A Serpentinite-Hosted Ecosystem: The Lost City Hydrothermal Field

Autor:	Deborah Glickson, A. M. Bradley, Matthew O. Schrenk, William J. Brazelton, Marvin D. Lilley, Roger E. Summons, Ben Larson, Adélie Delacour, Kate Buckman, Mitch J. Elend, John A. Baross, Alexander S. Bradley, Deborah S. Kelley, David A. Butterfield, Kevin K. Roe, Jeffrey A. Karson, Gretchen L. Früh-Green, Giora Proskurowski, Dana R. Yoerger, John M. Hayes, Stefano M. Bernasconi, Michael V. Jakuba, Sean P. Sylva, Kristin A. Ludwig, Eric J. Olson, Timothy M. Shank
Rok vydání:	2005
Předmět:	Geologic Sediments Hot Temperature Earth science Carbonates Colony Count Microbial Environment Hydrothermal circulation chemistry.chemical_compound Animals Seawater Biomass Ecosystem Phylogeny Chemosynthesis Peridotite geography Multidisciplinary geography.geographical_feature_category Bacteria Fishes Mid-ocean ridge Biodiversity Hydrogen-Ion Concentration Archaea Invertebrates Lipids Oceanic core complex Oceanography Lost City Hydrothermal Field chemistry Carbonate Methane Geology Hydrogen
Zdroj:	Science. 307:1428-1434
ISSN:	1095-9203 0036-8075
DOI:	10.1126/science.1102556
Popis:	The serpentinite-hosted Lost City hydrothermal field is a remarkable submarine ecosystem in which geological, chemical, and biological processes are intimately interlinked. Reactions between seawater and upper mantle peridotite produce methane- and hydrogen-rich fluids, with temperatures ranging from
Databáze:	OpenAIRE
Externí odkaz:	https://explore.openaire.eu/search/publication?articleId=doi_dedup___::995cd16c569b05189a5ec94070f5b555 https://doi.org/10.1126/science.1102556 Zobrazit plný text záznamu Plný text ve formátu PDF Plný text ve formátu HTML
Nepřihlášeným uživatelům se plný text nezobrazuje	K zobrazení výsledku je třeba se přihlásit.