Spatial and temporal variations in turbidity on two inshore turbid reefs on the Great Barrier Reef, Australia

This study describes the natural turbidity regimes at two inshore turbid reefs on the central Great Barrier Reef where wind-driven waves are the main agent of sediment resuspension. Many corals on inshore turbid reefs have adapted to high and fluctuating turbidity, however, anthropogenic activities...

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Main Authors: Browne, Nicola, Smithers, S., Perry, C.
Format: Journal Article
Published: Springer Verlag 2013
Subjects:
Online Access:http://link.springer.com/article/10.1007%2Fs00338-012-0965-1
http://hdl.handle.net/20.500.11937/43142
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author Browne, Nicola
Smithers, S.
Perry, C.
author_facet Browne, Nicola
Smithers, S.
Perry, C.
author_sort Browne, Nicola
building Curtin Institutional Repository
collection Online Access
description This study describes the natural turbidity regimes at two inshore turbid reefs on the central Great Barrier Reef where wind-driven waves are the main agent of sediment resuspension. Many corals on inshore turbid reefs have adapted to high and fluctuating turbidity, however, anthropogenic activities such as dredging are speculated to produce larger and more prolonged turbidity events that may exceed the environmental tolerance and adaptive capacity of corals on these reefs. Natural turbidity regimes must be described and understood to determine whether and when coral communities on inshore turbid reefs are at risk from anthropogenically elevated turbidity, but at present few baseline studies exist. Here, we present turbidity data from (a) Middle Reef, a semi-protected reef located between Magnetic Island and Townsville and (b) Paluma Shoals, a reef exposed to higher energy wind and waves located in Halifax Bay. Instruments were deployed on both reefs for 16 days to measure spatial and temporal variations in turbidity and its driving forces (waves, currents, tides). Locally driven wind waves were the key driver of turbidity, but the strength of the relationship was dependent on wave exposure. Turbidity regimes thus vary markedly over individual reefs and this is reflected in community assemblage distributions, with a high abundance of heterotrophic corals (e.g. Goniopora) in reef habitats subjected to large fluctuations in turbidity (>100 NTU).A turbidity model developed using local wind speed data explained up to 75 % and up to 46 % of the variance in turbidity at Paluma Shoals and Middle Reef, respectively. Although the model was based on a brief two-week observational period, it reliably predicted variations in 24-h averaged turbidity and identified periods when turbidity rose above ambient baseline levels, offering reef managers insights into turbidity responses to modified climate and coastal sediment delivery regimes.
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spelling curtin-20.500.11937-431422017-09-13T15:07:52Z Spatial and temporal variations in turbidity on two inshore turbid reefs on the Great Barrier Reef, Australia Browne, Nicola Smithers, S. Perry, C. Hydrodynamics Community assemblages Reef morphology Sediment This study describes the natural turbidity regimes at two inshore turbid reefs on the central Great Barrier Reef where wind-driven waves are the main agent of sediment resuspension. Many corals on inshore turbid reefs have adapted to high and fluctuating turbidity, however, anthropogenic activities such as dredging are speculated to produce larger and more prolonged turbidity events that may exceed the environmental tolerance and adaptive capacity of corals on these reefs. Natural turbidity regimes must be described and understood to determine whether and when coral communities on inshore turbid reefs are at risk from anthropogenically elevated turbidity, but at present few baseline studies exist. Here, we present turbidity data from (a) Middle Reef, a semi-protected reef located between Magnetic Island and Townsville and (b) Paluma Shoals, a reef exposed to higher energy wind and waves located in Halifax Bay. Instruments were deployed on both reefs for 16 days to measure spatial and temporal variations in turbidity and its driving forces (waves, currents, tides). Locally driven wind waves were the key driver of turbidity, but the strength of the relationship was dependent on wave exposure. Turbidity regimes thus vary markedly over individual reefs and this is reflected in community assemblage distributions, with a high abundance of heterotrophic corals (e.g. Goniopora) in reef habitats subjected to large fluctuations in turbidity (>100 NTU).A turbidity model developed using local wind speed data explained up to 75 % and up to 46 % of the variance in turbidity at Paluma Shoals and Middle Reef, respectively. Although the model was based on a brief two-week observational period, it reliably predicted variations in 24-h averaged turbidity and identified periods when turbidity rose above ambient baseline levels, offering reef managers insights into turbidity responses to modified climate and coastal sediment delivery regimes. 2013 Journal Article http://hdl.handle.net/20.500.11937/43142 10.1007/s00338-012-0965-1 http://link.springer.com/article/10.1007%2Fs00338-012-0965-1 Springer Verlag restricted
spellingShingle Hydrodynamics
Community assemblages
Reef morphology
Sediment
Browne, Nicola
Smithers, S.
Perry, C.
Spatial and temporal variations in turbidity on two inshore turbid reefs on the Great Barrier Reef, Australia
title Spatial and temporal variations in turbidity on two inshore turbid reefs on the Great Barrier Reef, Australia
title_full Spatial and temporal variations in turbidity on two inshore turbid reefs on the Great Barrier Reef, Australia
title_fullStr Spatial and temporal variations in turbidity on two inshore turbid reefs on the Great Barrier Reef, Australia
title_full_unstemmed Spatial and temporal variations in turbidity on two inshore turbid reefs on the Great Barrier Reef, Australia
title_short Spatial and temporal variations in turbidity on two inshore turbid reefs on the Great Barrier Reef, Australia
title_sort spatial and temporal variations in turbidity on two inshore turbid reefs on the great barrier reef, australia
topic Hydrodynamics
Community assemblages
Reef morphology
Sediment
url http://link.springer.com/article/10.1007%2Fs00338-012-0965-1
http://hdl.handle.net/20.500.11937/43142