Physiological responses of Pocillopora corals to upwelling events in the Eastern Tropical Pacific

Upwelling events can change the sea water conditions within few hours during several months on a seasonal regimen. These events are predicted to intensify due to climate change, exposing shallow benthic organisms to hypoxia and thermal stress, among other extreme conditions. Some coral reefs in the...

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Main Authors: Ana Lucia Castrillón-Cifuentes, Fernando A. Zapata, Christian Wild
Format: Article
Language:English
Published: Frontiers Media S.A. 2023-07-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2023.1212717/full
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author Ana Lucia Castrillón-Cifuentes
Ana Lucia Castrillón-Cifuentes
Fernando A. Zapata
Christian Wild
author_facet Ana Lucia Castrillón-Cifuentes
Ana Lucia Castrillón-Cifuentes
Fernando A. Zapata
Christian Wild
author_sort Ana Lucia Castrillón-Cifuentes
collection DOAJ
description Upwelling events can change the sea water conditions within few hours during several months on a seasonal regimen. These events are predicted to intensify due to climate change, exposing shallow benthic organisms to hypoxia and thermal stress, among other extreme conditions. Some coral reefs in the Eastern Tropical Pacific (ETP) recurrently experience upwelling events. Coral reefs off Gorgona Island, Colombia, are exposed to lower oxygen concentrations (3.0 - 3.7 mg O2 L-1) and lower temperatures (17 - 24°C) from mid-January to mid-April, when upwelling develops, compared to the rest of the year (4.9 ± 0.7 mg O2 L-1, 28.4 ± 0.3°C, mean ± SD). While no visible signs of stress have been reported for corals during upwelling, it can be hypothesized that corals would be negatively affected by these changes. Therefore, the objectives of this study were to (1) identify the effects of temperature and hypoxia on the metabolic rate (MO2) of Pocillopora corals under lab conditions, and (2) to examine the changes in skeletal growth and Symbiodiniaceae density of Pocillopora in the field between upwelling and non-upwelling seasons. Findings revealed that MO2 was significantly reduced by 20% at 24°C and significantly increased by 10% at 32°C compared to 28°C. During the upwelling season, Pocillopora corals exhibited a 52% increase in Symbiodiniaceae density, but the growth rate decreased by 50% compared to the non-upwelling season. Fast changes in water conditions during the upwelling strongly affects the metabolism of Pocillopora corals. Although conditions during upwelling were not lethal, they compromised the energy of the coral for their vital functions, indicating that upwelling pushes them toward their physiological limit. Consequently, predicted increases in upwelling events in combination with ocean warming and deoxygenation may be particularly critical for upwelling-exposed corals and the reefs they build in the Eastern Tropical Pacific.
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spelling doaj.art-7af8fef4dc56429da45c8f6a19b99f802023-07-31T13:16:53ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452023-07-011010.3389/fmars.2023.12127171212717Physiological responses of Pocillopora corals to upwelling events in the Eastern Tropical PacificAna Lucia Castrillón-Cifuentes0Ana Lucia Castrillón-Cifuentes1Fernando A. Zapata2Christian Wild3Marine Ecology Department, University of Bremen, Bremen, GermanyCoral Reef Ecology Research Group, Universidad del Valle, Cali, ColombiaCoral Reef Ecology Research Group, Universidad del Valle, Cali, ColombiaMarine Ecology Department, University of Bremen, Bremen, GermanyUpwelling events can change the sea water conditions within few hours during several months on a seasonal regimen. These events are predicted to intensify due to climate change, exposing shallow benthic organisms to hypoxia and thermal stress, among other extreme conditions. Some coral reefs in the Eastern Tropical Pacific (ETP) recurrently experience upwelling events. Coral reefs off Gorgona Island, Colombia, are exposed to lower oxygen concentrations (3.0 - 3.7 mg O2 L-1) and lower temperatures (17 - 24°C) from mid-January to mid-April, when upwelling develops, compared to the rest of the year (4.9 ± 0.7 mg O2 L-1, 28.4 ± 0.3°C, mean ± SD). While no visible signs of stress have been reported for corals during upwelling, it can be hypothesized that corals would be negatively affected by these changes. Therefore, the objectives of this study were to (1) identify the effects of temperature and hypoxia on the metabolic rate (MO2) of Pocillopora corals under lab conditions, and (2) to examine the changes in skeletal growth and Symbiodiniaceae density of Pocillopora in the field between upwelling and non-upwelling seasons. Findings revealed that MO2 was significantly reduced by 20% at 24°C and significantly increased by 10% at 32°C compared to 28°C. During the upwelling season, Pocillopora corals exhibited a 52% increase in Symbiodiniaceae density, but the growth rate decreased by 50% compared to the non-upwelling season. Fast changes in water conditions during the upwelling strongly affects the metabolism of Pocillopora corals. Although conditions during upwelling were not lethal, they compromised the energy of the coral for their vital functions, indicating that upwelling pushes them toward their physiological limit. Consequently, predicted increases in upwelling events in combination with ocean warming and deoxygenation may be particularly critical for upwelling-exposed corals and the reefs they build in the Eastern Tropical Pacific.https://www.frontiersin.org/articles/10.3389/fmars.2023.1212717/fullthermal stressmetabolic rategrowth rateZooxanthellae densityhypoxic threshold
spellingShingle Ana Lucia Castrillón-Cifuentes
Ana Lucia Castrillón-Cifuentes
Fernando A. Zapata
Christian Wild
Physiological responses of Pocillopora corals to upwelling events in the Eastern Tropical Pacific
Frontiers in Marine Science
thermal stress
metabolic rate
growth rate
Zooxanthellae density
hypoxic threshold
title Physiological responses of Pocillopora corals to upwelling events in the Eastern Tropical Pacific
title_full Physiological responses of Pocillopora corals to upwelling events in the Eastern Tropical Pacific
title_fullStr Physiological responses of Pocillopora corals to upwelling events in the Eastern Tropical Pacific
title_full_unstemmed Physiological responses of Pocillopora corals to upwelling events in the Eastern Tropical Pacific
title_short Physiological responses of Pocillopora corals to upwelling events in the Eastern Tropical Pacific
title_sort physiological responses of pocillopora corals to upwelling events in the eastern tropical pacific
topic thermal stress
metabolic rate
growth rate
Zooxanthellae density
hypoxic threshold
url https://www.frontiersin.org/articles/10.3389/fmars.2023.1212717/full
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