Data

Metabolic consequences and vulnerability to stress during reproduction in spawning corals

Australian Ocean Data Network
Luke Edwards (Distributes) van Keulen, Mike (Point of contact)
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ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=https://catalogue.aodn.org.au:443/geonetwork/srv/api/records/516811d7-cd0d-207a-e0440003ba8c79dd&rft.title=Metabolic consequences and vulnerability to stress during reproduction in spawning corals&rft.identifier=516811d7-cd0d-207a-e0440003ba8c79dd&rft.publisher=Australian Ocean Data Network&rft.description=Of key interest is the change in oxygen metabolism through the coral reproductive cycle, and the influence of mass coral spawning on water column oxygen levels, which has led to large fish kills in the Coral Bay region. Initial work will establish baseline natural rates of photosynthesis, respiration and calcification and overall oxygen demand of the system. Natural observations and manipulative experiments will examine the effect of temperature, spawning slicks, sedimentation and nutrient influx on these processes. As these environmental variables are of particular concern at Ningaloo Reef it is important to understand whether our coral reef communities can survive potential perturbations and if so how will they be altered. Sexual reproduction has narrower tolerance to stress than other life functions, and as a result corals divert resources away from reproduction in response to variety of sublethal stresses. Additionally, as the gametogenic cycle of corals at Ningaloo Reef occurs during a period of natural environmental extremes, with some evidence such as bleaching to suggest corals are under stress, it is possible that the tolerance of corals to additional perturbations may be lower than normal. Key questions being addressed include: 1. What are the baseline rates of photosynthesis, respiration and calcification of corals? 2. What influence do temperature, sediment load, nutrient input and mass spawning have, individually and in combination? 3. How do these processes affect overall oxygen demand of the coral reef ecosystem? 4. Is there a change in metabolic stress in corals during the coral reproductive cycle? A programme of field and laboratory experiments will address these questions.Maintenance and Update Frequency: unknownStatement: Original record compiled for the Western Australian Marine Science Institution (WAMSI), Project 3.8, 2008. Originally sourced from several databases compiled by WA DEC Marine Science Branch of projects relevant to the marine parks of WA. Variable metadata information was available.&rft.creator=Anonymous&rft.date=2017&rft.coverage=westlimit=113.5; southlimit=-23.61; eastlimit=114.19; northlimit=-21.66&rft.coverage=westlimit=113.5; southlimit=-23.61; eastlimit=114.19; northlimit=-21.66&rft_rights=No Restrictions&rft_subject=biota&rft_subject=Biosphere | Zoology | Corals&rft_subject=Marine Features (Australia) | Ningaloo Marine Park, WA&rft_subject=Metabolism&rft_subject=Stress&rft_subject=Spawning&rft_subject=Reproductive Biology&rft.type=dataset&rft.language=English Access the data

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Brief description

Of key interest is the change in oxygen metabolism through the coral reproductive cycle, and the influence of mass coral spawning on water column oxygen levels, which has led to large fish kills in the Coral Bay region. Initial work will establish baseline "natural" rates of photosynthesis, respiration and calcification and overall oxygen demand of the system. Natural observations and manipulative experiments will examine the effect of temperature, spawning slicks, sedimentation and nutrient influx on these processes. As these environmental variables are of particular concern at Ningaloo Reef it is important to understand whether our coral reef communities can survive potential perturbations and if so how will they be altered. Sexual reproduction has narrower tolerance to stress than other life functions, and as a result corals divert resources away from reproduction in response to variety of sublethal stresses. Additionally, as the gametogenic cycle of corals at Ningaloo Reef occurs during a period of natural environmental extremes, with some evidence such as bleaching to suggest corals are under stress, it is possible that the tolerance of corals to additional perturbations may be lower than normal. Key questions being addressed include: 1. What are the baseline rates of photosynthesis, respiration and calcification of corals? 2. What influence do temperature, sediment load, nutrient input and mass spawning have, individually and in combination? 3. How do these processes affect overall oxygen demand of the coral reef ecosystem? 4. Is there a change in metabolic stress in corals during the coral reproductive cycle? A programme of field and laboratory experiments will address these questions.

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Maintenance and Update Frequency: unknown
Statement: Original record compiled for the Western Australian Marine Science Institution (WAMSI), Project 3.8, 2008. Originally sourced from several databases compiled by WA DEC Marine Science Branch of projects relevant to the marine parks of WA. Variable metadata information was available.

Notes

Credit
Mike van Keulen
Credit
Murdoch University

Modified: 06 2008

Data time period: 2005

This dataset is part of a larger collection

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114.19,-21.66 114.19,-23.61 113.5,-23.61 113.5,-21.66 114.19,-21.66

113.845,-22.635

text: westlimit=113.5; southlimit=-23.61; eastlimit=114.19; northlimit=-21.66

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  • global : 516811d7-cd0d-207a-e0440003ba8c79dd