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Book ChapterDOI

Controls of Trace Metals in Seawater

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TLDR
In this article, a general overview of the major controls of trace metals in seawater is presented, developed from the extensive research on trace metals over the last few decades, with a focus on trace metal biogeochemistry.
Abstract
This chapter presents a general overview of the major controls of trace metals in seawater, developed from the extensive research on trace metals over the last few decades. The reader should be given a first-order understanding and insight into trace metal biogeochemistry in the oceans, rather than presented with a comprehensive review of the distribution of each trace metal. Each of the trace metals discussed will undoubtedly prove to have unique characteristics and subtle differences from this version, yet the comparison with these characteristics will serve as a good springboard to a more complete understanding.

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Journal ArticleDOI

Mercury biogeochemical cycling in the ocean and policy implications.

TL;DR: This analysis suggests that while atmospheric deposition is the main source of inorganic Hg to open ocean systems, most of the CH₃Hg accumulating in ocean fish is derived from in situ production within the upper waters (<1000 m), and that the deeper waters of the oceans are responding slowly to changes in atmospheric Hg inputs.
Journal ArticleDOI

The Trace Metal Composition of Marine Phytoplankton

TL;DR: There are notable differences between taxa and regions that inform the understanding of ocean metal biogeochemistry, and differences in the quotas estimated by the various techniques also provide information on metal behavior.
Book ChapterDOI

Chapter Fourteen Elemental Proxies for Palaeoclimatic and Palaeoceanographic Variability in Marine Sediments: Interpretation and Application

TL;DR: In this article, the elemental proxies for palaeoclimatic and palaeoceanographic variability in marine sediments are discussed, and the application of sedimentary geochemistry to the reconstruction of climatic and oceanographic changes over the Cenozoic is discussed.
Journal ArticleDOI

Feedback Interactions between Trace Metal Nutrients and Phytoplankton in the Ocean.

TL;DR: Iron is thought to play a key role in regulating biological cycles of carbon and nitrogen in the ocean, including the biological transfer of carbon to the deep sea, the so-called biological CO2 pump, which helps regulate atmospheric CO2 and CO2-linked global warming.
Journal ArticleDOI

The Isotope Geochemistry of Zinc and Copper

TL;DR: Chaboy et al. as mentioned in this paper showed that the symmetry of the hexaaqua complex of Cu(H2O)62+ has a Jahn-Teller distortion effect (Sherman 2001; Bersuker 2006), whereby the two Cu-O distances of the vertical axial bond (Cu-Oax) are longer than four Cu O distances in the equatorial plane (Cu Oax).
References
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Journal ArticleDOI

Global Iron Connections Between Desert Dust, Ocean Biogeochemistry, and Climate

TL;DR: The iron cycle, in which iron-containing soil dust is transported from land through the atmosphere to the oceans, affecting ocean biogeochemistry and hence having feedback effects on climate and dust production, is reviewed.
Book

Tracers in the Sea

Journal Article

Couplings between changes in the climate system and biogeochemistry

TL;DR: Denman et al. as discussed by the authors presented the Couplings between changes in the climate system and biogeochemistry Coordinating Lead Authors: Kenneth L. Denman (Canada), Guy Brasseur (USA, Germany), Amnat Chidthaisong (Thailand), Philippe Ciais (France), Peter M. Cox (UK), Robert E. Austin (USA), D.B. Wofsy (USA) and Xiaoye Zhang (China).
Journal ArticleDOI

Tracers in the Sea

Michael L. Bender
- 01 Aug 1984 - 
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