Human Activity Is Causing Toxic Thallium to Enter the Baltic Sea, According to New Study

Newswise — Woods Hole, Mass. -- Human activities account for a substantial amount - anywhere from 20% to more than 60% - of toxic thallium that has entered the Baltic Sea over the past 80 years, according to new research by scientists affiliated with the Woods Hole Oceanographic Institution (WHOI) and other institutions.

Currently, the amount of thallium (element symbol TI), which is considered the most toxic metal for mammals, remains low in Baltic seawater. However, the research suggests that the amount of thallium could increase due to further anthropogenic, or human induced, activities, or due to natural or human re-oxygenation of the Baltic that could make the sea less sulfide rich. Much of the thallium in the Baltic Sea, the largest human-induced hypoxic area on Earth, accumulates in the sediment thanks to abundant sulfide minerals.

“Anthropogenic activities release considerable amounts of toxic thallium annually. This study evidences an increase in the amount of thallium delivered by anthropogenic sources to the Baltic Sea since approximately 1947,” according to the journal article, “Anthropogenic forcing of the Baltic Sea thallium cycle,” published in Environmental Science & Technology.

“Humans are releasing a lot of thallium into the Baltic Sea, and people should be made aware of that. If this continues –  or if we further change the chemistry of the Baltic Sea in the future or if it naturally changes – then more thallium could accumulate. That would be of concern because of its toxicity,” said Chadlin Ostrander lead author of the article, which he conducted as a postdoctoral investigator in WHOI’s Department of Marine Chemistry and Geochemistry. Currently, he is an assistant professor in the Department of Geology & Geophysics at the University of Utah.

For the study, the researchers set out to better understand how thallium and its two stable isotopes ²⁰³Tl and ²⁰⁵Tl are cycled in the Baltic Sea. To discern modern thallium cycling, concentration and isotope ratio data were collected from seawater and shallow sediment core samples. To reconstruct thallium cycling further back in time, the researchers supplemented their short core samples with a longer sediment core that had been collected earlier near one of the deepest parts of the sea. They found Baltic seawater to be considerably more enriched in ²⁰⁵Tl than predicted. This enrichment started around 1940 to 1947 according to the longer sediment core.

It would be “highly coincidental” if the ²⁰⁵Tl increase was not associated with the “nearly contemporaneous trends linked to anthropogenic activities,” the article states. Though the exact sources of the thallium increase are not yet known, the article indicates that regional cement production, which was enhanced after the end of World War II, may play an important role, with other possible sources including coal combustion and the roasting of pyrite, an iron sulfide.

“For me, the most important aspect of the study is that we basically discovered that large portions – if not most – of the Baltic Sea are contaminated with the toxic metal thallium from human activities surrounding the basin,” said co-author Sune Nielsen, an adjunct scientist in WHOI’s Department of Geology & Geophysics. “As far as I am aware, this constitutes the geographically most extensive area of thallium contamination ever documented. It has long been known that the Baltic Sea has been strongly affected by anthropogenic activity, not least via the increasingly persistent loss of oxygen that has led to big losses for the fishing industry over the last several decades. As a Danish national, I follow the (bad) news about the Baltic in the Danish media, and our finding just adds another dimension to the already poor conditions in the basin for marine life. While thallium contamination may not be the most immediate concern for the Baltic Sea ecosystem, there is no doubt in my mind that it adds to the urgency of needing to do something to bring the Baltic Sea back to a state where humans and marine life can co-exist naturally.”

“Our data strengthens evidence that the removal of thallium from seawater and storage within sediments is tightly controlled by the absence of oxygen and presence of sulfide,” said co-author Colleen Hansel, a senior scientist in WHOI’s Department of Marine Chemistry and Geochemistry. “It is therefore concerning that recent movements to ‘solve the anoxia problem’ in the Baltic Sea involve pumping oxygen into the bottom waters. This oxygenation of the Baltic will likely lead to the release of thallium, as well as other sulfide-hosted metals like mercury, into the overlying seawater where they could bioaccumulate to toxic levels in fish. We predict, based on activities in the region, that the source of the thallium pollution is historic cement production in the region. As cement production continues to rise globally, this research could serve to caution manufacturers about the need to mitigate potential downstream effects of cement kiln dust on surrounding aquatic and marine ecosystems. This study highlights the utility of isotopes in identifying sources of pollutants to marine ecosystems, which is difficult to disentangle with concentration data alone.”

Funding for this research was provided by the U.S. National Science Foundation and by the Leibniz Association.

Key Takeaways:

• Human activities account for 20% to more than 60% of toxic thallium entering the Baltic Sea over the past eight decades, according to new research by scientists affiliated with the Woods Hole Oceanographic Institution and other institutions.
• Currently, the amount of thallium, which is considered the most toxic metal for mammals, remains low in Baltic seawater. Much of the thallium in the Baltic, which is the largest human-induced hypoxic area on Earth, has been accumulated in the sediment thanks to sulfide minerals.
• The amount of thallium could increase more due to further anthropogenic activities or due to natural or human re-oxygenation of the sea that could make the Baltic less sulfide rich.
• It would be “highly coincidental” if an observed increase in the amount of the heavier thallium stable isotope ²⁰⁵Tl was not associated with the “nearly contemporaneous trends linked to human activities,” according to the journal article.
• Though the exact sources of the thallium increase are not yet known, the article indicates that regional cement production, which was enhanced after the end of World War II, may play an important role, with other possible sources including coal combustion and the roasting of pyrite, an iron sulfide.

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Authors:  Chadlin M. Ostrander^1,2,†,*, Yunchao Shu^2,3,††, Sune G. Nielsen^{2,3,†††}, Olaf Dellwig⁴, Jerzy Blusztajn^2,3, Heide N. Schulz-Vogt⁵, Vera Hübner⁶, Colleen M. Hansel²

Affiliations:

¹Department of Marine Chemistry & Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA

²NIRVANA Laboratories, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA

³Department of Geology & Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA

⁴Department of Marine Geology, Leibniz Institute for Baltic Sea Research Warnemünde, IOW, Rostock, Germany

⁵Department of Biological Oceanography, Leibniz Institute for Baltic Sea Research Warnemünde, IOW, Rostock, Germany

⁶Microsensor group, Max Planck Institute for Marine Microbiology, Bremen, Germany

^†Now at Department of Geology & Geophysics, University of Utah, Salt Lake City, Utah, USA

^††Now at Department of Earth Sciences, University of Hong Kong, Pokfulam, Hong Kong

^†††Now at CRPG, CNRS, Université de Lorraine, 54500 Nancy, France

^* Corresponding author

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