Stuart H. Larsen results 4
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Reading tea leaves worldwide: Decoupled drivers of initial litter decomposition mass‐loss rate and stabilizationNARA Subscribed
The breakdown of plant material fuels soil functioning and biodiversity. Currently, process understanding of global decomposition patterns and the drivers of such patterns are hampered by the lack of coherent large‐scale datasets. We buried 36,000 individual litterbags (tea bags) worldwide and found an overall negative correlation between initial mass‐loss rates and stabilization factors of plant‐derived carbon, using the Tea...
Thinking beyond the data: When the sea went darkNARA Subscribed
Five mass extinction events in earth's history each resulted in major oceanic species loss. All of these appear to be associated with significant atmospheric aerosol loading and a reduction in sunlight intensity at the surface. Importantly for marine species, it is not only the intensity of the incident light, but also its colour that is important as, within the ocean, only light with wavelengths less than about 550 nm penetra...
Ecotrons: Powerful and versatile ecosystem analysers for ecology, agronomy and environmental scienceNARA Subscribed
Ecosystems integrity and services are threatened by anthropogenic global changes. Mitigating and adapting to these changes require knowledge of ecosystem functioning in the expected novel environments, informed in large part through experimentation and modelling. This paper describes 13 advanced controlled environment facilities for experimental ecosystem studies, herein termed ecotrons, open to the international community. Ec...
The Arctic Mediterranean (AM) is the collective name for the Arctic Ocean, the Nordic Seas, and their adjacent shelf seas. Water enters into this region through the Bering Strait (Pacific inflow) and through the passages across the Greenland–Scotland Ridge (Atlantic inflow) and is modified within the AM. The modified waters leave the AM in several flow branches which are grouped into two different categories: (1) overflow of d...
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