Investigation of submarine groundwater discharge into the Baltic Sea through varved glacial clays

Submarine groundwater discharge (SGD) is an important process responsible for transporting terrestrial dissolved chemical substances into the coastal ocean, thereby impacting the marine ecosystem. Despites its significance, there are few studies addressing SGD in the northern Baltic Sea. Here we investigate the potential occurrence of SGD in an area characterized by seafloor terraces formed in varved glacial clay located around Fifång Island, Southern Stockholm Archipelago. We analyzed 222 Rn activity and porewater geochemistry in both marine and terrestrial sediment cores retrieved from Fifång Island and its surrounding offshore areas. Results from 222 Rn mass-balance calculations, water isotopes, salinity, chloride concentration, and dating (including 14 C and helium-tritium dating) indicate that modern groundwater flows through varved glacial clay layers and fractured rocks on Fifång Island and discharges into Fifång Bay. Additionally, the offshore cores reveal a saline groundwater source that, dating of the dissolved inorganic carbon, appears systematically younger than the hosting clay varves dated using the Swedish clay varve chronology. Acoustic blanking in our acquired sub-bottom profiles may be related to this fluid migration. The occurrence of this saline groundwater seems to be independent from the distance to the submarine terraces. Collectively, our study confirms the occurrence of submarine groundwater in the varved glacial clay close to Fifång Island and further offshore. Our findings help establish the significance of submarine groundwater discharge in influencing the past and present coastal environment in the Baltic Sea region. • Groundwater pathways are investigated in onshore and offshore varved glacial clay. • Seawater invasion and modern fresh groundwater discharges into sea occur onshore. • Younger saline groundwater intrudes into 11k-year-old varved glacial clay offshore. • Paleo submarine groundwater may impact salinity records on the northern Baltic Sea coast.

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Publication Details

Journal
Continental Shelf Research
Published
2024-10-05
DOI
https://doi.org/10.1016/j.csr.2024.105337
Citations
4
Primary Topic
Methane Hydrates and Related Phenomena
Type
article
Field-Weighted Citation Impact
1.00

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article

Investigation of submarine groundwater discharge into the Baltic Sea through varved glacial clays

Tzu-Hao Huang, Valentí Rodellas, Carl‐Magnus Mörth, Carl Regnéll et al.
4 citations
Continental Shelf Research
Methane Hydrates and Related Phenomena
1.00
article

Investigation of submarine groundwater discharge into the Baltic Sea through varved glacial clays

Tzu-Hao Huang, Valentí Rodellas, Carl‐Magnus Mörth, Carl Regnéll, Jordi García-Orellana, Sophie ten Hietbrink, Florian Roth, Christian Stranne, Martin Jakobsson, Wei‐Li Hong, Hanna Sofia Marxen, Thomas Andrén, Anna Linderholm, Christoph Humborg, Matt O’Regan, Nai‐Chen Chen, Richard Gyllencreautz
article en
4 citations

Abstract

Submarine groundwater discharge (SGD) is an important process responsible for transporting terrestrial dissolved chemical substances into the coastal ocean, thereby impacting the marine ecosystem. Despites its significance, there are few studies addressing SGD in the northern Baltic Sea. Here we investigate the potential occurrence of SGD in an area characterized by seafloor terraces formed in varved glacial clay located around Fifång Island, Southern Stockholm Archipelago. We analyzed 222 Rn activity and porewater geochemistry in both marine and terrestrial sediment cores retrieved from Fifång Island and its surrounding offshore areas. Results from 222 Rn mass-balance calculations, water isotopes, salinity, chloride concentration, and dating (including 14 C and helium-tritium dating) indicate that modern groundwater flows through varved glacial clay layers and fractured rocks on Fifång Island and discharges into Fifång Bay. Additionally, the offshore cores reveal a saline groundwater source that, dating of the dissolved inorganic carbon, appears systematically younger than the hosting clay varves dated using the Swedish clay varve chronology. Acoustic blanking in our acquired sub-bottom profiles may be related to this fluid migration. The occurrence of this saline groundwater seems to be independent from the distance to the submarine terraces. Collectively, our study confirms the occurrence of submarine groundwater in the varved glacial clay close to Fifång Island and further offshore. Our findings help establish the significance of submarine groundwater discharge in influencing the past and present coastal environment in the Baltic Sea region. • Groundwater pathways are investigated in onshore and offshore varved glacial clay. • Seawater invasion and modern fresh groundwater discharges into sea occur onshore. • Younger saline groundwater intrudes into 11k-year-old varved glacial clay offshore. • Paleo submarine groundwater may impact salinity records on the northern Baltic Sea coast.

Continental Shelf ResearchVol. 282
Universitat Autònoma de Barcelona (ES), Södertörn University (SE), Stockholm University (SE), Centre for Palaeogenetics (SE), Bolin Centre for Climate Research (SE), Östersjöcentrum
Vetenskapsrådet, Strålsäkerhetsmyndigheten, H2020 European Research Council
Life below water
Openalex Percentile: Top 26%
Methane Hydrates and Related Phenomena
1.00
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