Titlebook: Deep-Sea Food Chains and the Global Carbon Cycle; Gilbert T. Rowe,Vita Pariente Book 1992 Springer Science+Business Media Dordrecht 1992 O

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VICT

The Spatial Distribution of Sea Floor Oxygen Consumption in The Atlantic and Pacific Oceans,benthic respiration must be supported predominantly by the rain of organic matter from surface waters, the pattern of oxygen consumption in the surface sediments reveals the distribution of particle fluxes in the deep ocean. Benthic oxygen consumption in the Atlantic and Pacific basins appears to ac

CLASP

Using Monod Kinetics in Geochemical Models of Organic Carbon Mineralization in Deep-Sea Surficial Ss model is based on mass balance and includes transport and reaction equations depicting microbially mediated transformations. This model represents, in its present state, the first steps of organic matter decomposition by the benthic microfauna using Monod rate laws..The results of simulations are

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1389-2185 ts, etc., leading to predictions of a gradual global warmingwhich will perturb the global biosphere. An important process whichcounters this trend toward potential climate change is the removal ofcarbon dioxide from the surface ocean by photosynthesis. This processpackages carbon in phytoplankton wh

Bone-Scan

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https://doi.org/10.1007/978-1-4757-1761-7 a factor of ten in 20 days. The same strong increase in ATP content was also described from sediments of the same area after the deposition of faecal pellets. Thus, the rapid changes in adenosine nucleotide levels and the ATP : AMP ratio are good indicators of deep-sea benthic metabolism.

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Development of Science Teachers‘ TPACKch individuals of a given species are continuously added to or removed from the community, is used to investigate mathematically the consequences of our inability to choose which configuration best describes the interactions among the species. The long-term outcome of press perturbations is quite sensitive to the details of model structure.

GNAT

https://doi.org/10.1007/978-94-011-9019-0mulated deep-sea conditions at rates of 0.6% to 2.3% d. during the initial rapid degradation phase of approximately 400 hrs. These rates are only slightly lower than those found in shallow water sediments. Under in situ pressure, more of the organic matter was consumed than at 1 atm.

FAWN

https://doi.org/10.1007/978-3-319-01324-4e visible on the photographs. Compared with other regions of similar water depth. the density and biomass of the megafauna at 47°N and 59°N appear to be very high. The importance of the megafauna at 47°N is demonstrated by a high megafauna/macrofauna biomass ratio of about 2.