4.3 Article

Benthic foraminifera from the Southeastern Mediterranean shelf: Dead assemblages and living-dead comparisons recording consequences of Nile River damming

期刊

MARINE MICROPALEONTOLOGY
卷 164, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.marmicro.2021.101977

关键词

Southeastern Levantine shelf; Eastern Mediterranean; Nile River damming; Dead and living benthic foraminifera; Taphonomy; Ecological indicators

资金

  1. Ministry of Energy, Isreal [014-06-211]
  2. Israeli Ministry of Environmental Protection
  3. Israeli Ministry of Energy

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This study explores the impact of the Nile River damming on the recent benthic ecology in the southeastern Levantine Basin of the Mediterranean Sea. The differences between dead benthic foraminiferal assemblages and living ones suggest ongoing human activity as a possible cause.
This study explores the role of the Nile River damming in shaping the recent benthic ecology in the southeastern Levantine (SL) Basin, the saltiest, hottest and the most oligotrophic basin within the Mediterranean Sea. The spatial distribution and diversity patterns of dead benthic foraminiferal (BF) faunas from the SL shelf were analyzed at 59 stations (40-100 water depths) sampled in August 2011 off the Israeli coast. Distinct dead BF assemblages were determined using multivariate statistical analyses, reflecting ecological preferences and their association with different environmental settings. The dead BF assemblages investigated in the current study were significantly different from the living BF assemblages explored in a previous study at the same stations. Ongoing human activity may explain these discrepancies, especially in the middle shelf, where continuous grain size coarsening, increase in carbonate content and decrease in TOC have occurred since the construction of the Aswan High Dam across the Nile River. These changes comprise (I) modest but clear changes in the lateral distribution of the biotopes, including continuous southward retreat of the southern middle shelf Nilotic biotope, and appearance of more fragmented, small biotopes due to the reduced impact of the Nile littoral cell; (II) dissimilarities in assemblage composition with higher numbers of opportunistic species occurring in the dead assemblages and increasing densities of sensitive taxa in the living assemblages.

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