Abundances and morphotypes of the coccolithophore Emiliania huxleyi in southern Patagonia compared to neighboring oceans and northern-hemisphere fjords
Coccolithophores are potentially affected by ongoing ocean acidification, where rising CO 2 lowers seawater pH and calcite saturation state (Ω cal ). Southern Patagonian fjords and channels provide natural laboratories for studying these issues due to high variability in physical and chemical condit...
| Main Authors: | , , , , , , |
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| Format: | Text |
| Language: | English |
| Published: |
2021
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| Subjects: | |
| Online Access: | https://doi.org/10.5194/bg-2020-449 https://bg.copernicus.org/preprints/bg-2020-449/ |
| Summary: | Coccolithophores are potentially affected by ongoing ocean acidification, where rising CO 2 lowers seawater pH and calcite saturation state (Ω cal ). Southern Patagonian fjords and channels provide natural laboratories for studying these issues due to high variability in physical and chemical conditions. We surveyed coccolithophore assemblages in Patagonian fjords during late-spring 2015 and early-spring 2017. Surface Ω cal exhibited large variations driven mostly by freshwater inputs. High Ω cal conditions (max. 3.6) occurred in the Archipelago Madre de Dios. Ω cal ranged from 2.0–2.6 in the western Strait of Magellan, 1.5–2.2 in the Inner Channel, and was sub-saturating (0.5) in Skyring Sound. Emiliania huxleyi was the only coccolithophore widely distributed in Patagonian fjords (> 96 % of total coccolitophores), only disappearing in the Skyring Sound, a semi-closed mesohaline system. Correspondence analysis associated higher E. huxleyi biomasses with lower diatom biomasses. The highest E. huxleyi abundances in Patagonia were in the lower range of those reported in Norwegian fjords. Predominant morphotypes were distinct from those previously documented in nearby oceans but similar to those of Norwegian fjords. Moderate-calcified forms of E. huxleyi A morphotype were uniformly distributed throughout Patagonia fjords. The exceptional R/hyper-calcified coccoliths, associated with low Ω cal values in Chilean and Peruvian coastal upwellings, were a minor component associated with high Ω cal levels in Patagonia. Outlying mean index (OMI) niche analysis suggested that pH/Ω cal conditions explained most variation in the realized niches of E. huxleyi morphotypes. The moderate-calcified A morphotype exhibited the widest niche-breadth (generalist), while the R/hyper-calcified morphotype exhibited a more restricted realized niche (specialist). Nevertheless, when considering an expanded sampling domain, including nearby Southeast Pacific coastal and offshore waters, even the R/hyper-calcified morphotype exhibited a higher niche breadth than other closely phylogenetically-related coccolithophore species. The occurrence of E. huxleyi in naturally low pH/Ω cal environments indicates that its ecological response is plastic and capable of adaptation. |
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