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Silica depletion in Lake Victoria: sedimentary signals at offshore stations

Dirk Verschuren UGent, David N Edgington, Hedy J Kling and Thomas C Johnson (1998) JOURNAL OF GREAT LAKES RESEARCH. 24(1). p.118-130
abstract
Six short sediment cores from offshore stations in Lake Victoria (East Africa) were analyzed for evidence of recent change in the lake's pelagic ecosystem. Three stations were located on a NW-SE transect between 48 m water depth, near the present upper limit of seasonal hypolimnetic oxygen depletion, and the deepest point of Lake Victoria at 68 m. Four stations formed a NE-SW transect across the east-central zone of maximum Holocene sediment accumulation below 64 m water depth. (210)Pb dating of two cores from deepwater stations established average recent sediment accummulation rates of 0.032 +/- 0.001 g/cm(2)/yr and 0.028 +/- 0.001 g/cm(2)/yr. Although the deepest part of the basin has been subject to an event of possibly widespread sediment erosion dated to the mid-1920s, core correlation based on the stratigraphy of biogenic Si above this unconformity indicates that deepwater stations have accumulated representative high-resolution archives of lake history over the past 70 years. The sedimentary record of biogenic-Si accumulation in deepwater cores reflects a sequence of events in which progressive enrichment of Lake Victoria with essential nutrients other than Si first led to increased diatom production, until the combination of excess Si demand and greater burial losses of diatom-Si resulted in depletion of the dissolved-Si reservoir and a transition to Si-limited diatom growth, Available sediment chronologies infer that increased diatom production in offshore areas started between the 1930s and early 1950s, and that the recently documented phytoplankton transition to year-round dominance by cyanobacteria started in the late 1980s. Excess diatom production over the past half century has led to significantly higher burial losses of biogenic Si only in the depositional center of the basin at water depths below 60 m.
Please use this url to cite or link to this publication:
author
organization
year
type
journalArticle (original)
publication status
published
subject
keyword
eutrophication, biogenic silica, Lake Victoria, paleolimnology, silica depletion, GREAT-LAKES, BIOGENIC SILICA, EAST-AFRICA, EUTROPHICATION, PB-210, WATER, ACCUMULATION, MICHIGAN, MALAWI, FISHES
journal title
JOURNAL OF GREAT LAKES RESEARCH
J. Gt. Lakes Res.
volume
24
issue
1
pages
118 - 130
Web of Science type
Article
Web of Science id
000072958100011
ISSN
0380-1330
language
English
UGent publication?
yes
classification
A1
copyright statement
I have transferred the copyright for this publication to the publisher
id
177425
handle
http://hdl.handle.net/1854/LU-177425
date created
2004-01-14 13:41:00
date last changed
2016-12-19 15:38:06
@article{177425,
  abstract     = {Six short sediment cores from offshore stations in Lake Victoria (East Africa) were analyzed for evidence of recent change in the lake's pelagic ecosystem. Three stations were located on a NW-SE transect between 48 m water depth, near the present upper limit of seasonal hypolimnetic oxygen depletion, and the deepest point of Lake Victoria at 68 m. Four stations formed a NE-SW transect across the east-central zone of maximum Holocene sediment accumulation below 64 m water depth. (210)Pb dating of two cores from deepwater stations established average recent sediment accummulation rates of 0.032 +/- 0.001 g/cm(2)/yr and 0.028 +/- 0.001 g/cm(2)/yr. Although the deepest part of the basin has been subject to an event of possibly widespread sediment erosion dated to the mid-1920s, core correlation based on the stratigraphy of biogenic Si above this unconformity indicates that deepwater stations have accumulated representative high-resolution archives of lake history over the past 70 years. The sedimentary record of biogenic-Si accumulation in deepwater cores reflects a sequence of events in which progressive enrichment of Lake Victoria with essential nutrients other than Si first led to increased diatom production, until the combination of excess Si demand and greater burial losses of diatom-Si resulted in depletion of the dissolved-Si reservoir and a transition to Si-limited diatom growth, Available sediment chronologies infer that increased diatom production in offshore areas started between the 1930s and early 1950s, and that the recently documented phytoplankton transition to year-round dominance by cyanobacteria started in the late 1980s. Excess diatom production over the past half century has led to significantly higher burial losses of biogenic Si only in the depositional center of the basin at water depths below 60 m.},
  author       = {Verschuren, Dirk and Edgington, David N and Kling, Hedy J and Johnson, Thomas C},
  issn         = {0380-1330},
  journal      = {JOURNAL OF GREAT LAKES RESEARCH},
  keyword      = {eutrophication,biogenic silica,Lake Victoria,paleolimnology,silica depletion,GREAT-LAKES,BIOGENIC SILICA,EAST-AFRICA,EUTROPHICATION,PB-210,WATER,ACCUMULATION,MICHIGAN,MALAWI,FISHES},
  language     = {eng},
  number       = {1},
  pages        = {118--130},
  title        = {Silica depletion in Lake Victoria: sedimentary signals at offshore stations},
  volume       = {24},
  year         = {1998},
}

Chicago
Verschuren, Dirk, David N Edgington, Hedy J Kling, and Thomas C Johnson. 1998. “Silica Depletion in Lake Victoria: Sedimentary Signals at Offshore Stations.” Journal of Great Lakes Research 24 (1): 118–130.
APA
Verschuren, D., Edgington, D. N., Kling, H. J., & Johnson, T. C. (1998). Silica depletion in Lake Victoria: sedimentary signals at offshore stations. JOURNAL OF GREAT LAKES RESEARCH, 24(1), 118–130.
Vancouver
1.
Verschuren D, Edgington DN, Kling HJ, Johnson TC. Silica depletion in Lake Victoria: sedimentary signals at offshore stations. JOURNAL OF GREAT LAKES RESEARCH. 1998;24(1):118–30.
MLA
Verschuren, Dirk, David N Edgington, Hedy J Kling, et al. “Silica Depletion in Lake Victoria: Sedimentary Signals at Offshore Stations.” JOURNAL OF GREAT LAKES RESEARCH 24.1 (1998): 118–130. Print.