N. R. Meyer
University of Wisconsin–Milwaukee
6 Papers
1 Citations
N. R. Meyer is an academic researcher from University of Wisconsin–Milwaukee. The author has contributed to research in topics: Convection & Structural basin. The author has an hindex of 1, co-authored 1 publications.
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Papers
Heat flow and thermal regime in the Guaymas Basin, Gulf of California: Estimates of conductive and advective heat transport
Robert N. Harris,Juan Contreras,Manet S. Peña‐Salinas,Ronald M. Spelz,Andreas P Teske,Daniel Lizarralde,T. W. Höfig,Ivano W. Aiello,Janine L. Ash,D.P. Bojanova,M.D. Buatier,Virginia P. Edgcomb,Christophe Galerne,S. Gontharet,Verena B Heuer,Shijun Jiang,Myriam Kars,Ji-Hoon Kim,Louise M.T. Koornneef,Kathleen M. Marsaglia,N. R. Meyer,Yuki Morono,Raquel Negrete-Aranda,Florian Neumann,L. Pastor,M.E. Peña-Salinas,L. Pérez Cruz,Lihua Ran,Armelle Riboulleau,J. Sarao,Florian Schubert,S. K. Singh,Joann M. Stock,Laurent Toffin,W. Xie,Toshiro Yamanaka,Guang-Chao Zhuang +36 more
TL;DR: In this article , the authors studied the thermal regime of the Guaymas Basin and heat transfer between off-axis sills intruding the organic-rich sediments of the basin, and the basin floor.
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Inactive hydrothermal vent microbial communities are important contributors to deep ocean primary productivity.
Amanda M. Achberger,Rose Jones,John Jamieson,Charles P. Holmes,Florence Schubotz,N. R. Meyer,Anne E. Dekas,Sarah Moriarty,Eoghan P. Reeves,Alex Manthey,Jonas Brünjes,Daniel J Fornari,Margaret K. Tivey,Brandy M. Toner,Jason B. Sylvan +14 more
TL;DR: Inactive hydrothermal vent deposits support primary productivity in the deep ocean, with microbial communities fixing inorganic carbon at rates comparable to active vents, contributing significantly to new organic carbon production.
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Rates and physicochemical drivers of microbial anabolic activity in deep-sea sediments and implications for deep time.
TL;DR: In this article , the authors conducted nearly 300 stable isotope tracer experiments in sediments from the Pacific and Atlantic Oceans (100-4500 m water depth) to determine the rates, spatial distribution, and physicochemical controls on microbial total anabolic activity, nitrogen fixation, and inorganic/organic carbon uptake.
1
Single-cell analysis reveals an active and heterotrophic microbiome in the Guaymas Basin deep subsurface with significant inorganic carbon fixation by heterotrophs.
N. R. Meyer,Yuki Morono,Anne E. Dekas +2 more
TL;DR: The Guaymas Basin deep subsurface microbiome is active and heterotrophic, with significant inorganic carbon fixation by heterotrophs.
Unified parameterization of the planetary boundary layer and shallow convection with a higher-order turbulence closure in the Community Atmosphere Model: single-column experiments
Peter A. Bogenschutz,Andrew Gettelman,Hugh Morrison,Vincent E. Larson,D. P. Schanen,N. R. Meyer,C. Craig +6 more
TL;DR: In this article, the authors describe the coupling of the Community Atmosphere Model (CAM) version 5 with a unified multi-variate probability density function (PDF) parameterization, Cloud Layers Unified by Binormals (CLUBB), which replaces the planetary boundary layer, shallow convection, and cloud macrophysics schemes in CAM5 with a higher-order turbulence closure based on an assumed PDF.