964 resultados para Aurelia (1er s. av. J.-C.) -- Portraits


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Fil: Snchez García, Victoria. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

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Fil: Snchez, Victoria. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

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Most deep ocean carbon flux profiles show low and almost constant fluxes of particulate organic carbon (POC) in the deep ocean. However, the reason for the non-changing POC fluxes at depths is unknown. This study presents direct measurements of formation, degradation, and sinking velocity of diatom aggregates from laboratory studies performed at 15 °C and 4 °C during a three-week experiment. The average carbon-specific respiration rate during the experiment was 0.12 ± 0.03 at 15 °C, and decreased 3.5-fold when the temperature was lowered to 4 °C. No direct influence of temperature on aggregate sinking speed was observed. Using the remineralisation rate measured at 4 °C and an average particle sinking speed of 150 m d**-1, calculated carbon fluxes were similar to those collected in deep ocean sediment traps from a global data set, indicating that temperature plays a major role for deep ocean fluxes of POC.

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On mat: D.H. Swartz, 600 Main Street, Fort Worth, Tex.

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Cropped from 1889 team photo.

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Lodi Township (Mich.) residence. Publication information: Chicago, Ill. : Everts & Stewart, 1874.

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Mode of access: Internet.

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Text signed: Gisela M. A. Richter.