Volcanic CO2 seep geochemistry and use in understanding ocean acidification
| Autor: | Marco Milazzo, Jason M. Hall-Spencer, R. Di Napoli, Stefano Caliro, Alessandro Aiuppa, G. Turco |
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| Přispěvatelé: | Aiuppa A., Hall-Spencer J.M., Milazzo M., Turco G., Caliro S., Di Napoli R. |
| Jazyk: | angličtina |
| Rok vydání: | 2021 |
| Předmět: |
0106 biological sciences
Settore BIO/07 - Ecologia 010504 meteorology & atmospheric sciences Geochemistry Marine life 01 natural sciences chemistry.chemical_compound Algae Environmental Chemistry Submarine hydrothermalism Marine ecosystem 0105 earth and related environmental sciences Earth-Surface Processes Water Science and Technology Calcifying species Carbon dioxide in Earth's atmosphere biology 010604 marine biology & hydrobiology Natural analogues Coralline algae Ocean acidification biology.organism_classification Ecosystem effects Settore GEO/08 - Geochimica E Vulcanologia chemistry Carbon dioxide Environmental science Seawater |
| Popis: | Ocean acidification is one of the most dramatic effects of the massive atmospheric release of anthropogenic carbon dioxide (CO2) that has occurred since the Industrial Revolution, although its effects on marine ecosystems are not well understood. Submarine volcanic hydrothermal fields have geochemical conditions that provide opportunities to characterise the effects of elevated levels of seawater CO2 on marine life in the field. Here, we review the geochemical aspects of shallow marine CO2-rich seeps worldwide, focusing on both gas composition and water chemistry. We then describe the geochemical effects of volcanic CO2 seepage on the overlying seawater column. We also present new geochemical data and the first synthesis of marine biological community changes from one of the best-studied marine CO2 seep sites in the world (off Vulcano Island, Sicily). In areas of intense bubbling, extremely high levels of pCO2 (> 10,000 μatm) result in low seawater pH (2. Laboratory advances in our understanding of species sensitivity to high CO2 and low pH seawater, reveal how marine organisms react to simulated ocean acidification conditions (e.g., using energetic trade-offs for calcification, reproduction, growth and survival). Research at volcanic marine seeps, such as those off Vulcano, highlight consistent ecosystem responses to rising levels of seawater CO2, with the simplification of food webs, losses in functional diversity and reduced provisioning of goods and services for humans. |
| Databáze: | OpenAIRE |
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