The effect of ocean acidification and temperature on the fertilization and embryonic development of the Sydney rock oyster Saccostrea glomerata (Gould 1850)

This study investigated the synergistic effects of ocean acidification (caused by elevations in the partial pressure of carbon dioxide pCO2) and temperature on the fertilization and embryonic development of the economically and ecologically important Sydney rock oyster, Saccostrea glomerata (Gould 1...

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Published in:Global Change Biology
Main Authors: Parker, L M, Ross, P M, O'Connor, W A
Format: Article in Journal/Newspaper
Language:English
Published: Wiley-Blackwell Publishing Ltd. 2009
Subjects:
Online Access:https://doi.org/10.1111/j.1365-2486.2009.01895.x
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spelling ftunivscoast:usc:23732 2023-05-15T17:49:57+02:00 The effect of ocean acidification and temperature on the fertilization and embryonic development of the Sydney rock oyster Saccostrea glomerata (Gould 1850) Parker, L M Ross, P M O'Connor, W A 2009 https://doi.org/10.1111/j.1365-2486.2009.01895.x eng eng Wiley-Blackwell Publishing Ltd. usc:23732 URN:ISSN: 1354-1013 FoR 06 (Biological Sciences) FoR 05 (Environmental Sciences) abnormality carbon dioxide climate change D-veliger embryonic development fertilization ocean acidification saccostrea glomerata Sydney rock oyster temperature acidification fertilization (reproduction) invertebrata Journal Article 2009 ftunivscoast https://doi.org/10.1111/j.1365-2486.2009.01895.x 2018-07-29T23:50:55Z This study investigated the synergistic effects of ocean acidification (caused by elevations in the partial pressure of carbon dioxide pCO2) and temperature on the fertilization and embryonic development of the economically and ecologically important Sydney rock oyster, Saccostrea glomerata (Gould 1850). As pCO2 increased, fertilization significantly decreased. The temperature of 26 °C was the optimum temperature for fertilization, as temperature increased and decreased from this optimum, fertilization decreased. There was also an effect of pCO2 and temperature on embryonic development. Generally as pCO2 increased, the percentage and size of D-veligers decreased and the percentage of D-veligers that were abnormal increased. The optimum temperature was 26 °C and embryonic development decreased at temperatures that were above and below this temperature. Abnormality of D-veligers was greatest at 1000 ppm and 18 and 30 °C (≥90%) and least at 375 ppm and 26 °C (≤4%). Finally prolonged exposure of elevated pCO2 and temperature across early developmental stages led to fewer D-veligers, more abnormality and smaller sizes in elevated CO2 environments and may lead to lethal effects at suboptimal temperatures. Embryos that were exposed to the pCO2 and temperature treatments for fertilization and embryonic development had fewer D-veligers, greater percentage of abnormality and reduced size than embryos that were exposed to the treatments for embryonic development only. Further at the elevated temperature of 30 °C and 750-1000 ppm, there was no embryonic development. The results of this study suggest that predicted changes in ocean acidification and temperature over the next century may have severe implications for the distribution and abundance of S. glomerata as well as possible implications for the reproduction and development of other marine invertebrates. © 2009 Blackwell Publishing Ltd. Article in Journal/Newspaper Ocean acidification University of the Sunshine Coast, Queensland, Australia: COAST Research Database Global Change Biology 15 9 2123 2136
institution Open Polar
collection University of the Sunshine Coast, Queensland, Australia: COAST Research Database
op_collection_id ftunivscoast
language English
topic FoR 06 (Biological Sciences)
FoR 05 (Environmental Sciences)
abnormality
carbon dioxide
climate change
D-veliger
embryonic development
fertilization
ocean acidification
saccostrea glomerata
Sydney rock oyster
temperature
acidification
fertilization (reproduction)
invertebrata
spellingShingle FoR 06 (Biological Sciences)
FoR 05 (Environmental Sciences)
abnormality
carbon dioxide
