Over-calcified forms of the coccolithophore Emiliania huxley in high-CO2 waters are not preadapted to ocean acidification
© Author(s) 2018. Marine multicellular organisms inhabiting waters with natural high fluctuations in pH appear more tolerant to acidification than conspecifics occurring in nearby stable waters, suggesting that environments of fluctuating pH hold genetic reservoirs for adaptation of key groups to oc...
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Online Access: | https://doi.org/10.5194/bg-15-1515-2018 http://hdl.handle.net/10722/253187 |
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ftunivhongkonghu:oai:hub.hku.hk:10722/253187 2023-05-15T17:50:48+02:00 Over-calcified forms of the coccolithophore Emiliania huxley in high-CO2 waters are not preadapted to ocean acidification Mella-Flores, Daniella Gaitán-Espitia, Juan Diego Mahdi Bendif, El DÍaz-Rosas, Francisco Von Dassow, Peter Torres, Rodrigo Rokitta, Sebastian John, Uwe 2018 https://doi.org/10.5194/bg-15-1515-2018 http://hdl.handle.net/10722/253187 eng eng Biogeosciences Biogeosciences, 2018, v. 15, n. 5, p. 1515-1534 doi:10.5194/bg-15-1515-2018 1726-4189 1534 1726-4170 5 eid_2-s2.0-85043990633 1515 http://hdl.handle.net/10722/253187 15 Article 2018 ftunivhongkonghu https://doi.org/10.5194/bg-15-1515-2018 2023-01-14T16:24:51Z © Author(s) 2018. Marine multicellular organisms inhabiting waters with natural high fluctuations in pH appear more tolerant to acidification than conspecifics occurring in nearby stable waters, suggesting that environments of fluctuating pH hold genetic reservoirs for adaptation of key groups to ocean acidification (OA). The abundant and cosmopolitan calcifying phytoplankton Emiliania huxley exhibits a range of morphotypes with varying degrees of coccolith mineralization. We show that E. huxley populations in the naturally acidified upwelling waters of the eastern South Pacific, where pH drops below 7.8 as is predicted for the global surface ocean by the year 2100, are dominated by exceptionally over-calcified morphotypes whose distal coccolith shield can be almost solid calcite. Shifts in morphotype composition of E. huxley populations correlate with changes in carbonate system parameters. We tested if these correlations indicate that the hyper-calcified morphotype is adapted to OA. In experimental exposures to present-day vs. future pCO2 (400 vs. 1200 μatm), the over-calcified morphotypes showed the same growth inhibition (g-29.1±6.3 %) as moderately calcified morphotypes isolated from non-acidified water (g-30.7±8.8 %). Under the high-CO2-low-pH condition, production rates of particulate organic carbon (POC) increased, while production rates of particulate inorganic carbon (PIC) were maintained or decreased slightly (but not significantly), leading to lowered PIC / POC ratios in all strains. There were no consistent correlations of response intensity with strain origin. The high-CO2-low-pH condition affected coccolith morphology equally or more strongly in over-calcified strains compared to moderately calcified strains. High-CO2-low-pH conditions appear not to directly select for exceptionally over-calcified morphotypes over other morphotypes, but perhaps indirectly by ecologically correlated factors. More generally, these results suggest that oceanic planktonic microorganisms, despite their rapid turnover ... Article in Journal/Newspaper Ocean acidification University of Hong Kong: HKU Scholars Hub Huxley ENVELOPE(162.867,162.867,-77.850,-77.850) Pacific Biogeosciences 15 5 1515 1534 |
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Open Polar |
collection |
University of Hong Kong: HKU Scholars Hub |
op_collection_id |
ftunivhongkonghu |
language |
English |
description |
