Bioactive trace metal time series during Austral summer in Ryder Bay, Western Antarctic Peninsula-Reference-Cited by-同舟云学术

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Bioactive trace metal time series during Austral summer in Ryder Bay, Western Antarctic Peninsula

Published:2017-05 Issue: Volume:139 Page:103-119
ISSN:0967-0645
Container-title:Deep Sea Research Part II: Topical Studies in Oceanography
language:en
Short-container-title:Deep Sea Research Part II: Topical Studies in Oceanography

Author:

Bown Johann,Laan Patrick,Ossebaar Sharyn,Bakker Karel,Rozema Patrick,de Baar Hein J.W.

Funder

Sven Ober (NIOZ)

Netherlands Organisation for Scientific Research (NWO)

Publisher

Elsevier BV

Subject

Oceanography

Reference65 articles.

1. Iron from melting glaciers fuels phytoplankton blooms in the Amundsen Sea (Southern Ocean): phytoplankton characteristics and productivity;Alderkamp;Deep-Sea Res. Part II,2012

2. Seasonal progression of diatom assemblages in surface waters of Ryder Bay, Antarctica;Annett;Polar Biol.,2010

3. Comparative roles of upwelling and glacial iron sources to Ryder Bay, coastal western Antarctic Peninsula;Annett;Mar. Chem.,2015

4. Natural iron enrichment around the Antarctic Peninsula in the Southern Ocean;Ardelan;Biogeosciences,2010

5. Impact of a shrinking Arctic ice cover on marine primary production;Arrigo;Geophys. Res. Lett.,2008

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