Atmospheric Deposition Effects on Mediterranean Marine Ecosystems

Summary

The Mediterranean Sea, bounded by arid continents and subject to frequent dust storms, is a naturally oligotrophic basin where external inputs of nutrients via atmospheric deposition play a pivotal role in regulating productivity, biogeochemical cycles and carbon export. Mineral dust, predominantly from the Sahara, delivers phosphorus, iron and trace metals that can alleviate nutrient limitation in surface waters, stimulating phytoplankton growth and altering community composition. Wet deposition processes, including dust scavenging by clouds and precipitation, often supply a pulse of bioavailable nitrogen and phosphorus, whereas dry deposition tends to release minerals more slowly and with lower nutrient solubility. These inputs can shift the balance between regenerated and new production, enhance microbial activity, and promote aggregation of particulate organic carbon (POC) through a lithogenic ballast effect. The magnitude and frequency of deposition events modulate deep carbon export efficiency, influence nitrogen fixation and interact with climate-driven changes in stratification. Understanding these deposition-driven dynamics is essential for predicting ecosystem responses under future scenarios of increased aridity and shifting atmospheric circulation.

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Atmospheric Deposition Effects on Mediterranean Marine Ecosystems publication trend

The graph below shows the total number of articles in atmospheric deposition effects on mediterranean marine ecosystems across all publications each year (not limited to Nature Index journals).

Technical terms

Oligotrophic: Waters with low nutrient concentrations and limited primary productivity.

Mesocosm: A contained experimental system used to simulate natural environmental conditions.

Particulate Organic Carbon (POC): Organic carbon particles in the water column, central to export flux.

New production: Primary production supported by externally supplied nutrients rather than recycled nutrients.

Regenerated production: Primary production based on nutrients recycled within the euphotic zone.

Lithogenic ballast effect: Enhanced sinking of organic matter due to aggregation with mineral particles.

References

  1. The Potential Impact of Saharan Dust and Polluted Aerosols on Microbial Populations in the East Mediterranean Sea, an Overview of a Mesocosm Experimental Approach. Frontiers in Marine Science (2016).
  2. Quantification of the lithogenic carbon pump following a simulated dust-deposition event in large mesocosms. Biogeosciences (2014).

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