DOI: 10.1016/j.quascirev.2019.02.011
Scopus记录号: 2-s2.0-85061814304
论文题名: Dinocyst records from deep cores reveal a reversed salinity gradient in the Caspian Sea at 8.5–4.0 cal ka BP
作者: Leroy S.A.G. ; López-Merino L. ; Kozina N.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2019
卷: 209 起始页码: 1
结束页码: 12
语种: 英语
英文关键词: Amu-Darya
; Micropalaeontology dinocyst
; Palaeolimnology
; Pontocaspian
; Quaternary
; Southwestern Asia
; Water flow direction
Scopus关键词: Catchments
; Flow of water
; Hydraulics
; Lakes
; Water levels
; Amu-Darya
; Micropalaeontology dinocyst
; Palaeolimnology
; Ponto-caspian
; Quaternary
; Southwestern Asia
; Water flow direction
; Climate models
; climate modeling
; coastal sediment
; dinoflagellate cyst
; drainage basin
; freshwater environment
; global climate
; global ocean
; paleolimnology
; Quaternary
; salinity
; water flow
; water level
; Amu Darya Basin
; Caspian Sea
; Karakum
; Russian Federation
; Turkmenistan
; Volga River
; Dinophyceae
英文摘要: Understanding the long-term environmental forcings driving Caspian Sea (CS) water levels is of utmost importance, not only owing to its large size, or to the surrounding developing economies but also to improve global climate models and forecasts. However, Late Quaternary CS level changes and their amplitude are mostly documented from incomplete coastal sediment records. Because of the CS idiosyncrasies, that behaves neither as a sea nor as a lake, the methods used to reconstruct water levels in the global ocean or in freshwater lakes do not always apply. Here, we propose a first step toward the use of dinoflagellate cysts records to reconstruct qualitative changes in water mass, focusing on new and published deep-water sedimentary sequences from the south and middle CS basins. Trends in water level changes are reconstructed on the relative proportions of dinocyst assemblages with different levels of brackishness. A higher highstand than previously seen is reconstructed post-Mangyshlak lowstand. A reverse water flow gradient from S to N, not previously detected, is identified at 8.5–8 to 4 cal ka BP. A major turnover in dinocyst assemblage is found at 4 cal ka BP. While the Volga River is the main source of water nowadays, we propose that the source of water to maintain the 8.5–8 to 4 cal ka BP highstand is the now-disconnected drainage basin of the Amu-Darya. The CS was at that time most likely strongly influenced by low latitude climates, with more precipitation over the Karakum and, perhaps, even indirect monsoonal influence. © 2019 Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/117358
Appears in Collections: 气候变化与战略
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Recommended Citation:
Leroy S.A.G.,López-Merino L.,Kozina N.. Dinocyst records from deep cores reveal a reversed salinity gradient in the Caspian Sea at 8.5–4.0 cal ka BP[J]. Quaternary Science Reviews,2019-01-01,209