Phytoliths from the Southwest Pacific, Site 591

Phytoliths are described from deep sea sediments at Site 591 in the southwestern Pacific. Their regional distribution is related to the arid and semiarid regions of Australia, from where they were blown by westerly winds into the Tasman Sea area. The stratigraphic record ranges from the middle Mioce...

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Bibliographic Details
Main Authors: Locker, Sigurd, Martini, Erlend
Format: Article in Journal/Newspaper
Language:English
Published: 1985
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/31781/
https://oceanrep.geomar.de/id/eprint/31781/1/dsdp90pt2_22.pdf
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spelling ftoceanrep:oai:oceanrep.geomar.de:31781 2023-05-15T14:13:55+02:00 Phytoliths from the Southwest Pacific, Site 591 Locker, Sigurd Martini, Erlend 1985 text https://oceanrep.geomar.de/id/eprint/31781/ https://oceanrep.geomar.de/id/eprint/31781/1/dsdp90pt2_22.pdf en eng https://oceanrep.geomar.de/id/eprint/31781/1/dsdp90pt2_22.pdf Locker, S. and Martini, E. (1985) Phytoliths from the Southwest Pacific, Site 591. Initial Reports of The Deep Sea Drilling Project, 90 . pp. 1079-1084. Article NonPeerReviewed 1985 ftoceanrep 2023-04-07T15:24:21Z Phytoliths are described from deep sea sediments at Site 591 in the southwestern Pacific. Their regional distribution is related to the arid and semiarid regions of Australia, from where they were blown by westerly winds into the Tasman Sea area. The stratigraphic record ranges from the middle Miocene, at about 14.4 m.y., until the early Pleistocene. A distinct increase in frequencies observed during the Pliocene and a maximum at about 2.5 m.y. coincide with important trends in paleogeography and paleoclimatology: the development of the Antarctic ice cap, the northward drift of the Australian Plate, and the generation of arid conditions on the Australian continent. Article in Journal/Newspaper Antarc* Antarctic Ice cap OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Antarctic Pacific The Antarctic
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
description Phytoliths are described from deep sea sediments at Site 591 in the southwestern Pacific. Their regional distribution is related to the arid and semiarid regions of Australia, from where they were blown by westerly winds into the Tasman Sea area. The stratigraphic record ranges from the middle Miocene, at about 14.4 m.y., until the early Pleistocene. A distinct increase in frequencies observed during the Pliocene and a maximum at about 2.5 m.y. coincide with important trends in paleogeography and paleoclimatology: the development of the Antarctic ice cap, the northward drift of the Australian Plate, and the generation of arid conditions on the Australian continent.
format Article in Journal/Newspaper
author Locker, Sigurd
Martini, Erlend
spellingShingle Locker, Sigurd
Martini, Erlend
Phytoliths from the Southwest Pacific, Site 591
author_facet Locker, Sigurd
Martini, Erlend
author_sort Locker, Sigurd
title Phytoliths from the Southwest Pacific, Site 591
title_short Phytoliths from the Southwest Pacific, Site 591
title_full Phytoliths from the Southwest Pacific, Site 591
title_fullStr Phytoliths from the Southwest Pacific, Site 591
title_full_unstemmed Phytoliths from the Southwest Pacific, Site 591
title_sort phytoliths from the southwest pacific, site 591
publishDate 1985
url https://oceanrep.geomar.de/id/eprint/31781/
https://oceanrep.geomar.de/id/eprint/31781/1/dsdp90pt2_22.pdf
geographic Antarctic
Pacific
The Antarctic
geographic_facet Antarctic
Pacific
The Antarctic
genre Antarc*
Antarctic
Ice cap
genre_facet Antarc*
Antarctic
Ice cap
op_relation https://oceanrep.geomar.de/id/eprint/31781/1/dsdp90pt2_22.pdf
Locker, S. and Martini, E. (1985) Phytoliths from the Southwest Pacific, Site 591. Initial Reports of The Deep Sea Drilling Project, 90 . pp. 1079-1084.
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