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Open AccessJournal ArticleDOI

Is pore water oxygen content decoupled from productivity on the California Margin? Trace element results from Ocean Drilling Program Hole 1017E, San Lucia slope, California

TLDR
In this article, the influence of export production on intermediate water oxygen content can be distinguished from lateral ventilation through comparisons among proxies representing export production flux (percent Corg) and sediment-surface (I/Br) and pore water (Mo, Ag, Cd, Re, and U) oxygenation proxies.
Abstract
[1] Trace element evidence from the California Margin (Ocean Drilling Program Hole 1017E) shows significant changes in sediment redox chemistry at intermediate water depths over the last 60 kyr. The influence of export production on intermediate water oxygen content can be distinguished from lateral ventilation through comparisons among proxies representing export production flux (percent Corg) and sediment-surface (I/Br) and pore water (Mo, Ag, Cd, Re, and U) oxygenation proxies. Sulfate reduction within the uppermost sediment column occurred during late Quaternary interstadials and the Holocene, indicating reduced intermediate water ventilation. However, sulfate reduction was most intense during major interstadials when productivity was enhanced. Decoupling between export production and pore water oxygen content is demonstrated during deglaciation when the sediment pore water oxygen content increases without a corresponding reduction in export productivity. Thus both export production and intermediate water ventilation play a role in oxygen minimum zone processes on the California Margin.

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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

Deep water formation in the North Pacific and deglacial CO2 rise

TL;DR: In this paper, paired radiocarbon and boron isotope data from foraminifera from sediment core MD02-2489 at 3640m in the North East Pacific were presented.
Journal ArticleDOI

Paleoceanographic Insights on Recent Oxygen Minimum Zone Expansion: Lessons for Modern Oceanography

TL;DR: These analyses provide new evidence for the geographically and vertically extensive expansion of OMZs, and the extreme compression of upper-ocean oxygenated ecosystems during the geologically recent deglaciation.
Journal ArticleDOI

Intermediate and deep water mass distribution in the Pacific during the Last Glacial Maximum inferred from oxygen and carbon stable isotopes

TL;DR: In this article, the authors show a fundamental change in the carbon isotopic gradient between intermediate and deep waters during the last Glacial Maximum (LGM) in the eastern North Pacific indicating a deepening of nutrient and carbon rich waters.
Journal ArticleDOI

Oxygen minimum zone expansion in the eastern tropical North Pacific during deglaciation

TL;DR: Hendy et al. as discussed by the authors found that OMZ expansion in the Gulf was contemporaneous with changes in sea ice extent and zonal wind shifts around Antarctica, pointing to Subantarctic Mode Water and Antarctic Intermediate Water as likely sources of oxygen depletion.
References
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Book

Early Diagenesis: A Theoretical Approach

TL;DR: In this article, Berner developed the mathematical theory of early diagenesis, introducing a general diagenetic equation and discussing it in terms of each major diagenetics process, including diffusion, compaction, pore-water flow, burial advection, bioturbation, adsorption, radioactive decay and especially chemical and biochemical reactions.
Journal ArticleDOI

Geochemistry of Recent oxic and anoxic marine sediments: Implications for the geological record

TL;DR: In this article, the authors examined the distribution of minor and trace elements in marine sediments and provided forensic tools for determining the redox conditions of the bottom waters at the time of deposition.
Journal ArticleDOI

Rhenium and molybdenum enrichments in sediments as indicators of oxic, suboxic and sulfidic conditions of deposition

TL;DR: In this article, the authors present sedimentary Re and Mo data from box-and multi-cores spanning a range of redox conditions, from well-oxygenated sites to locations with substantial sulfide concentrations.
Journal ArticleDOI

The California current system—hypotheses and facts☆

TL;DR: In this article, the authors describe the seasonal variation of the various currents which comprise the California Current System, the California Undercurrent, the Davidson Current and the Southern California Countercurrent and investigate qualitatively the dynamical relationships among these currents.
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