ABOUT THE WORLD OCEAN LEVEL CHANGE IN HOLOCENE AND EVOLUTION OF THE BLACK SEA COAST AND SHELF
Authors:
1.
Yuzhnoe otdelenie Instituta okeanologii im. P.P. Shirshova RAN
2.
Yuzhnoe otdelenie Instituta okeanologii im. P.P. Shirshova RAN
3.
Yuzhnoe otdelenie Instituta okeanologii im. P.P. Shirshova RAN
Type:
Сonference article
Published:
24.11.2012
Subject area:
CSCSTI 06.01
BISAK NAT010000 Ecology
BISAK NAT045050 Ecosystems & Habitats / Coastal Regions & Shorelines
BISAK NAT025000 Ecosystems & Habitats / Oceans & Seas
BISAK NAT045030 Ecosystems & Habitats / Polar Regions
BISAK SCI081000 Earth Sciences / Hydrology
BISAK SCI092000 Global Warming & Climate Change
BISAK SCI020000 Life Sciences / Ecology
BISAK SCI039000 Life Sciences / Marine Biology
BISAK SOC053000 Regional Studies
BISAK TEC060000 Marine & Naval
BISAK NAT010000 Ecology
BISAK NAT045050 Ecosystems & Habitats / Coastal Regions & Shorelines
BISAK NAT025000 Ecosystems & Habitats / Oceans & Seas
BISAK NAT045030 Ecosystems & Habitats / Polar Regions
BISAK SCI081000 Earth Sciences / Hydrology
BISAK SCI092000 Global Warming & Climate Change
BISAK SCI020000 Life Sciences / Ecology
BISAK SCI039000 Life Sciences / Marine Biology
BISAK SOC053000 Regional Studies
BISAK TEC060000 Marine & Naval
Language:
Russian, English
Keywords:
Mediterranean Sea
Abstract (English):
A method of calculation on local curves of the World ocean eustatic (absolute) variations is presented in this paper. It is shown that vertical motions of the Earth's Crust considerably distort eustatic curve of the sea level change (up to the contrary result). Thus, the local curves present little volume of information. A method of extraction of tectonic component from local curves is proposed. The World ocean level change in Holocene is calculated on local curves of the Mediterranean Sea. It was ascertained that the process of an active erosion of the Black Sea shelf began 3–4 ka.
A method of calculation on local curves of the World ocean eustatic (absolute) variations is presented in this paper. It is shown that vertical motions of the Earth's Crust considerably distort eustatic curve of the sea level change (up to the contrary result). Thus, the local curves present little volume of information. A method of extraction of tectonic component from local curves is proposed. The World ocean level change in Holocene is calculated on local curves of the Mediterranean Sea. It was ascertained that the process of an active erosion of the Black Sea shelf began 3–4 ka.
Keywords:
Mediterranean Sea
Mediterranean Sea
1. net spiska literatury
