Abundances and morphotypes of the coccolithophore <i>Emiliania huxleyi</i> in southern Patagonia compared to neighbouring oceans and Northern Hemisphere fjords
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Published:2021-10-08
Issue:19
Volume:18
Page:5465-5489
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ISSN:1726-4189
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Container-title:Biogeosciences
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language:en
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Short-container-title:Biogeosciences
Author:
Díaz-Rosas FranciscoORCID, Alves-de-Souza Catharina, Alarcón Emilio, Menschel Eduardo, González Humberto E., Torres Rodrigo, von Dassow Peter
Abstract
Abstract. Coccolithophores are potentially affected by ongoing
ocean acidification, where rising CO2 lowers seawater pH and calcite
saturation state (Ωcal). 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 Ωcal exhibited large variations driven mostly by
freshwater inputs. High-Ωcal conditions (max. 3.6) occurred in
the Archipelago Madre de Dios. Ωcal ranged from 2.0–2.6 in the
western Strait of Magellan and 1.5–2.2 in the inner channel and was
subsaturating (0.5) in Skyring Sound. Emiliania huxleyi was the only coccolithophore widely
distributed in Patagonian fjords (> 96 % of total
coccolithophores), 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. Moderately calcified forms of E. huxleyi A morphotype were
uniformly distributed throughout Patagonia fjords. The exceptional
R/hyper-calcified coccoliths, associated with low Ωcal values
in Chilean and Peruvian coastal upwellings, were a minor component
associated with high Ωcal levels in Patagonia. Outlying mean
index (OMI) niche analysis suggested that pH and Ωcal conditions
explained most variation in the realized niches of E. huxleyi morphotypes. The
moderately 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–Ωcal
environments indicates that its ecological response is plastic and capable
of adaptation.
Funder
Fondo Nacional de Desarrollo Científico y Tecnológico Instituto Milenio de Oceanografía Comisión Nacional de Investigación Científica y Tecnológica
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics
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