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James E. Bauer

Researcher at Ohio State University

Publications -  105
Citations -  10906

James E. Bauer is an academic researcher from Ohio State University. The author has contributed to research in topics: Dissolved organic carbon & Organic matter. The author has an hindex of 50, co-authored 105 publications receiving 10048 citations. Previous affiliations of James E. Bauer include Florida State University & Chesapeake Biological Laboratory.

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The changing carbon cycle of the coastal ocean

TL;DR: The sources, exchanges and fates of carbon in the coastal ocean and how anthropogenic activities have altered the carbon cycle are discussed.
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Southern Ocean Iron Enrichment Experiment: Carbon Cycling in High- and Low-Si Waters

TL;DR: Two mesoscale experiments, designed to investigate the effects of iron enrichment in regions with high and low concentrations of silicic acid, were performed in the Southern Ocean, demonstrating iron's pivotal role in controlling carbon uptake and regulating atmospheric partial pressure of carbon dioxide.
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Riverine export of aged terrestrial organic matter to the North Atlantic Ocean

TL;DR: It is found that much of the young dissolved organic carbon can be selectively degraded over the residence times of river and coastal waters, leaving an even older and more refractory component for oceanic export.
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Cycling of dissolved and particulate organic matter in the open ocean

TL;DR: In this paper, Druffel et al. defined three overlapping pools of dissolved organic carbon (DOC): (1) DOC that is oxidizable by UV radiation (DOCuv), (2) extra DOC measured by Co/CoO flow-through high-temperature catalytic oxidation (DOCFt-htc), which also has low Δ14C values like DOCuv, and (3) a potential residual DOC fraction that is the difference between DOC measurement by discrete-injection high-totime catalytic oxidization (DOChtc) and DOCF
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Use of 14C and 13C natural abundances for evaluating riverine, estuarine, and coastal DOC and POC sources and cycling: a review and synthesis

TL;DR: In this article, the authors summarized the available data on 14C and 13C measurements in dissolved and particulate organic carbon (DOC and POC, respectively) in these systems, and concluded that through the use of paired 14C-13C measurements, a more robust interpretation of sources, sinks, and residence times of organic matter may be attained than by using either isotope separately.