The Ioffe Drift (Hardcover, 1st ed. 2021)

The Discovery of the calcareous Ioffe Drift in the SW Atlantic in 2010 opens new perspectives in the contourite theory. Although demonstrating similar behavior relative to bottom water dynamics, rather rare and poorly studied calcareous contourites differ from their terrigenous analogs in origin, grain-size distribution, chemical and mineral composition of sedimentary particles. The detailed multidisciplinary study of the Ioffe Drift produces new knowledge on biogenic contourites deposited in pelagic realm, in conditions of low biological productivity and terrigenous material supply, under the influence of the Antarctic Bottom Water flow from the Vema Channel. The major intervals of prevailing erosion are inferred on the drift from 2.51/2.59 to 1.9 Ma and from 1.6 to 0.81 Ma thus indicating strong paleoceanographic changes most likely associated with the reorganization of deep-sea circulation and increased bottom water production in the Southern Ocean during the Early Pleistocene and, in particular, around the Mid-Pleistocene Transition.

General

Imprint:	Springer Nature Switzerland AG
Country of origin:	Switzerland
Series:	Springer Geology
Release date:	October 2021
First published:	2021
Editors:	Ivar Murdmaa • Elena Ivanova
Dimensions:	235 x 155mm (L x W)
Format:	Hardcover
Pages:	195
Edition:	1st ed. 2021
ISBN-13:	978-3-03-082870-7
Categories:	Books > Science & Mathematics > Physics > Applied physics & special topics > Geophysics Books > Earth & environment > Earth sciences > Geology & the lithosphere > Soil science, sedimentology Books > Earth & environment > Earth sciences > The hydrosphere > Oceanography (seas) Promotions
LSN:	3-03-082870-0
Barcode:	9783030828707

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