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The role of diazotrophic cyanobacterial blooms in the expansion of bottom water hypoxia in the Holocene and late Weichselian Baltic Sea

Subject Area Palaeontology
Term from 2014 to 2018
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 261181348
 
Final Report Year 2020

Final Report Abstract

The modern Baltic Sea experiences massive blooms of N 2-fixing heterocytous cyanobacteria. These blooms facilitate the spread of hypoxic bottom waters due to the massive export or organic matter and its subsequent decay, rendering one-third of the Baltic Sea an ecological “dead zone”. Anthropogenic loading of nutrients (in particular phosphorous) is commonly considered the main reason for the proliferation of N2-fixing cyanobacteria in the Baltic Sea over the last decades. Other factors that may facilitate cyanobacterial bloom formation, however, are only poorly constrained. In this study, we analyzed sediments recovered during IODP Expedition 347: “Baltic Sea Paleoenvironment” to study the deglacial history of cyanobacterial blooms in the Baltic Sea. Bulk-geochemical, isotope and lipid biomarker data indicate that the postglacial Baltic Sea was a low productivity environment with a predominantly oxygenated water column. With the establishment of brackish conditions about 8000 years ago, the Baltic Sea repeatedly experienced blooms of heterocytous cyanobacteria that were tightly coupled to a spread of bottom water anoxia. All time periods of enhanced bloom formation were associated with an increase in surface water temperatures above 15 °C, suggesting that climate warming exerts a major control on the formation of cyanobacterial blooms in the Baltic Sea. Our results thus indicate that the combined effect of nutrient over-enrichment and increasing surface water temperatures may result in a significant intensification of cyanobacterial bloom events in the future Baltic Sea.

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