Inputs of glacially derived dissolved and colloidal iron to the coastal ocean and implications for primary productivity-Reference-Cited by-同舟云学术

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Inputs of glacially derived dissolved and colloidal iron to the coastal ocean and implications for primary productivity

Published:2008-08-05 Issue:3 Volume:22 Page:n/a-n/a
ISSN:0886-6236
Container-title:Global Biogeochemical Cycles
language:en
Short-container-title:Global Biogeochem. Cycles

Author:

Statham Peter J.¹,Skidmore Mark²,Tranter Martyn³

Affiliation:

1. School of Ocean and Earth Science, National Oceanography Centre; University of Southampton; Southampton; UK

2. Department of Earth Sciences; Montana State University; Bozeman; Montana; USA

3. School of Geographical Sciences; University of Bristol; Bristol; UK

Publisher

American Geophysical Union (AGU)

Subject

Atmospheric Science,General Environmental Science,Environmental Chemistry,Global and Planetary Change

Reference59 articles.

1. Chemical weathering in glacial environments;Anderson;Geology,1997

2. Glaciers and nutrients in Arctic Seas;Apollonio;Science,1973

3. A biogeochemical study of the island mass effect in the context of the iron hypothesis: Kerguelen Islands, Southern Ocean;Blain;Deep Sea Res., Part I,2001

4. Availability of iron and major nutrients for phytoplankton in the northeast Atlantic Ocean;Blain;Limnol. Oceanogr.,2004

5. Effect of natural iron fertilization on carbon sequestration in the Southern Ocean;Blain;Nature,2007

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