Climate feedback loop: Rising seas unlock millennia of carbon?

Sediment cores extracted from a Guatemalan lake have revealed what scientists have dubbed ‘a troubling feedback loop’ between sea-level rise and carbon release, indicating that the one could accelerate the other and – ironically – the very changes driving it in the first place.

New research, published in Science of the Total Environment, suggests that rising seas may pose a threat far beyond the inundation of coastlines and that they could unlock vast reserves of carbon locked away in coastal ecosystems. 

The release of this carbon could then – potentially – “turbocharge” the atmospheric changes already driving sea-level rise in the first place.

The findings have emerged from a chemical analysis of sediment cores spanning roughly 9,500 years of environmental history, recently extracted from Lake Izabal in Guatemala by researchers at Missouri University of Science and Technology (Missouri S&T).

The lake has proved to be an exceptionally valuable archive for the study. Situated near coastal waterways, it has experienced repeated intrusions of seawater over millennia, making it a natural laboratory for understanding how saline inundation affects carbon-rich sediments. The researchers have noted that each compressed layer of organic material functions “as a time capsule” – preserving the chemical fingerprint of the conditions under which it was deposited.

By tracing how the carbon content of those layers shifted in response to historical flooding events, the team was able to reconstruct a stark pattern. When seawater penetrated the lake system, its elevated sulfate concentrations accelerated the microbial breakdown of organic matter – in some instances releasing up to 90% of the carbon stored in affected sediments into the atmosphere.