Anthropocene publishes study
2020-08-25 (IPMA)
The global ocean plays a major role in modulating Earth’s climate by absorbing about one-third of anthropogenic emissions of CO2. However, this important ecosystem service comes with a cost: enhanced CO2 absorption since the onset of the industrial revolution has increased the oceans' acidity about 30% and is expected to increase up to 100% by the end of the century. While the chemical response of the marine CO2 system is known reasonably well, the effects of ocean acidification on marine ecosystems are poorly understood and need to be quantified. Owing to their low temperatures and moderate alkalinity, Southern Ocean waters are expected to experience the most severe impacts of ocean acidification. Therefore, these ecosystems can be used as bellwethers for prospective impacts of ocean acidification on marine ecosystems at mid and low latitudes. Coccolithophores, unicellular eukaryotic algae that secrete calcite plates (coccoliths; Figure 1), are the most abundant marine calcareous phytoplankton and play an important role in the marine carbon cycle by contributing to the oceanic pumps of organic matter and carbonate. The cosmopolitan coccolithophore Emiliania huxleyi is known to develop large-scale blooms in high latitudes systems where the overproduction and shedding of coccoliths gives the surface waters a milky-turquoise appearance allowing their detection from satellites.
The Marie-Skłodowska-Curie-funded Action SONaR-CO2 leaded by Spanish (Universidad de Salamanca) and Portuguese (IPMA & CCMAR) teams aims to shed light on the ongoing debate whether or not ocean acidification will lead to a replacement of heavily-calcified coccolithophores by lightly-calcified ones in polar and subpolar ecosystems. SONAR-CO2 aims to answer the call of the Southern Ocean Observing System Science Strategy for urgent and increased research efforts that address the impacts of ocean acidification on marine and coastal ecosystems and resources.
A recent study in Anthropocene by the SONaR-CO2 team assessed the changes that the subantarctic key stone species, Emiliania huxleyi, has experienced during the Industrial era. To do so, authors compared annual modern records of E. huxleyi coccoliths collected in the water column with those found in the underlying Holocene-aged sediment samples from south of Tasmania (Australia). Cutting-edge and traditional microscopy techniques were combined to evaluate changes in composition, morphology and calcification of E. huxleyi coccoliths. Results revealed that modern E. huxleyi coccoliths are similar to those produced before the industrial revolution, being only about 2% thinner than their pre-industrial counterparts. The subtle variation in coccolith calcification of E. huxleyi since the pre-industrial era contrasts sharply with the 30-35% reduction in shell weight of the other major pelagic calcifiers in the Southern Ocean, planktonic foraminifera. Overall, the results of this study reveal important differences in the natural response of major marine calcifying plankton groups to ongoing ocean acidification since the onset of the industrial revolution with subantarctic coccolithophores being more resilient than planktonic foraminifera.
Access the publication at the link below.
Imagens associadas
Complete cell (coccosphere) (a) and detached coccoliths (b) of the coccolithophore Emiliania huxleyi. Scale bar 1 µm.
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