Depth variation in benthic community response to repeated marine heatwaves on remote Central Indian Ocean reefs

Allbwn ymchwil: Cyfraniad at gyfnodolynErthygladolygiad gan gymheiriaid

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Depth variation in benthic community response to repeated marine heatwaves on remote Central Indian Ocean reefs. / Sannassy Pilly, Jyodee; Roche, Ronan; Richardson, Laura et al.
Yn: Royal Society Open Science, Cyfrol 11, Rhif 3, 27.03.2024, t. 231246.

Allbwn ymchwil: Cyfraniad at gyfnodolynErthygladolygiad gan gymheiriaid

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Sannassy Pilly J, Roche R, Richardson L, Turner J. Depth variation in benthic community response to repeated marine heatwaves on remote Central Indian Ocean reefs. Royal Society Open Science. 2024 Maw 27;11(3):231246. Epub 2024 Maw 27. doi: 10.1098/rsos.231246

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Sannassy Pilly, Jyodee ; Roche, Ronan ; Richardson, Laura et al. / Depth variation in benthic community response to repeated marine heatwaves on remote Central Indian Ocean reefs. Yn: Royal Society Open Science. 2024 ; Cyfrol 11, Rhif 3. tt. 231246.

RIS

TY - JOUR

T1 - Depth variation in benthic community response to repeated marine heatwaves on remote Central Indian Ocean reefs

AU - Sannassy Pilly, Jyodee

AU - Roche, Ronan

AU - Richardson, Laura

AU - Turner, John

N1 - © 2024 The Authors.

PY - 2024/3/27

Y1 - 2024/3/27

N2 - Coral reefs are increasingly impacted by climate-induced warming events. However, there is limited empirical evidence on the variation in the response of shallow coral reef communities to thermal stress across depths. Here, we assess depth-dependent changes in coral reef benthic communities following successive marine heatwaves from 2015 to 2017 across a 5–25 m depth gradient in the remote Chagos Archipelago, Central Indian Ocean. Our analyses show an overall decline in hard and soft coral cover and an increase in crustose coralline algae, sponge and reef pavement following successive marine heatwaves on the remote reef system. Our findings indicate that the changes in benthic communities in response to elevated seawater temperatures varied across depths. We found greater changes in benthic group cover at shallow depths (5–15 m) compared with deeper zones (15–25 m). The loss of hard coral cover was better predicted by initial thermal stress, while the loss of soft coral was associated with repeated thermal stress following successive warming events. Our study shows that benthic communities extending to 25 m depth were impacted by successive marine heatwaves, supporting concerns about the resilience of shallow coral reef communities to increasingly severe climate-driven warming events.

AB - Coral reefs are increasingly impacted by climate-induced warming events. However, there is limited empirical evidence on the variation in the response of shallow coral reef communities to thermal stress across depths. Here, we assess depth-dependent changes in coral reef benthic communities following successive marine heatwaves from 2015 to 2017 across a 5–25 m depth gradient in the remote Chagos Archipelago, Central Indian Ocean. Our analyses show an overall decline in hard and soft coral cover and an increase in crustose coralline algae, sponge and reef pavement following successive marine heatwaves on the remote reef system. Our findings indicate that the changes in benthic communities in response to elevated seawater temperatures varied across depths. We found greater changes in benthic group cover at shallow depths (5–15 m) compared with deeper zones (15–25 m). The loss of hard coral cover was better predicted by initial thermal stress, while the loss of soft coral was associated with repeated thermal stress following successive warming events. Our study shows that benthic communities extending to 25 m depth were impacted by successive marine heatwaves, supporting concerns about the resilience of shallow coral reef communities to increasingly severe climate-driven warming events.

KW - benthic communities

KW - climate-induced thermal stress

KW - depth zonation

KW - marine heatwaves

KW - remote reef systems

KW - shallow coral reefs

U2 - 10.1098/rsos.231246

DO - 10.1098/rsos.231246

M3 - Article

C2 - 38545610

VL - 11

SP - 231246

JO - Royal Society Open Science

JF - Royal Society Open Science

SN - 2054-5703

IS - 3

ER -