Natascha Riedinger

ORCID: 0000-0001-6766-0749
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About
Contact & Profiles
Research Areas
  • Methane Hydrates and Related Phenomena
  • Hydrocarbon exploration and reservoir analysis
  • Geology and Paleoclimatology Research
  • Geological Studies and Exploration
  • Seismic Imaging and Inversion Techniques
  • Geochemistry and Elemental Analysis
  • Geological and Geophysical Studies
  • Atmospheric and Environmental Gas Dynamics
  • Paleontology and Stratigraphy of Fossils
  • Reservoir Engineering and Simulation Methods
  • Geomagnetism and Paleomagnetism Studies
  • Marine and coastal ecosystems
  • Geochemistry and Geologic Mapping
  • Geological formations and processes
  • earthquake and tectonic studies
  • Marine and environmental studies
  • Geophysics and Gravity Measurements
  • Geological and Geochemical Analysis
  • Groundwater and Isotope Geochemistry
  • Hydraulic Fracturing and Reservoir Analysis
  • Microbial Community Ecology and Physiology
  • Isotope Analysis in Ecology
  • Radioactive element chemistry and processing
  • Heavy metals in environment
  • Marine Biology and Ecology Research

Oklahoma State University
2015-2025

Expedition Technology (United States)
2024

Oklahoma State University Oklahoma City
2022-2023

Appalachian State University
2020-2021

University of California, Riverside
2011-2017

Newcastle University
2015

Max Planck Institute for Marine Microbiology
2009-2015

University of California System
2011

University of Bremen
2003-2005

Microbial life inhabits deeply buried marine sediments, but the extent of this vast ecosystem remains poorly constrained. Here we provide evidence for existence microbial communities in ~40° to 60°C sediment associated with lignite coal beds at ~1.5 2.5 km below seafloor Pacific Ocean off Japan. methanogenesis was indicated by isotopic compositions methane and carbon dioxide, biomarkers, cultivation data, gas compositions. Concentrations indigenous cells 1.5 ranged from <10 ~10(4) cm(-3)....

10.1126/science.aaa6882 article EN Science 2015-07-23

Abstract Here, we present results from sediments collected in the Argentine Basin, a non‐steady state depositional marine system characterized by abundant oxidized iron within methane‐rich layers due to sediment reworking followed rapid deposition. Our comprehensive inorganic data set shows that reduction these sulfate and sulfide‐depleted is best explained microbially mediated process—implicating anaerobic oxidation of methane coupled (Fe‐ AOM ) as most likely major mechanism. Although...

10.1111/gbi.12077 article EN Geobiology 2014-01-27

Integrated Ocean Drilling Program (IODP) Expedition 316 Sites C0006 and C0007 examined the deformation front of Nankai accretionary prism offshore Kii Peninsula, Japan. In drilling area, frontal thrust shows unusual behavior as compared to other regions Trough. results, integrated with observations from seismic reflection profiles, suggest that has been active since ∼0.78–0.436 Ma accommodated ∼13 34% estimated plate convergence during time. The remainder likely distributed among...

10.1029/2009gc002713 article EN Geochemistry Geophysics Geosystems 2009-12-01

Abstract Successful chemotherapeutic intervention for management of lung cancer requires an efficient drug delivery system. Gold nanoparticles (GNPs) can incorporate various therapeutics; however, GNPs have limitations as carriers. Nano-sized cellular vesicles like exosomes (Exo) ferry GNP-therapeutic complexes without causing any particle aggregation or immune response. In the present study, we describe development and testing a novel Exo-GNP-based therapeutic system -‘nanosomes’- therapy....

10.1038/srep38541 article EN cc-by Scientific Reports 2016-12-12

The interplay between sediment deposition patterns, organic matter type and the quantity quality of reactive mineral phases determines accumulation, speciation isotope composition pore water solid phase sulfur constituents in marine sediments. Here, we present geochemistry siliciclastic sediments from two sites along Argentine continental slope—a system characterized by dynamic reworking, which result non-steady state conditions. investigated have different depositional histories but common...

10.3389/feart.2017.00033 article EN cc-by Frontiers in Earth Science 2017-05-09

Iron speciation and trace metal proxies are commonly applied together in efforts to identify anoxic settings marked by the presence of free sulfide (euxinia) or dissolved iron (ferruginous) water column. Here, we use a literature compilation from modern localities provide new empirical evaluation coupled Fe Mo concentrations as proxy for pore accumulation at non-euxinic localities. We also present speciation, concentration, S isotope data Friends Anoxic Mud (FOAM) site Long Island Sound,...

10.2475/05.2018.04 article EN American Journal of Science 2018-05-01

The modern Baltic Sea is the world9s largest anthropogenically forced anoxic basin. Using integrated geochemical records collected during Integrated Ocean Drilling Program (IODP) Expedition 347 from deepest and one of most reducing sub-basins in Sea, Landsort Deep, we explore degree frequency natural anoxia through Holocene. A marked decrease carbon-to-sulfur ratios (C/S) cores indicate transition Ice Lake to current brackish sea, which occurred about 8.5 kyrs B.P. Following this,...

10.2475/08.2016.01 article EN American Journal of Science 2016-10-01

The deep oceans are environments of complex carbon dynamics that have the potential to significantly impact global cycle. However, role hadal zones, particularly trenches (water depth > 6 km), in oceanic dissolved organic (DOC) cycle is not thoroughly investigated. Here we report distinct DOC signatures Japan Trench bottom water. We find up 34% ± 7% trench removed during northeastward transport along axis. This removal increases overall recalcitrance Pacific pool, and potentially enhanced by...

10.1038/s41467-025-55883-1 article EN cc-by-nc-nd Nature Communications 2025-01-16

The 2011 Tohoku-Oki earthquake highlighted substantial deficiencies in our understanding and an underestimation of the hazard potential megathrust earthquakes their cascading effects, including tsunamis. Offshore deep-sea paleoseismology evolved from need to better understand mechanisms depositional processes within subduction zones. examination sedimentary records has demonstrated effectiveness reconstructing complex historical seismic events resulting multi-pulse sequences. However,...

10.5194/egusphere-egu25-18629 preprint EN 2025-03-15

Abstract The nitrogen isotopic composition of diatom frustule‐bound organic matter (δ 15 N DB ) is often used to study changes in high latitude biological pump efficiency across glacial‐interglacial cycles, but the proxy may be biased by species‐specific effects. genus Chaetoceros particular interest because its abundance throughout ocean basins, shifting biogeography during glacial periods, and ability many species form heavily silicified resting spores. Here we investigate how spores (CRS)...

10.1029/2024pa005041 article EN cc-by-nc-nd Paleoceanography and Paleoclimatology 2025-04-01

Research Article| September 01, 2010 Oxidative sulfur cycling in the deep biosphere of Nankai Trough, Japan N. Riedinger; Riedinger * 1Max Planck Institute for Marine Microbiology, Celsiusstraße 1, 28359 Bremen, Germany *Current address: Department Earth Sciences, Biogeochemistry, University California–Riverside, 900 Avenue, Riverside, California 92521-0432, USA; E-mail: natascha.riedinger@ucr.edu. Search other works by this author on: GSW Google Scholar B. Brunner; Brunner M.J. Formolo;...

10.1130/g31085.1 article EN Geology 2010-08-19
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