Variability in diatom and silicoflagellate assemblages during mid-Pliocene glacial-interglacial cycles determined in Hole U1361A of IODP Expedition 318, Antarctic Wilkes Land Margin

Author:

Armbrecht Linda H.ORCID,Lowe VikkiORCID,Escutia Carlota,Iwai Masao,McKay RobertORCID,Armand Leanne K.

Funder

Australia-New Zealand IODP Consortium

Spanish Ministry of Science and Innovation

European Regional Development Fund

Japan Society for Promotion of Science

Royal Society of New Zealand Rutherford Discovery Fellowship

Publisher

Elsevier BV

Subject

Paleontology,Oceanography

Reference53 articles.

1. Palaeo sea-ice distribution and reconstruction derived from the geological records;Armand,2010

2. Advances in palaeo sea-ice estimation;Armand,2017

3. An expert judgement assessment of future sea level rise from the ice sheets;Bamber;Nat. Clim. Chang.,2013

4. Paleoceanographic and tectonic controls on deposition of the Monterey Formation and related siliceous rocks in California;Barron;Palaeogeogr. Palaeoclimatol. Palaeoecol.,1986

5. The overdeepening hypothesis: how erosional modification of the marine-scape during the early Pliocene altered glacial dynamics on the Antarctic Peninsula's Pacific margin;Bart;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2012

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