Laboratory And Field Based Investigations Of Subsurface Geochemical Processes In Seafloor Hydrothermal Systems
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Author | : Jun-ichiro Ishibashi |
Publisher | : Springer |
Total Pages | : 651 |
Release | : 2015-01-10 |
Genre | : Science |
ISBN | : 4431548653 |
This book is the comprehensive volume of the TAIGA (“a great river ” in Japanese) project. Supported by the Japanese government, the project examined the hypothesis that the subseafloor fluid advection system (subseafloor TAIGA) can be categorized into four types, TAIGAs of sulfur, hydrogen, carbon (methane), and iron, according to the most dominant reducing substance, and the chemolithoautotrophic bacteria/archaea that are inextricably associated with respective types of TAIGAs which are strongly affected by their geological background such as surrounding host rocks and tectonic settings. Sub-seafloor ecosystems are sustained by hydrothermal circulation or TAIGA that carry chemical energy to the chemosynthetic microbes living in an extreme environment. The results of the project have been summarized comprehensively in 50 chapters, and this book provides an overall introduction and relevant topics on the mid-ocean ridge system of the Indian Ocean and on the arc-backarc systems of the Southern Mariana Trough and Okinawa Trough.
Author | : Andreas Teske |
Publisher | : Frontiers Media SA |
Total Pages | : 305 |
Release | : 2015-07-01 |
Genre | : Microbiology |
ISBN | : 2889195368 |
Deep subsurface microbiology is a highly active and rapidly advancing research field at the interface of microbiology and the geosciences; it focuses on the detection, identification, quantification, cultivation and activity measurements of bacteria, archaea and eukaryotes that permeate the subsurface biosphere of deep marine sediments and the basaltic ocean and continental crust. The deep subsurface biosphere abounds with uncultured, only recently discovered and – at best - incompletely understood microbial populations. In spatial extent and volume, Earth's subsurface biosphere is only rivaled by the deep sea water column. So far, no deep subsurface sediment has been found that is entirely devoid of microbial life; microbial cells and DNA remain detectable at sediment depths of more than 1 km; microbial life permeates deeply buried hydrocarbon reservoirs, and is also found several kilometers down in continental crust aquifers. Severe energy limitation, either as electron acceptor or donor shortage, and scarcity of microbially degradable organic carbon sources are among the evolutionary pressures that have shaped the genomic and physiological repertoire of the deep subsurface biosphere. Its biogeochemical role as long-term organic carbon repository, inorganic electron and energy source, and subduction recycling engine continues to be explored by current research at the interface of microbiology, geochemistry and biosphere/geosphere evolution. This Research Topic addresses some of the central research questions about deep subsurface microbiology and biogeochemistry: phylogenetic and physiological microbial diversity in the deep subsurface; microbial activity and survival strategies in severely energy-limited subsurface habitats; microbial activity as reflected in process rates and gene expression patterns; biogeographic isolation and connectivity in deep subsurface microbial communities; the ecological standing of subsurface biospheres in comparison to the surface biosphere – an independently flourishing biosphere, or mere survivors that tolerate burial (along with organic carbon compounds), or a combination of both? Advancing these questions on Earth’s deep subsurface biosphere redefines the habitat range, environmental tolerance, activity and diversity of microbial life.
Author | : |
Publisher | : |
Total Pages | : 1200 |
Release | : 1973 |
Genre | : Marine biology |
ISBN | : |
Author | : |
Publisher | : |
Total Pages | : 710 |
Release | : 1990 |
Genre | : Water |
ISBN | : |
Author | : Anke Marianne Herrmann |
Publisher | : Frontiers Media SA |
Total Pages | : 190 |
Release | : 2020-01-10 |
Genre | : |
ISBN | : 288963308X |
Author | : United States. National Oceanic and Atmospheric Administration |
Publisher | : |
Total Pages | : 1200 |
Release | : 1973 |
Genre | : Marine biology |
ISBN | : |
Author | : David M. Karl |
Publisher | : Springer |
Total Pages | : 328 |
Release | : 1995-07-14 |
Genre | : Science |
ISBN | : |
The Microbiology of Deep-Sea Hydrothermal Vents is the first comprehensive treatment of the microbiology of these unusual deep-sea ecosystems. It includes information on microbial biodiversity, ecology, physiology, and the origin of life. It is the first volume available on the subject. All chapters are written by leaders in their respective fields who have made substantial contributions to the current understanding of these novel deep-sea habitats. Much of the book's material is entirely new and forward looking. Individual chapters examine the geologic setting and chemistry of deep-sea hydrothermal vents, growth at high temperatures, microbe-metal interactions and mineral deposition, stable isotopes, and more. This reference presents a unique interdisciplinary approach to the study of hydrothermal vents. Because of its thorough coverage of the subject, the book will continue to be a valuable resource for researchers in this field for the next decade.
Author | : Susan Humphris |
Publisher | : |
Total Pages | : 488 |
Release | : 1995 |
Genre | : Science |
ISBN | : |
Author | : Andreas Teske |
Publisher | : Frontiers Media SA |
Total Pages | : 286 |
Release | : 2015-11-24 |
Genre | : Microbiology |
ISBN | : 2889196828 |
The papers in the "Hydrothermal Vent" e-book cover a range of microbiological research in deep and shallow hydrothermal environments, from high temperature “black smokers,” to diffuse flow habitats and episodically discharging subsurface fluids, to the hydrothermal plumes. Together they provide a snapshot of current research interests in a field that has evolved rapidly since the discovery of hydrothermal vents in 1977. Hydrothermally influenced microbial habitats and communities represent a wide spectrum of geological setting, chemical in-situ regimes, and biotic communities; the classical examples of basalt-hosted black smoker chimneys at active mid-ocean spreading centers have been augmented by hydrothermally heated and chemically altered sediments, microbiota fueled by serpentinization reactions, and low-temperature vents with unusual menus of electron donors. Environmental gradients and niches provide habitats for unusual or unprecedented microorganisms and microbial ecosystems. The discovery of novel extremophiles underscores untapped microbial diversity in hydrothermal vent microbial communities. Different stages of hydrothermal activity, from early onset to peak activity, gradual decline, and persistence of cold and fossil vent sites, correspond to different colonization waves by microorganisms as well as megafauna. Perhaps no other field in microbiology is so intertwined with the geological and geochemical evolution of the oceans, and promises so many biochemical and physiological discoveries still to be made within the unexhausted richness of extreme microbial life.
Author | : Robert P. Lowell |
Publisher | : John Wiley & Sons |
Total Pages | : 304 |
Release | : 2013-04-30 |
Genre | : Science |
ISBN | : 1118671899 |
Magma to Microbe Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 178. Hydrothermal systems at oceanic spreading centers reflect the complex interactions among transport, cooling and crystallization of magma, fluid circulation in the crust, tectonic processes, water-rock interaction, and the utilization of hydrothermal fluids as a metabolic energy source by microbial and macro-biological ecosystems. The development of mathematical and numerical models that address these complex linkages is a fundamental part the RIDGE 2000 program that attempts to quantify and model the transfer of heat and chemicals from “mantle to microbes” at oceanic ridges. This volume presents the first “state of the art” picture of model development in this context. The most outstanding feature of this volume is its emphasis on mathematical and numerical modeling of a broad array of hydrothermal processes associated with oceanic spreading centers. By examining the state of model development in one volume, both cross-fertilization of ideas and integration across the disparate disciplines that study seafloor hydrothermal systems is facilitated. Students and scientists with an interest in oceanic spreading centers in general and more specifically in ridge hydrothermal processes will find this volume to be an up-to-date and indispensable resource.