Late Pleistocene – Holocene sea-level dynamics in the Caspian and Black Seas: Data synthesis and Paradoxical interpretations
作者： Valentina Yanko-Hombach , Alexander Kislov
DOI: 10.1016/J.QUAINT.2017.11.030
关键词:
摘要: Abstract Different multidisciplinary data concerning the paleodynamics of sea-level variations in Caspian and Black seas are controversial some aspects. There at least three paradoxes that discussed paper. The Paradox No. 1 relates to Early Late Khvalynian transgressions occurred CS during second part MIS 3 (∼35–25 ka BP) Glacial epoch (∼17–12 BP), respectively. It is unclear what main source or sources water were caused them. 2 emerges from comparison climate events transgressive-regressive cycles Sea Sea. implies large anomalies accordance with global changes (because they influenced by variations). However, other (not so long-lived) fluctuations poorly correlated events. question why climatically-induced did not follow climatic variations. concerns contradiction between massive discharge into Marmara via Bosphorus Strait level Latest Pleistocene-Holocene could exist simultaneously. shown has been solved, on conceptual level. Solutions Paradoxes still lacking: further geological geochronological evidence as well simulation required. Formulation solutions for these should make a major contribution only problems seas’ paleogeography, but also provide help explaining reasons inadequate regional changes. This important context development models future prediction.
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