Low Bioerosion Rates on Inshore Turbid Reefs of Western Australia

Bioerosion on inshore reefs is expected to increase with global climate change reducing reef stability and accretionary potential. Most studies investigating bioerosion have focused on external grazers, such as parrotfish and urchins, whose biomass is more easily measured. Yet, cryptic endolithic bi...

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Main Authors: Shannon Dee, Thomas DeCarlo, Ivan Lozić, Jake Nilsen, Nicola K. Browne
Format: Article
Language:English
Published: MDPI AG 2023-01-01
Series:Diversity
Subjects:
Online Access:https://www.mdpi.com/1424-2818/15/1/62
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author Shannon Dee
Thomas DeCarlo
Ivan Lozić
Jake Nilsen
Nicola K. Browne
author_facet Shannon Dee
Thomas DeCarlo
Ivan Lozić
Jake Nilsen
Nicola K. Browne
author_sort Shannon Dee
collection DOAJ
description Bioerosion on inshore reefs is expected to increase with global climate change reducing reef stability and accretionary potential. Most studies investigating bioerosion have focused on external grazers, such as parrotfish and urchins, whose biomass is more easily measured. Yet, cryptic endolithic bioeroders such as macroboring (worms, sponges and bivalves) and microboring taxa (fungus and algae) have the potential to be the dominant source of reef erosion, especially among inshore reef systems exposed to increased nutrient supply. We measured bioerosion rates of bioeroder functional groups (microborers, macroborers, and grazers), and their response to environmental parameters (temperature, light, turbidity, chlorophyll <i>a</i>), as well as habitat variables (coral cover, turfing algae, macroalgae) across two inshore turbid reefs of north Western Australia. Total bioerosion rates were low (0.163 ± 0.012 kg m<sup>−2</sup> year<sup>−1</sup>) likely due to low light and nutrient levels. Macroborers were the dominant source of bioerosion and were positively correlated with turfing algae cover, highlighting the role of turf-grazing fish on endolithic bioerosion rates. Overall low bioerosion rates suggest that despite the reduced coral cover and carbonate production, these reefs may still maintain positive reef accretion rates, at least under current environmental conditions. However, an improved understanding of relationships between environmental drivers, habitat and grazing pressure with bioeroding communities is needed to improve predictions of reef carbonate loss with future climate change.
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spelling doaj.art-7de9a996501f4081b7e3267c5dfc6dc82023-11-30T21:54:03ZengMDPI AGDiversity1424-28182023-01-011516210.3390/d15010062Low Bioerosion Rates on Inshore Turbid Reefs of Western AustraliaShannon Dee0Thomas DeCarlo1Ivan Lozić2Jake Nilsen3Nicola K. Browne4School of Molecular and Life Sciences, Curtin University, Bentley Campus, Bentley, WA 6102, AustraliaCollege of Natural and Computational Sciences, Hawai’I Pacific University, 1 Aloha Tower Drive, Honolulu, HI 96813, USACentre for Microscopy, Characterisation, and Analysis, The University of Western Australia, Nedlands, WA 6009, AustraliaSchool of Molecular and Life Sciences, Curtin University, Bentley Campus, Bentley, WA 6102, AustraliaSchool of Molecular and Life Sciences, Curtin University, Bentley Campus, Bentley, WA 6102, AustraliaBioerosion on inshore reefs is expected to increase with global climate change reducing reef stability and accretionary potential. Most studies investigating bioerosion have focused on external grazers, such as parrotfish and urchins, whose biomass is more easily measured. Yet, cryptic endolithic bioeroders such as macroboring (worms, sponges and bivalves) and microboring taxa (fungus and algae) have the potential to be the dominant source of reef erosion, especially among inshore reef systems exposed to increased nutrient supply. We measured bioerosion rates of bioeroder functional groups (microborers, macroborers, and grazers), and their response to environmental parameters (temperature, light, turbidity, chlorophyll <i>a</i>), as well as habitat variables (coral cover, turfing algae, macroalgae) across two inshore turbid reefs of north Western Australia. Total bioerosion rates were low (0.163 ± 0.012 kg m<sup>−2</sup> year<sup>−1</sup>) likely due to low light and nutrient levels. Macroborers were the dominant source of bioerosion and were positively correlated with turfing algae cover, highlighting the role of turf-grazing fish on endolithic bioerosion rates. Overall low bioerosion rates suggest that despite the reduced coral cover and carbonate production, these reefs may still maintain positive reef accretion rates, at least under current environmental conditions. However, an improved understanding of relationships between environmental drivers, habitat and grazing pressure with bioeroding communities is needed to improve predictions of reef carbonate loss with future climate change.https://www.mdpi.com/1424-2818/15/1/62macro-bioerosionmicro-bioerosiongrazersmicroCT
spellingShingle Shannon Dee
Thomas DeCarlo
Ivan Lozić
Jake Nilsen
Nicola K. Browne
Low Bioerosion Rates on Inshore Turbid Reefs of Western Australia
Diversity
macro-bioerosion
micro-bioerosion
grazers
microCT
title Low Bioerosion Rates on Inshore Turbid Reefs of Western Australia
title_full Low Bioerosion Rates on Inshore Turbid Reefs of Western Australia
title_fullStr Low Bioerosion Rates on Inshore Turbid Reefs of Western Australia
title_full_unstemmed Low Bioerosion Rates on Inshore Turbid Reefs of Western Australia
title_short Low Bioerosion Rates on Inshore Turbid Reefs of Western Australia
title_sort low bioerosion rates on inshore turbid reefs of western australia
topic macro-bioerosion
micro-bioerosion
grazers
microCT
url https://www.mdpi.com/1424-2818/15/1/62
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