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Jess F. Adkins

Researcher at California Institute of Technology

Publications -  202
Citations -  15538

Jess F. Adkins is an academic researcher from California Institute of Technology. The author has contributed to research in topics: Glacial period & Last Glacial Maximum. The author has an hindex of 60, co-authored 186 publications receiving 12921 citations. Previous affiliations of Jess F. Adkins include Lamont–Doherty Earth Observatory & University of Southern California.

Papers
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Journal ArticleDOI

The carbonic anhydrase activity of sinking and suspended particles in the North Pacific Ocean

TL;DR: In this paper, the enzyme carbonic anhydrase (CA) is crucial to many physiological processes involving CO₂, from photosynthesis and respiration, to calcification and CaCO₃ dissolution.
Journal ArticleDOI

Brachiopod δ34SCAS microanalyses indicate a dynamic, climate-influenced Permo-Carboniferous sulfur cycle

TL;DR: A new record of Carboniferous and Early Permian brachiopod δ 34 S CAS generated from over 130 measurements of micro-sampled brachiopsod shells is presented in this article.
Book ChapterDOI

Development and Initial Biogeochemical Applications of Compound-Specific Sulfur Isotope Analysis

TL;DR: In this paper, compound-specific isotope analysis (CSIA) has been extended to the stable isotopes of sulfur (δ(34)S) through the combination of gas chromatography (GC) and multi-collector inductively coupled mass spectrometry (ICPMS).

Quantification and Isotopic Analysis of Intracellular Sulfur Metabolites in the Dissimilatory Sulfate Reduction Pathway

TL;DR: In this paper, the authors report the concentrations and isotopic ratios of sulfur metabolites in the dissimilatory sulfate reduction pathway of Desulfovibrio alaskensis and interpret this pattern to indicate that enzymatic fractionations remain large but the net fractionation between sulfate and sulfide is muted by the closed-system limitation of intracellular sulfate.
Journal ArticleDOI

The Role of the Southern Ocean in Abrupt Transitions and Hysteresis in Glacial Ocean Circulation

TL;DR: In this paper, a time-dependent coarse-resolution isopycnal model with four density classes and two basins, linked by a Southern Ocean, was used to explore overturning states and their stability to changes in external parameters.