenges of interpreting oxygen isotope ratios in terms of climate. Here, we present a new Holocene record of biogenic silica abundance (BSi), diatom flora, and diatom oxygen isotopes (delta O-18(BSi)) analyzed in sediments from Sunken Island Lake (SIL) in the Kenai Peninsula lowlands, which we interpret in the context of previously published paleoclimate records, and use to understand regional changes in hydroclimate. Changes in lake level documented by aerial photography coupled with a survey of regional lake water isotopes indicate SIL is sensitive to changes in the balance of precipitation and evaporation (P-E). However, an analysis of SIL delta O-18(BSi) over the instrumental period indicates that delta O-18(BSi) is sensitive to both P-E and the isotope composition of precipitation (delta O-18(precip)), which is driven by changes in the Aleutian Low atmospheric pressure cell (AL). We attribute a similar to 2 parts per thousand increase in delta O-18(BSi) from 5.5 to 4.5 ka cal BP to a stronger AL, which resulted in the delivery of isotopically heavier precipitation to the Kenai lowlands, and wetter conditions during the late Holocene. These interpretations are supported by late Holocene increases in the relative abundance of planktonic diatoms and BSi-inferred storminess, and by evidence for higher-than-present lake levels on the paleo-shorelines above SIL at similar to 1.5-0.5 ka cal BP. Our dataset demonstrates that this region was characterized by relatively low lake levels and dry climate in the early Holocene, a strengthening of the AL in the late Holocene, and wetter climate during the late Holocene until recent decades. (C) 2020 Elsevier Ltd. All rights reserved.

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