2021
DOI: 10.1130/ges02359.1
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Late Pleistocene and early Holocene sea-level history and glacial retreat interpreted from shell-bearing marine deposits of southeastern Alaska, USA

Abstract: We leverage a data set of >720 shell-bearing marine deposits throughout southeastern Alaska (USA) to develop updated relative sea-level curves that span the past ∼14,000 yr. This data set includes site location, elevation, description when available, and 436 14C ages, 45 of which are published here for the first time. Our sea-level curves suggest a peripheral forebulge developed west of the retreating Cordilleran Ice Sheet (CIS) margin between ca. 17,000 and 10,800 calibrated yr B.P. By 14,870 ± 630 to … Show more

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Cited by 12 publications
(8 citation statements)
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“…Hence, in the case of polar bears and brown bears, which have clearly demonstrated gene flow following their divergence (see below), the split time estimated using SMC++ is most likely underestimated, possibly associated instead with cessation of gene flow between the two lineages. Likewise, the ∼11.8-ka split time estimate for ABC-A and ABC-BC brown bears more likely reflects interpopulational gene flow termination accompanying fragmentation of Alexander Archipelago landmasses by sea-level rise at the end of the last Ice Age ( 32 ).…”
Section: Resultsmentioning
confidence: 99%
“…Hence, in the case of polar bears and brown bears, which have clearly demonstrated gene flow following their divergence (see below), the split time estimated using SMC++ is most likely underestimated, possibly associated instead with cessation of gene flow between the two lineages. Likewise, the ∼11.8-ka split time estimate for ABC-A and ABC-BC brown bears more likely reflects interpopulational gene flow termination accompanying fragmentation of Alexander Archipelago landmasses by sea-level rise at the end of the last Ice Age ( 32 ).…”
Section: Resultsmentioning
confidence: 99%
“…Recent studies based on cosmogenic exposure dating have demonstrated that areas in SE Alaska above sea level today were covered in ice during the local LGM (20–17 ka) and deglaciation began between ~16.3 to 15.1 ka along the coast (Lesnek et al, 2018, 2020; Walcott et al, 2022). Nevertheless, due to considerable sea‐level changes in the region (Baichtal et al, 2021; Bard et al, 1990; Shugar et al, 2014), areas that may now be submerged could have served as Pleistocene coastal refugia (Lesnek et al, 2020; Walcott et al, 2022), which could help explain the high level of endemism in the archipelago (MacDonald & Cook, 2007). For example, native bears in the region today appear to represent populations distinct from the mainland, suggesting long‐term isolation in the archipelago (Byun et al, 1997; Davison et al, 2011; MacDonald & Cook, 2007; Puckett et al, 2015; Talbot & Shields, 1996; Wooding & Ward, 1997).…”
Section: Discussionmentioning
confidence: 99%
“…After the LGM deglaciation, sea levels in the region varied and at time surpassed the modern sea level. During the early Holocene, sea levels on Prince of Wales Island were higher when compared to the northern islands (Baichtal et al, 2021). Furthermore, temperatures in the mid‐Holocene decreased resulting in an abrupt cooling event ~8.2 ka (Rohling & Pälike, 2005).…”
Section: Discussionmentioning
confidence: 99%
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