The objective of this research is to determine the correlation of lacustrine micro-fossils in Lake Tanganyika to changes in climate and lake levels during the Late Pleistocene and Early Holocene.
Lake Tanganyika is the second deepest and one of the oldest lakes in the world. The horst and graben geometry...
Full Text:
planktonic diatom was
Stephanodiscus astraea, which thrived in low Si:P supply ratio, stratified lake
The objective of this research is to determine the correlation of lacustrine micro-fossils in Lake Tanganyika to changes in climate and lake levels during the Late Pleistocene and Early Holocene.
Lake Tanganyika is the second deepest and one of the oldest lakes in the world. The horst and graben geometry...
Full Text:
level variations by
recording changes in microfossil assemblages. Changes in diatom taxa occur in
Diatoms are a ubiquitous group of plankton responsible for 20-40% of oceanic
primary production, and a higher fraction of organic matter export to the ocean
interior. Diatoms actively transport dissolved inorganic silicon into their cells, and
through the process of silicification (i.e. biogenic silica production) they build tough
and intricate...
Diatoms are a ubiquitous group of plankton responsible for 20-40% of oceanic
primary production, and a higher fraction of organic matter export to the ocean
interior. Diatoms actively transport dissolved inorganic silicon into their cells, and
through the process of silicification (i.e. biogenic silica production) they build tough
and intricate...
Diatoms are a ubiquitous group of plankton responsible for 20-40% of oceanic
primary production, and a higher fraction of organic matter export to the ocean
interior. Diatoms actively transport dissolved inorganic silicon into their cells, and
through the process of silicification (i.e. biogenic silica production) they build tough
and intricate...
Full Text:
matter to the ocean interior) by diatoms
in this region was 4-10 times higher than the diatom
