A 1500-year multiproxy record of coastal hypoxia from the northern Baltic Sea indicates unprecedented deoxygenation over the 20th century

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Jokinen , S , Virtasalo , J J , Jilbert , T , Kaiser , J , Dellwig , O , Arz , H W , Hänninen , J , Arppe , L , Collander , M & Saarinen , T 2018 , ' A 1500-year multiproxy record of coastal hypoxia from the northern Baltic Sea indicates unprecedented deoxygenation over the 20th century ' , Biogeosciences , vol. 15 , no. 13 , pp. 3975-4001 . https://doi.org/10.5194/bg-2018-25

Title: A 1500-year multiproxy record of coastal hypoxia from the northern Baltic Sea indicates unprecedented deoxygenation over the 20th century
Author: Jokinen, Sami; Virtasalo, Joonas J.; Jilbert, Tom; Kaiser, Jerome; Dellwig, Olaf; Arz, Helge W.; Hänninen, Jari; Arppe, Laura; Collander, Miia; Saarinen, Timo
Contributor: University of Helsinki, Helsinki Institute of Sustainability Science (HELSUS)
University of Helsinki, Natural Sciences Unit
Date: 2018-07-05
Number of pages: 27
Belongs to series: Biogeosciences
ISSN: 1726-4170
URI: http://hdl.handle.net/10138/237520
Abstract: The anthropogenically forced expansion of coastal hypoxia is a major environmental problem affecting coastal ecosystems and biogeochemical cycles throughout the world. The Baltic Sea is a semi-enclosed shelf sea whose central deep basins have been highly prone to deoxygenation during its Holocene history, as shown previously by numerous paleoenvironmental studies. However, long-term data on past fluctuations in the intensity of hypoxia in the coastal zone of the Baltic Sea are largely lacking, despite the significant role of these areas in retaining nutrients derived from the catchment. Here we present a 1500-year multiproxy record of near-bottom water redox changes from the coastal zone of the northern Baltic Sea, encompassing the climatic phases of the Medieval Climate Anomaly (MCA), the Little Ice Age (LIA), and the Modern Warm Period (MoWP). Our reconstruction shows that although multicentennial climate variability has modulated the depositional conditions and delivery of organic matter (OM) to the basin the modern aggravation of coastal hypoxia is unprecedented and, in addition to gradual changes in the basin configuration, it must have been forced by excess human-induced nutrient loading. Alongside the anthropogenic nutrient input, the progressive deoxygenation since the beginning of the 1900s was fueled by the combined effects of gradual shoaling of the basin and warming climate, which amplified sediment focusing and increased the vulnerability to hypoxia. Importantly, the eutrophication of coastal waters in our study area began decades earlier than previously thought, leading to a marked aggravation of hypoxia in the 1950s. We find no evidence of similar anthropogenic forcing during the MCA. These results have implications for the assessment of reference conditions for coastal water quality. Furthermore, this study highlights the need for combined use of sedimentological, ichnological, and geochemical proxies in order to robustly reconstruct subtle redox shifts especially in dynamic, non-euxinic coastal settings with strong seasonal contrasts in the bottom water quality.
Subject: SEDIMENTARY ORGANIC-MATTER
ATMOSPHERIC LEAD POLLUTION
ARCHIPELAGO SEA
MARINE-SEDIMENTS
LATE HOLOCENE
STOCKHOLM ARCHIPELAGO
SOURCE IDENTIFICATION
CYANOBACTERIA BLOOMS
EPICONTINENTAL BASIN
ESTUARINE SEDIMENTS
1172 Environmental sciences
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