## Abstract The transition from the Last Glacial Maximum to the Holocene was an internal of climate variability that was characterised by large spatial and temporal variations. Here we show that deglaciation warming in the northern Indian Ocean was initiated ca. 19โka, which is contemporary with de
On the role of bacterioplankton in the tropical ocean
โ Scribed by K. Banse
- Publisher
- Springer-Verlag
- Year
- 1974
- Tongue
- English
- Weight
- 520 KB
- Volume
- 24
- Category
- Article
- ISSN
- 0025-3162
No coin nor oath required. For personal study only.
โฆ Synopsis
The high rates of produetien by plank~nio bacteria reported by Sorokin for the warm surface layer of the oceans cannot be reconciled with the geographic distaqbution of dissolved organic carbon. Those rates, as well as Sorokin's figure8 of bactewial production and, hence, consumption of oxygen in the deep sea are too high by an order of magnitude. It is left undecided whether the prinoipM ainl~ for the dissolved organic matter roaching the deep sea is in the warm surface layer of the oceans, as suggested by Sornk~n~ or the deep sea itself.
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