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The Ioffe Drift

Ivanova, Elena.

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The Ioffe Drift

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	The Ioffe Drift/ edited by Ivar Murdmaa, Elena Ivanova.
其他作者:	Ivanova, Elena.
出版者:	Cham :Springer International Publishing : : 2021.,
面頁冊數:	vii, 195 p. :ill. (some col.), digital ;24 cm.
內容註:	Introduction -- Regional setting -- Regional stratigraphic frames based on calcareous microfossils -- Materials -- The Ioffe Drift geomorphology and seismic stratigraphy -- Lithology and sedimentology -- Micropaleontology and stratigraphy -- Ferromanganese nodules -- Hiatuses and core correlations -- The Ioffe Drift history and mechanisms of sedimentation -- Conclusions and Perspectives.
Contained By:	Springer Nature eBook
標題:	Nannofossils. -
電子資源:	https://doi.org/10.1007/978-3-030-82871-4
ISBN:	9783030828714

The Ioffe Drift
The Ioffe Drift[electronic resource] /edited by Ivar Murdmaa, Elena Ivanova. - Cham :Springer International Publishing :2021. - vii, 195 p. :ill. (some col.), digital ;24 cm. - Springer geology,2197-9553. - Springer geology..

Introduction -- Regional setting -- Regional stratigraphic frames based on calcareous microfossils -- Materials -- The Ioffe Drift geomorphology and seismic stratigraphy -- Lithology and sedimentology -- Micropaleontology and stratigraphy -- Ferromanganese nodules -- Hiatuses and core correlations -- The Ioffe Drift history and mechanisms of sedimentation -- Conclusions and Perspectives.

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.

ISBN: 9783030828714

Standard No.: 10.1007/978-3-030-82871-4doiSubjects--Topical Terms:

3521926
Nannofossils.

LC Class. No.: QE719 / .I64 2021

Dewey Class. No.: 561.93

The Ioffe Drift
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505 0 $a Introduction -- Regional setting -- Regional stratigraphic frames based on calcareous microfossils -- Materials -- The Ioffe Drift geomorphology and seismic stratigraphy -- Lithology and sedimentology -- Micropaleontology and stratigraphy -- Ferromanganese nodules -- Hiatuses and core correlations -- The Ioffe Drift history and mechanisms of sedimentation -- Conclusions and Perspectives.
520 $a 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.
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