Thresholds of hypoxia of two Red Sea coral species (Porites sp. and Galaxea fascicularis)

Anthropogenic pressures have driven large-scale declines in coral cover on >50% of tropical coral reefs. Most research efforts have focused on ocean warming, ocean acidification, and overfishing impacts. Despite increasing instances of reef-associated hypoxic events, the role of reduced O2 in...

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Main Authors: Jacqueline V. Alva García, Shannon G. Klein, Taiba Alamoudi, Silvia Arossa, Anieka J. Parry, Alexandra Steckbauer, Carlos M. Duarte
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-10-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2022.945293/full
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author Jacqueline V. Alva García
Shannon G. Klein
Taiba Alamoudi
Silvia Arossa
Anieka J. Parry
Alexandra Steckbauer
Carlos M. Duarte
author_facet Jacqueline V. Alva García
Shannon G. Klein
Taiba Alamoudi
Silvia Arossa
Anieka J. Parry
Alexandra Steckbauer
Carlos M. Duarte
author_sort Jacqueline V. Alva García
collection DOAJ
description Anthropogenic pressures have driven large-scale declines in coral cover on >50% of tropical coral reefs. Most research efforts have focused on ocean warming, ocean acidification, and overfishing impacts. Despite increasing instances of reef-associated hypoxic events, the role of reduced O2 in affecting coral reef performance is largely unknown. Here, we assessed the hypoxic thresholds of two Red Sea coral species: Porites sp. and Galaxea fascicularis. We exposed coral fragments of both species to one control treatment (6.8 mg O2 L−1) and three reduced dissolved oxygen treatments (5.25, 3.5, and 1.25 mg O2 L−1) during a 10-day experiment. Across the two species, maximum (Fv/Fm) and effective (F′/Fm′) photochemical efficiency, chlorophyll a, and dark respiration declined under the lowest O2 treatment (1.25 mg O2 L−1). Porites sp. coral fragments, however, were remarkably resistant and showed no signs of sublethal bleaching after 10 days of exposure to reduced O2. Conversely, 17% of G. fascicularis fragments bleached after only three nights of exposure to the lowest O2 treatment (1.25 mg O2 L−1). Our data show that longer-term hypoxic events (i.e., days to weeks) can induce coral bleaching, but these effects depend on the extent of O2 reduction and are likely species-specific. Importantly, the levels of O2 usually defined as hypoxic (~2.0 to 2.8 mg O2 L−1) do not adequately capture the thresholds reported here. Hence, further research is urgently needed to more accurately describe the vulnerability of coral taxa to hypoxic and anoxic events.
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spelling doaj.art-62db14dc87be467d870f9cbbfc92cd3f2022-12-22T02:37:28ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452022-10-01910.3389/fmars.2022.945293945293Thresholds of hypoxia of two Red Sea coral species (Porites sp. and Galaxea fascicularis)Jacqueline V. Alva GarcíaShannon G. KleinTaiba AlamoudiSilvia ArossaAnieka J. ParryAlexandra SteckbauerCarlos M. DuarteAnthropogenic pressures have driven large-scale declines in coral cover on >50% of tropical coral reefs. Most research efforts have focused on ocean warming, ocean acidification, and overfishing impacts. Despite increasing instances of reef-associated hypoxic events, the role of reduced O2 in affecting coral reef performance is largely unknown. Here, we assessed the hypoxic thresholds of two Red Sea coral species: Porites sp. and Galaxea fascicularis. We exposed coral fragments of both species to one control treatment (6.8 mg O2 L−1) and three reduced dissolved oxygen treatments (5.25, 3.5, and 1.25 mg O2 L−1) during a 10-day experiment. Across the two species, maximum (Fv/Fm) and effective (F′/Fm′) photochemical efficiency, chlorophyll a, and dark respiration declined under the lowest O2 treatment (1.25 mg O2 L−1). Porites sp. coral fragments, however, were remarkably resistant and showed no signs of sublethal bleaching after 10 days of exposure to reduced O2. Conversely, 17% of G. fascicularis fragments bleached after only three nights of exposure to the lowest O2 treatment (1.25 mg O2 L−1). Our data show that longer-term hypoxic events (i.e., days to weeks) can induce coral bleaching, but these effects depend on the extent of O2 reduction and are likely species-specific. Importantly, the levels of O2 usually defined as hypoxic (~2.0 to 2.8 mg O2 L−1) do not adequately capture the thresholds reported here. Hence, further research is urgently needed to more accurately describe the vulnerability of coral taxa to hypoxic and anoxic events.https://www.frontiersin.org/articles/10.3389/fmars.2022.945293/fullcoral reefsdissolved oxygendeoxygenationO2 depletionexposure time
spellingShingle Jacqueline V. Alva García
Shannon G. Klein
Taiba Alamoudi
Silvia Arossa
Anieka J. Parry
Alexandra Steckbauer
Carlos M. Duarte
Thresholds of hypoxia of two Red Sea coral species (Porites sp. and Galaxea fascicularis)
Frontiers in Marine Science
coral reefs
dissolved oxygen
deoxygenation
O2 depletion
exposure time
title Thresholds of hypoxia of two Red Sea coral species (Porites sp. and Galaxea fascicularis)
title_full Thresholds of hypoxia of two Red Sea coral species (Porites sp. and Galaxea fascicularis)
title_fullStr Thresholds of hypoxia of two Red Sea coral species (Porites sp. and Galaxea fascicularis)
title_full_unstemmed Thresholds of hypoxia of two Red Sea coral species (Porites sp. and Galaxea fascicularis)
title_short Thresholds of hypoxia of two Red Sea coral species (Porites sp. and Galaxea fascicularis)
title_sort thresholds of hypoxia of two red sea coral species porites sp and galaxea fascicularis
topic coral reefs
dissolved oxygen
deoxygenation
O2 depletion
exposure time
url https://www.frontiersin.org/articles/10.3389/fmars.2022.945293/full
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