Titlebook: Marine Pelagic Cyanobacteria: Trichodesmium and other Diazotrophs; E. J. Carpenter,D. G. Capone,J. G. Rueter Book 1992 Springer Science+Bu

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M. J. Furnasgrates the long-range contextual information of these two views. Two refined heat maps in the sagittal and coronal planes are generated by a globally-refining module, adjusting vertebra locations using the global location information in an attention manner. Experiments on a public dataset of 302 3D

Harbor

judicial

John G. Rueter,David A. Hutchins,Randall W. Smith,Nancy L. Unsworthuce user variability, challenges remain with regards to robustness, as well as generalizability to new data. To improve bone localization, from which the metrics are calculated, we first build upon recent phase-based feature extraction by applying spatial anatomical priors to eliminate false positiv

headway

Diverticulitis

Oxygen Cycling in Cyanobacteria, with Specific Reference to Oxygen Protection in , spp., a cyanobacterium. The dark respiration rate was approximately 30% of the maximum gross oxygen evolution rate. Oxygen uptake was also light dependent, increasing in proportion to light intensity from 50 to 400 μE m. s., then remaining constant up to 1700 μE m. s.. The high respiration rate resulted

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Oxygen Dynamics in , spp. Aggregates,over 500 .M O.. Irradiance at sub-saturating levels would push the oxygen balance towards net O. consumption by the aggregates whereas reduced O. consumption would result in net O. evolution by the aggregates. Net oxygen evolution by aggregates is possible throughout the diel cycle, and some diel ch

滑稽

Grazers and Associated Organisms of ,,cant contribution to “new production” of nitrogen and the flux of organic matter from surface waters. Therefore, the consumption and fate of . has important consequences for understanding the inputs and outputs of carbon and nitrogen in the open ocean.

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