Further evidence of abrupt Holocene drowning of the Black Sea shelf

被引:78
作者
Ballard, RD
Coleman, DF
Rosenberg, GD
机构
[1] Inst Explorat, Mystic, CT 06355 USA
[2] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA
[3] Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA
[4] Natl Acad Sci, Philadelphia, PA USA
关键词
Black Sea; side-scan sonar; paleoshoreline; radiocarbon dating;
D O I
10.1016/S0025-3227(00)00108-0
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
A 1999 survey of the Black Sea continental shelf off the north central Turkish seaport of Sinop using a side-scan sonar, small remotely operated vehicles, and a series of dredge lowerings located, inspected and sampled an exposed high-energy paleoshoreline at a depth of 155 m. Radiocarbon dating of mollusk shells collected from this ancient beach revealed that the marine flooding of the Black Sea took place between 7460 and 6820 yr B.P. tall ages are reported in radiocarbon years, not calendar years, without correction for reservoir age or dendro-calibration) changing it from a lacustrine to marine environment. This relic surface remained in contact with the bottom waters of the Black Sea for a long period of time before being draped by a thin layer of sapropel mud. Wood samples recovered from this same location were very well preserved and yielded dates as old as 3580 yr B.P. (C) 2000 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:253 / 261
页数:9
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