A series of simple hydraulic calculations has been performed to examine some of the questions associated with the reconnection of the Black Sea to the Mediterranean through the Turkish Strait System during the Holocene. Ryan et al.'s catastrophic flood scenario, whereby the erosive power of the marine in-fluxes, initiated after eustatic sea level reached the sill depth, opened up the Bosphorus, allowing saline water to pour into the Black Sea and filling it on a short time scale, is examined. The calculations show that although it might be possible to fill the palaeo-Black Sea within the order of a decade, a 1-2 year filling time scale is not physically possible. A hydraulic model is also used to examine the more traditional connection hypo...
Author Posting. © American Geophysical Union, 2004. This article is posted here by permission of Am...
The sediment infill over the Paleozoic bedrock in the Bosphorus Strait consists of four sedimentary ...
The Marmara Sea (area 11,350 km2; volume 3,378 km3; central basins >1100 m deep) straddles the North...
The present study attempts to estimate the time of infilling of the Black Sea with Mediterranean wat...
Controversy surrounds reconnection of the Black Sea and Mediterranean during Holocene sea-level rise...
Abstract: The Late Quaternary history of connection of the Black Sea to the Eastern Mediterranean ha...
Chloride and δ18O compositions of interstitial water extracted from a long sediment core retrieved f...
Previous studies concluded that the Bosphorus Strait was formed during the Quaternary by fluvial inc...
[1] We apply a shock-capturing numerical model based on the single-layer shallow water equations to ...
The Black Sea becomes periodically isolated from the global ocean during each glacial period. This o...
Core M02-45 recovered 9.5m of a similar to 12m-thick transgressive succession on the SW Black Sea sh...
A catastrophic flooding of the Black Sea basin was proposed to have occurred during its reconnection...
Detailed interpretation of single-channel air-gun and deep-tow boomer profiles demonstrates that the...
Benthic foraminifera were studied from four gravity cores that penetrated Holocene marine sediments ...
The Black Sea is an essentially isolated sea connected to the Mediterranean Sea through two narrow a...
Author Posting. © American Geophysical Union, 2004. This article is posted here by permission of Am...
The sediment infill over the Paleozoic bedrock in the Bosphorus Strait consists of four sedimentary ...
The Marmara Sea (area 11,350 km2; volume 3,378 km3; central basins >1100 m deep) straddles the North...
The present study attempts to estimate the time of infilling of the Black Sea with Mediterranean wat...
Controversy surrounds reconnection of the Black Sea and Mediterranean during Holocene sea-level rise...
Abstract: The Late Quaternary history of connection of the Black Sea to the Eastern Mediterranean ha...
Chloride and δ18O compositions of interstitial water extracted from a long sediment core retrieved f...
Previous studies concluded that the Bosphorus Strait was formed during the Quaternary by fluvial inc...
[1] We apply a shock-capturing numerical model based on the single-layer shallow water equations to ...
The Black Sea becomes periodically isolated from the global ocean during each glacial period. This o...
Core M02-45 recovered 9.5m of a similar to 12m-thick transgressive succession on the SW Black Sea sh...
A catastrophic flooding of the Black Sea basin was proposed to have occurred during its reconnection...
Detailed interpretation of single-channel air-gun and deep-tow boomer profiles demonstrates that the...
Benthic foraminifera were studied from four gravity cores that penetrated Holocene marine sediments ...
The Black Sea is an essentially isolated sea connected to the Mediterranean Sea through two narrow a...
Author Posting. © American Geophysical Union, 2004. This article is posted here by permission of Am...
The sediment infill over the Paleozoic bedrock in the Bosphorus Strait consists of four sedimentary ...
The Marmara Sea (area 11,350 km2; volume 3,378 km3; central basins >1100 m deep) straddles the North...