Nutrient conditions in the subpolar North Atlantic during the last glacial period reconstructed from foraminifera-bound nitrogen isotopes-Reference-Cited by-同舟云学术

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Nutrient conditions in the subpolar North Atlantic during the last glacial period reconstructed from foraminifera-bound nitrogen isotopes

Published:2013-03 Issue:1 Volume:28 Page:79-90
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Straub M.¹,Tremblay M. M.²,Sigman D. M.³,Studer A. S.¹,Ren H.⁴,Toggweiler J. R.⁵,Haug G. H.¹

Affiliation:

1. Geological Institute; Department of Earth Sciences, ETH Zurich; Zurich; Switzerland

2. Department of Earth and Planetary Science; University of California at Berkeley; Berkeley; California; USA

3. Department of Geosciences; Princeton University; Princeton; New Jersey; USA

4. Lamont-Doherty Earth Observatory; Columbia University; Palisades; New York; USA

5. Geophysical Fluid Dynamics Laboratory; National Oceanic and Atmospheric Administration; Princeton; New Jersey; USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference81 articles.

1. Isotopic Tracers of the Marine Nitrogen Cycle: Present and Past

2. Sedimentary nitrogen isotopic ratio as a recorder for surface ocean nitrate utilization;Altabet;Global Biogeochem. Cycles,1994

3. Nitrogen isotope biogeochemistry of the Antarctic Polar Frontal Zone at 170 degrees W;Altabet;Deep Sea Res. Part II: Topical Studies Oceanogr.,2001

4. Seasonal and depth-related changes in the source of sinking particles in the North Atlantic;Altabet;Nature,1991

5. Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2;Anderson;Science,2009

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