Evidence of intensified biogenic silica recycling in the Black Sea after 1970

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Evidence of intensified biogenic silica recycling in the Black Sea after 1970. / Mousing, Erik Askov; Adjou, Mohamed; Ellegaard, Marianne.

In: Estuarine, Coastal and Shelf Science, Vol. 164, 2015, p. 335-339.

Research output: Contribution to journal › Letter › Research › peer-review

Harvard

Mousing, EA, Adjou, M & Ellegaard, M 2015, 'Evidence of intensified biogenic silica recycling in the Black Sea after 1970', Estuarine, Coastal and Shelf Science, vol. 164, pp. 335-339. https://doi.org/10.1016/j.ecss.2015.07.031

APA

Mousing, E. A., Adjou, M., & Ellegaard, M. (2015). Evidence of intensified biogenic silica recycling in the Black Sea after 1970. Estuarine, Coastal and Shelf Science, 164, 335-339. https://doi.org/10.1016/j.ecss.2015.07.031

Vancouver

Mousing EA, Adjou M, Ellegaard M. Evidence of intensified biogenic silica recycling in the Black Sea after 1970. Estuarine, Coastal and Shelf Science. 2015;164:335-339. https://doi.org/10.1016/j.ecss.2015.07.031

Author

Mousing, Erik Askov ; Adjou, Mohamed ; Ellegaard, Marianne. / Evidence of intensified biogenic silica recycling in the Black Sea after 1970. In: Estuarine, Coastal and Shelf Science. 2015 ; Vol. 164. pp. 335-339.

Bibtex

@article{eb467c42d6d74125ae87bba38da6c4e0,
title = "Evidence of intensified biogenic silica recycling in the Black Sea after 1970",
abstract = "The Black Sea has been subject to increased levels of nitrogen and phosphorus loading and a decrease in silicate input after around 1970. Changes in phytoplankton community composition from diatoms to non-diatom groups have been attributed to the decrease in silicate. However, a discrepancy between the decreasing silicate input and the increasing silicate pool in the deep sea reported elsewhere implies that another silicate source exists which challenges the current paradigm of widespread silicate limitation. In this study, we investigate changes in the dissolution state of siliceous protists over the last 140 years and show that siliceous protists became significantly more dissolved after the late 1960s indicating a reduction of the silicate pool preserved in the deep sea sediment. We hypothesize that the decline in the dissolution state is caused by increased recycling of biogenic silica in the water column due to an increased annual production driven by nitrogen enrichment.",
keywords = "Black sea, Dissolution, Eutrophication, Protists, Sedimentation, Silica",
author = "Mousing, {Erik Askov} and Mohamed Adjou and Marianne Ellegaard",
year = "2015",
doi = "10.1016/j.ecss.2015.07.031",
language = "English",
volume = "164",
pages = "335--339",
journal = "Estuarine, Coastal and Shelf Science",
issn = "0272-7714",
publisher = "Academic Press",

}

RIS

TY - JOUR

T1 - Evidence of intensified biogenic silica recycling in the Black Sea after 1970

AU - Mousing, Erik Askov

AU - Adjou, Mohamed

AU - Ellegaard, Marianne

PY - 2015

Y1 - 2015

N2 - The Black Sea has been subject to increased levels of nitrogen and phosphorus loading and a decrease in silicate input after around 1970. Changes in phytoplankton community composition from diatoms to non-diatom groups have been attributed to the decrease in silicate. However, a discrepancy between the decreasing silicate input and the increasing silicate pool in the deep sea reported elsewhere implies that another silicate source exists which challenges the current paradigm of widespread silicate limitation. In this study, we investigate changes in the dissolution state of siliceous protists over the last 140 years and show that siliceous protists became significantly more dissolved after the late 1960s indicating a reduction of the silicate pool preserved in the deep sea sediment. We hypothesize that the decline in the dissolution state is caused by increased recycling of biogenic silica in the water column due to an increased annual production driven by nitrogen enrichment.

AB - The Black Sea has been subject to increased levels of nitrogen and phosphorus loading and a decrease in silicate input after around 1970. Changes in phytoplankton community composition from diatoms to non-diatom groups have been attributed to the decrease in silicate. However, a discrepancy between the decreasing silicate input and the increasing silicate pool in the deep sea reported elsewhere implies that another silicate source exists which challenges the current paradigm of widespread silicate limitation. In this study, we investigate changes in the dissolution state of siliceous protists over the last 140 years and show that siliceous protists became significantly more dissolved after the late 1960s indicating a reduction of the silicate pool preserved in the deep sea sediment. We hypothesize that the decline in the dissolution state is caused by increased recycling of biogenic silica in the water column due to an increased annual production driven by nitrogen enrichment.

KW - Black sea

KW - Dissolution

KW - Eutrophication

KW - Protists

KW - Sedimentation

KW - Silica

U2 - 10.1016/j.ecss.2015.07.031

DO - 10.1016/j.ecss.2015.07.031

M3 - Letter

AN - SCOPUS:84939634343

VL - 164

SP - 335

EP - 339

JO - Estuarine, Coastal and Shelf Science

JF - Estuarine, Coastal and Shelf Science

SN - 0272-7714

ER -

ID: 154441509