Rapid Holocene sea-level and climate change in the Black Sea: An evaluation of the Balabanov sea-level curve

2011 ◽  
Author(s):  
Ronald E. Martin ◽  
Valentina Yanko-Hombach
Keyword(s):  
Climate Change ◽  
Sea Level ◽  
Black Sea ◽  
The Black Sea ◽  
Level Curve ◽  
Holocene Sea Level

CORRELATION OF THE BLACK, MARMARA AND AEGEAN SEAS DURING THE HOLOCENE

2017 ◽  
Author(s):  
Nikolay Esin ◽  
Nikolay Esin ◽  
Vladimir Ocherednik ◽  
Vladimir Ocherednik
Keyword(s):  
Mathematical Model ◽  
Sea Level ◽  
Black Sea ◽  
Aegean Sea ◽  
The Black Sea ◽  
Sea Level Changes ◽  
The Holocene

A mathematical model describing the change in the Black Sea level depending on the Aegean Sea level changes is presented in the article. Calculations have shown that the level of the Black Sea has been repeating the course of the Aegean Sea level for the last at least 6,000 years. And the level of the Black Sea above the Aegean Sea level in the tens of centimeters for this period of time.

scholarly journals Flexure due to the Messinian-Pontian sea level drop in the Black Sea

2009 ◽  
Vol 10 (10) ◽  
pp. n/a-n/a ◽  
Author(s):  
J. Bartol ◽  
R. Govers
Keyword(s):  
Sea Level ◽  
Black Sea ◽  
The Black Sea

Internal and external forcing of sea level variability in the Black Sea

2015 ◽  
Vol 45 (9-10) ◽  
pp. 2633-2646 ◽  
Author(s):  
Denis L. Volkov ◽  
Felix W. Landerer
Keyword(s):  
Sea Level ◽  
Black Sea ◽  
The Black Sea ◽  
External Forcing ◽  
Sea Level Variability

Oscillations of the Black Sea sea level in the north part of the coast

1999 ◽  
Vol 10 (2) ◽  
pp. 123-130
Author(s):  
Yu. I. Goryachkin ◽  
V. A. Ivanov ◽  
Yu. A. Stepanyants
Keyword(s):  
Sea Level ◽  
Black Sea ◽  
The Black Sea ◽  
The North ◽  
North Part

The Black Sea level trends from tide gages and satellite altimetry

2013 ◽  
Vol 38 (5) ◽  
pp. 329-333 ◽  
Author(s):  
A. A. Kubryakov ◽  
S. V. Stanichnyi
Keyword(s):  
Sea Level ◽  
Black Sea ◽  
Satellite Altimetry ◽  
The Black Sea

GNSS Reflectometry of the Black Sea Level in the Experiments at the Stationary Oceanographic Platform

2018 ◽  
Vol 73 (4) ◽  
pp. 422-427 ◽  
Author(s):  
A. M. Padokhin ◽  
G. A. Kurbatov ◽  
M. O. Nazarenko ◽  
V. E. Smolov
Keyword(s):  
Sea Level ◽  
Black Sea ◽  
The Black Sea ◽  
Gnss Reflectometry

scholarly journals Lack of marine entry into Marmara and Black Sea-lakes indicate low relative sea level during MIS 3 in the northeastern Mediterranean

2019 ◽  
Author(s):  
Anastasia G. Yanchilina ◽  
Celine Grall ◽  
William B. F. Ryan ◽  
Jerry F. McManus ◽  
Candace O. Major
Keyword(s):  
Sea Level ◽  
Black Sea ◽  
Global Ocean ◽  
The Black Sea ◽  
Marmara Sea ◽  
Independent Data ◽  
Relative Sea Level ◽  
Mis 3 ◽  
History Of ◽  
Marine Isotope Stage 3

Abstract. The Marine Isotope Stage 3 (MIS 3) is considered a period of persistent and rapid climate and sea level variabilities during which eustatic sea level is observed to have varied by tens of meters. Constraints on local sea level during this time are critical for further estimates of these variabilities. We here present constraints on relative sea level in the Marmara and Black Sea regions in the northeastern Mediterranean, inferred from reconstructions of the history of the connections and disconnections (partial or total) of these seas together with the global ocean. We use a set of independent data from seismic imaging and core-analyses to infer that the Marmara and Black Seas remained connected persistent freshwater lakes that outflowed to the global ocean during the majority of MIS 3. Marine water intrusion during the early MIS-3 stage may have occurred into the Marmara Sea-Lake but not the Black Sea-Lake. This suggests that the relative sea level was near the paleo-elevation of the Bosporus sill and possibly slightly above the Dardanelles paleo-elevation, ~80 mbsl. The Eustatic sea level may have been even lower, considering the isostatic effects of the Eurasian ice sheet would have locally uplifted the topography of the northeastern Mediterrranean.

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