气候变化领域集成服务门户(CCPortal): Climate-driven connectivity changes of the Black Sea since 430 ka: Testing a dual palynological and geochemical approach

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DOI	10.1016/j.palaeo.2020.110069
	Climate-driven connectivity changes of the Black Sea since 430 ka: Testing a dual palynological and geochemical approach
	Hoyle T.M.; Bista D.; Flecker R.; Krijgsman W.; Sangiorgi F.
发表日期	2021
ISSN	0031-0182
卷号	561
英文摘要	The Black Sea experienced multiple episodes of connection with both the Mediterranean and Caspian seas during the Quaternary. Global sea-level variation has been proposed as the main driver of changes in Mediterranean-Black Sea connectivity, while positive water budgets drove Caspian overspill. We present a new, two proxy, low-resolution record from the Black Sea that allows reconstruction of connectivity history from 430 to 50 ka: dinoflagellate cysts (dinocysts) provide direct evidence for properties of surface waters and strontium isotopes constrain the source(s) of water entering the basin. Dinocysts and 87Sr/86Sr suggest that the Black Sea was isolated from the Mediterranean during global sea-level lowstands associated with glacials MIS 4, 8 and 10. Both proxies also strongly suggest that marine (Mediterranean) water flowed into the Black Sea during the eustatic highstands associated with peak interglacials during MIS 5 and 9. However, while the contribution of marine waters during MIS 5e was similar to the present day, lower 87Sr/86Sr during MIS 9 suggests lower than present input. Connectivity during MIS 11, MIS 7 and MIS 6 is more enigmatic. Lower 87Sr/86Sr than those of the isolated Black Sea and dinocyst assemblages dominated by species of Paratethyan lineage are compatible with input from the Caspian Sea. Dinocyst taxa recovered in MIS 11 can be found in both the Caspian Sea and the Black Sea today. All four interglacials studied contain different dinocyst assemblages, suggesting that different conditions may have prevailed during each warm period. However, high-resolution studies are needed to confirm this observation. Further work on the same sequence could be valuable in elucidating the connectivity history of the Black Sea over the glacial-interglacial cycles of the late Quaternary. © 2020
英文关键词	Connectivity; Dinoflagellate cysts; Late Quaternary; Pontocaspian region; Strontium isotopes
语种	英语
scopus关键词	climate change; connectivity; dinoflagellate cyst; geochemistry; glacial-interglacial cycle; interglacial; lowstand; marine isotope stage; paleoceanography; palynology; Quaternary; reconstruction; sea level change; testing method; Black Sea; Caspian Sea; Dinophyceae
来源期刊	Palaeogeography, Palaeoclimatology, Palaeoecology
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/150259
作者单位	Department of Earth Sciences, Utrecht University, Vening Meineszgebouw A, Princetonlaan 8a, Utrecht, 3584 CB, Netherlands; BRIDGE, School of Geographical Sciences and Cabot Institute, University of Bristol, University Road, Bristol, BS8 1SS, United Kingdom
推荐引用方式 GB/T 7714	Hoyle T.M.,Bista D.,Flecker R.,et al. Climate-driven connectivity changes of the Black Sea since 430 ka: Testing a dual palynological and geochemical approach[J],2021,561.
APA	Hoyle T.M.,Bista D.,Flecker R.,Krijgsman W.,&Sangiorgi F..(2021).Climate-driven connectivity changes of the Black Sea since 430 ka: Testing a dual palynological and geochemical approach.Palaeogeography, Palaeoclimatology, Palaeoecology,561.
MLA	Hoyle T.M.,et al."Climate-driven connectivity changes of the Black Sea since 430 ka: Testing a dual palynological and geochemical approach".Palaeogeography, Palaeoclimatology, Palaeoecology 561(2021).