Richard G. Keil

ORCID: 0000-0001-7483-1606
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About
Contact & Profiles
Research Areas
  • Marine and coastal ecosystems
  • Microbial Community Ecology and Physiology
  • Marine Biology and Ecology Research
  • Isotope Analysis in Ecology
  • Geology and Paleoclimatology Research
  • Ocean Acidification Effects and Responses
  • Methane Hydrates and Related Phenomena
  • Atmospheric and Environmental Gas Dynamics
  • Wastewater Treatment and Nitrogen Removal
  • Aquatic Ecosystems and Phytoplankton Dynamics
  • Coral and Marine Ecosystems Studies
  • Protist diversity and phylogeny
  • Metabolomics and Mass Spectrometry Studies
  • Geochemistry and Elemental Analysis
  • Diatoms and Algae Research
  • Paleontology and Stratigraphy of Fossils
  • Hydrocarbon exploration and reservoir analysis
  • Soil and Water Nutrient Dynamics
  • Fish Ecology and Management Studies
  • Mass Spectrometry Techniques and Applications
  • Fish biology, ecology, and behavior
  • Groundwater and Isotope Geochemistry
  • Genomics and Phylogenetic Studies
  • Advanced Proteomics Techniques and Applications
  • Geological formations and processes

University of Washington
2015-2025

Seattle University
1994-2021

Irvine University
2010

University of Delaware
1989-2005

College of Marin
1989-2005

Maine Medical Center
1998

University of Maine
1998

University of Georgia
1998

University of Virginia
1998

Paul Scherrer Institute
1994

The purpose of this review is to highlight progress in unraveling carbon cycling dynamics across the continuum landscapes, inland waters, coastal oceans, and atmosphere. Earth systems are intimately interconnected, yet most biogeochemical studies focus on specific components isolation. movement water drives cycle, and, as such, waters provide a critical intersection between terrestrial marine biospheres. Inland, estuarine, well studied regions near centers human population Northern...

10.3389/fmars.2017.00007 article EN cc-by Frontiers in Marine Science 2017-01-31

Biologically available nitrogen limits photosynthesis in much of the world ocean. Organic matter (OM) stoichiometry had been thought to control balance between two major removal pathways-denitrification and anammox-but expected proportion 30% anammox derived from mean oceanic OM is rarely observed environment. With incubations designed directly test effects stoichiometry, however, we showed that ratio denitrification depends on supply, as predicted. Furthermore, rates loss increase with...

10.1126/science.1248364 article EN Science 2014-04-11

Controlling Factors on Source Rock Development-A Review Of Productivity, Preservation, and Sedimentation Rate

10.2475/ajs.299.7-9.529 article EN American Journal of Science 1999-11-01

The Branched and Isoprenoid Tetraether (BIT) index (a ratio of marine terrestrial glycerol dialkyl tetraether [GDGT] membrane lipids) was recently introduced as a proxy for the fraction fluvially derived organic carbon (OC) buried in sediments. We investigate source distribution OC sediments large spatial data set that encompasses Washington‐Vancouver Island Margin, Vancouver fjords, Puget Sound with goal comparing BIT to other traditional measures (δ 13 C [δ org ] lignin phenols). δ values...

10.4319/lo.2008.53.3.1054 article EN Limnology and Oceanography 2008-05-01

Abstract Here we present direct measurements of the biological breakdown 13 C‐labeled substrates to CO 2 at seven locations along lower Amazon River, from Óbidos mouth. Dark incubation experiments were performed high and low water periods using vanillin, a lignin phenol derived vascular plants, period four different plant litter leachates. Leachates oak wood degraded most slowly with vanillin monomers, macrophyte leaves, stems, whole grass leachates being converted 1.2, 1.3, 1.7, 2.3 times...

10.1002/2016jg003342 article EN Journal of Geophysical Research Biogeosciences 2016-05-24

Where they can't breathe Climate warming is causing the expansion of marine oxygen-deficient zones, which are regions in dissolved oxygen concentrations so low that many animals cannot survive. This phenomenon also might affect global cycles carbon, sulfur, nitrogen, and trace metals oceans. Raven et al. show how ocean anoxia affects microbial sulfur processing sinking particles. They observed cryptic sulfate reduction, forms organic resistant to acid hydrolysis, a process could enhance...

10.1126/science.abc6035 article EN Science 2021-01-07

Abstract. Human activities are drastically altering water and material flows in river systems across Asia. These anthropogenic perturbations have rarely been linked to the carbon (C) fluxes of Asian rivers that may account for up 40–50 % global fluxes. This review aims provide a conceptual framework assessing human impacts on C fluxes, along with an update alterations riverine Drawing case studies conducted three selected (the Ganges, Mekong, Yellow River) other major rivers, focuses...

10.5194/bg-15-3049-2018 article EN cc-by Biogeosciences 2018-05-17

The chemical form and bacterial utilization of dissolved combined amino acids (DCAA) were studied in the Delaware estuary coastal waters. Concentrations DCAA estimated after vapor-phase hydrolysis 1.1–2.5-fold higher than those liquid-phase hydrolysis; concentrations ranged from 40 to 1,490 µg liter−1. Protein by bicinchoninic acid method within 13% measured hydrolysis, suggesting that recovers primarily protein. Vapor-phase apparently protein an unknown component because only 30–80% DCAA....

10.4319/lo.1993.38.6.1256 article EN Limnology and Oceanography 1993-09-01

Total nitrogen (TN) loadings in riverine sediments and their coastal depocenters were compared for 11 river systems worldwide to assess the potential impact of particulates on budgets. Strong relationships between sediment specific surface area TN allow these impacts be estimated without intense sampling normally required achieve such About half showed higher than those from depocenter. In spite uncertainties, comparisons indicate that large, turbid rivers, as Amazon, Huanghe, Mississippi,...

10.1029/98gb02267 article EN Global Biogeochemical Cycles 1998-12-01
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