© Author(s) 2018. Marine multicellular organisms inhabiting waters with natural high fluctuations in pH appear more tolerant to acidification than conspecifics occurring in nearby stable waters, suggesting that environments of fluctuating pH hold genetic reservoirs for adaptation of key groups to ocean acidification (OA). The abundant and cosmopolitan calcifying phytoplankton Emiliania huxley exhibits a range of morphotypes with varying degrees of coccolith mineralization. We show that E. huxley populations in the naturally acidified upwelling waters of the eastern South Pacific, where pH drops below 7.8 as is predicted for the global surface ocean by the year 2100, are dominated by exceptionally over-calcified morphotypes whose distal coccolith shield can be almost solid calcite. Shifts in morphotype composition of E. huxley populations correlate with changes in carbonate system parameters. We tested if these correlations indicate that the hyper-calcified morphotype is adapted to OA. In experimental exposures to present-day vs. future pCO2 (400 vs. 1200 μatm), the over-calcified morphotypes showed the same growth inhibition (g-29.1±6.3 %) as moderately calcified morphotypes isolated from non-acidified water (g-30.7±8.8 %). Under the high-CO2-low-pH condition, production rates of particulate organic carbon (POC) increased, while production rates of particulate inorganic carbon (PIC) were maintained or decreased slightly (but not significantly), leading to lowered PIC / POC ratios in all strains. There were no consistent correlations of response intensity with strain origin. The high-CO2-low-pH condition affected coccolith morphology equally or more strongly in over-calcified strains compared to moderately calcified strains. High-CO2-low-pH conditions appear not to directly select for exceptionally over-calcified morphotypes over other morphotypes, but perhaps indirectly by ecologically correlated factors. More generally, these results suggest that oceanic planktonic microorganisms, despite their rapid turnover ... |
format |
Article in Journal/Newspaper |
author |
Mella-Flores, Daniella Gaitán-Espitia, Juan Diego Mahdi Bendif, El DÍaz-Rosas, Francisco Von Dassow, Peter Torres, Rodrigo Rokitta, Sebastian John, Uwe |
spellingShingle |
Mella-Flores, Daniella Gaitán-Espitia, Juan Diego Mahdi Bendif, El DÍaz-Rosas, Francisco Von Dassow, Peter Torres, Rodrigo Rokitta, Sebastian John, Uwe Over-calcified forms of the coccolithophore Emiliania huxley in high-CO2 waters are not preadapted to ocean acidification |
author_facet |
Mella-Flores, Daniella Gaitán-Espitia, Juan Diego Mahdi Bendif, El DÍaz-Rosas, Francisco Von Dassow, Peter Torres, Rodrigo Rokitta, Sebastian John, Uwe |
author_sort |
Mella-Flores, Daniella |
title |
Over-calcified forms of the coccolithophore Emiliania huxley in high-CO2 waters are not preadapted to ocean acidification |
title_short |
Over-calcified forms of the coccolithophore Emiliania huxley in high-CO2 waters are not preadapted to ocean acidification |
title_full |
Over-calcified forms of the coccolithophore Emiliania huxley in high-CO2 waters are not preadapted to ocean acidification |
title_fullStr |
Over-calcified forms of the coccolithophore Emiliania huxley in high-CO2 waters are not preadapted to ocean acidification |
title_full_unstemmed |
Over-calcified forms of the coccolithophore Emiliania huxley in high-CO2 waters are not preadapted to ocean acidification |
title_sort |
over-calcified forms of the coccolithophore emiliania huxley in high-co2 waters are not preadapted to ocean acidification |
publishDate |
2018 |
url |
https://doi.org/10.5194/bg-15-1515-2018 http://hdl.handle.net/10722/253187 |
long_lat |
ENVELOPE(162.867,162.867,-77.850,-77.850) |
geographic |
Huxley Pacific |
geographic_facet |
Huxley Pacific |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_relation |
Biogeosciences Biogeosciences, 2018, v. 15, n. 5, p. 1515-1534 doi:10.5194/bg-15-1515-2018 1726-4189 1534 1726-4170 5 eid_2-s2.0-85043990633 1515 http://hdl.handle.net/10722/253187 15 |
op_doi |
https://doi.org/10.5194/bg-15-1515-2018 |
container_title |
Biogeosciences |
container_volume |
15 |
container_issue |
5 |
container_start_page |
1515 |
op_container_end_page |
1534 |
_version_ |
1766157713355571200 |