Comparative roles of upwelling and glacial iron sources in Ryder Bay, coastal western Antarctic Peninsula-Reference-Cited by-同舟云学术

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Comparative roles of upwelling and glacial iron sources in Ryder Bay, coastal western Antarctic Peninsula

Published:2015-11 Issue: Volume:176 Page:21-33
ISSN:0304-4203
Container-title:Marine Chemistry
language:en
Short-container-title:Marine Chemistry

Author:

Annett Amber L.,Skiba Marta,Henley Sian F.,Venables Hugh J.,Meredith Michael P.,Statham Peter J.,Ganeshram Raja S.

Funder

NERC, UK

University of Edinburgh)

NSERC (Canada)

Publisher

Elsevier BV

Subject

Water Science and Technology,Environmental Chemistry,General Chemistry,Oceanography

Reference84 articles.

1. Phytoplankton Ecology and Biogeochemistry of the Warming Antarctic Sea-ice Zone;Annett,2013

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

3. Use of radium isotopes to estimate mixing rates and trace sediment inputs to surface waters in northern Marguerite Bay (Antarctic Peninsula);Annett;Antarct. Sci.,2013

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

5. Trends in the solubility of iron, aluminium, manganese and phosphorus in aerosol collected over the Atlantic Ocean;Baker;Mar. Chem.,2006

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