climate change
D-veliger
embryonic development
fertilization
ocean acidification
saccostrea glomerata
Sydney rock oyster
temperature
acidification
fertilization (reproduction)
invertebrata
Parker, L M
Ross, P M
O'Connor, W A
The effect of ocean acidification and temperature on the fertilization and embryonic development of the Sydney rock oyster Saccostrea glomerata (Gould 1850)
topic_facet FoR 06 (Biological Sciences)
FoR 05 (Environmental Sciences)
abnormality
carbon dioxide
climate change
D-veliger
embryonic development
fertilization
ocean acidification
saccostrea glomerata
Sydney rock oyster
temperature
acidification
fertilization (reproduction)
invertebrata
description This study investigated the synergistic effects of ocean acidification (caused by elevations in the partial pressure of carbon dioxide pCO2) and temperature on the fertilization and embryonic development of the economically and ecologically important Sydney rock oyster, Saccostrea glomerata (Gould 1850). As pCO2 increased, fertilization significantly decreased. The temperature of 26 °C was the optimum temperature for fertilization, as temperature increased and decreased from this optimum, fertilization decreased. There was also an effect of pCO2 and temperature on embryonic development. Generally as pCO2 increased, the percentage and size of D-veligers decreased and the percentage of D-veligers that were abnormal increased. The optimum temperature was 26 °C and embryonic development decreased at temperatures that were above and below this temperature. Abnormality of D-veligers was greatest at 1000 ppm and 18 and 30 °C (≥90%) and least at 375 ppm and 26 °C (≤4%). Finally prolonged exposure of elevated pCO2 and temperature across early developmental stages led to fewer D-veligers, more abnormality and smaller sizes in elevated CO2 environments and may lead to lethal effects at suboptimal temperatures. Embryos that were exposed to the pCO2 and temperature treatments for fertilization and embryonic development had fewer D-veligers, greater percentage of abnormality and reduced size than embryos that were exposed to the treatments for embryonic development only. Further at the elevated temperature of 30 °C and 750-1000 ppm, there was no embryonic development. The results of this study suggest that predicted changes in ocean acidification and temperature over the next century may have severe implications for the distribution and abundance of S. glomerata as well as possible implications for the reproduction and development of other marine invertebrates. © 2009 Blackwell Publishing Ltd.
format Article in Journal/Newspaper
author Parker, L M
Ross, P M
O'Connor, W A
author_facet Parker, L M
Ross, P M
O'Connor, W A
author_sort Parker, L M
title The effect of ocean acidification and temperature on the fertilization and embryonic development of the Sydney rock oyster Saccostrea glomerata (Gould 1850)
title_short The effect of ocean acidification and temperature on the fertilization and embryonic development of the Sydney rock oyster Saccostrea glomerata (Gould 1850)
title_full The effect of ocean acidification and temperature on the fertilization and embryonic development of the Sydney rock oyster Saccostrea glomerata (Gould 1850)
title_fullStr The effect of ocean acidification and temperature on the fertilization and embryonic development of the Sydney rock oyster Saccostrea glomerata (Gould 1850)
title_full_unstemmed The effect of ocean acidification and temperature on the fertilization and embryonic development of the Sydney rock oyster Saccostrea glomerata (Gould 1850)
title_sort effect of ocean acidification and temperature on the fertilization and embryonic development of the sydney rock oyster saccostrea glomerata (gould 1850)
publisher Wiley-Blackwell Publishing Ltd.
publishDate 2009
url https://doi.org/10.1111/j.1365-2486.2009.01895.x
genre Ocean acidification
genre_facet Ocean acidification
op_relation usc:23732
URN:ISSN: 1354-1013
op_doi https://doi.org/10.1111/j.1365-2486.2009.01895.x
container_title Global Change Biology
container_volume 15
container_issue 9
container_start_page 2123
op_container_end_page 2136
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