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Hydrological Alterations and Marine Biogeochemistry: A Silicate Issue?

  • Venugopalan Ittekkot
  • Christoph Humborg
  • Petra Schäfer

Abstract

Freshwater and sediment inputs from rivers play a major role in sustaining estuarine and coastal ecosystems. Nutrients from rivers promote biological productivity in estuaries and coastal waters, and the sediments supplied by the rivers stabilize deltas and coastal zones and help to maintain ecosystems along the periphery of landmasses. In the last few decades, human activities have caused enormous changes both in the nature and quantity of these inputs. Fluxes to the oceans of mineral nutrients, such as phosphate and nitrate, have increased worldwide by more than a factor of two (Meybeck 1998). This increase has led to accelerated algal growth, known as eutrophi cation, and consequently to deterioration in water quality because of oxygen depletion. Toxic algal blooms occurring in coastal waters, which have devastating effects on fisheries and on biodiversity in general, are also attributable to eutrophication. Oxygen-deficient conditions, in turn, pro mote the production of greenhouse gases such as nitrous oxide and methane and their emission from coastal waters to the atmosphere.

Cite this activity

Ittekkot V., Humborg C. and Schäfer P. (2000) Hydrological Alterations and Marine Biogeochemistry: A Silicate Issue? BioScience 50(9): 776. 10.1641/0006-3568(2000)050[0776:HAAMBA]2.0.CO;2

Details

Date 01.09.2000
Journal BioScience
Issue 9
Volume 50
Pages 776
Open Access Closed Access
Open Access Status Closed Access
Eprints_link https://cris.leibniz-zmt.de/id/eprint/5940
Peer-Reviewed

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