Oceanic phosphorus imbalance: Magnitude of the mid-ocean ridge flank hydrothermal sink-Reference-Cited by-同舟云学术

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Oceanic phosphorus imbalance: Magnitude of the mid-ocean ridge flank hydrothermal sink

Published:2003-09 Issue:17 Volume:30 Page:n/a-n/a
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Wheat C. Geoffrey¹,McManus James²,Mottl Michael J.³,Giambalvo Emily⁴

Affiliation:

1. Global Undersea Research Unit; Univ. of Alaska Fairbanks; Fairbanks Alaska USA

2. College of Oceanic and Atmospheric Sciences; Oregon State Univ.; Corvallis Oregon USA

3. Dept. of Oceanography, SOEST; Univ. of Hawaii; Honolulu Hawaii USA

4. Sandia National Laboratories; Carlsbad New Mexico USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference24 articles.

1. The relationship between near-axis hydrothermal cooling and the spreading rate of mid-ocean ridges;Baker;Earth Plan. Sci. Lett.,1996

2. Phosphorus in sediments of the Amazon River and estuary: Implications for the global flux of phosphorus to the sea;Berner;Geochim. Cosmochim. Acta.,1994

3. Broecker , W. S. T.-H. Peng Tracers in the Sea Lamont-Doherty Geological Observatory Palisades, N. Y. 1982

4. Controls on phosphorus concentration and accumulation in oceanic sediments;Filippelli;Mar. Geol.,1997

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