Buoyant weight, chemical bioerosion, and mechanical bioerosion from sponge ocean acidification study; sponges collected in Florida Keys and State Waters of Miami Dade (NCEI Accession 0276485)
Coral reef ecosystems are experiencing increased rates of dissolution due to the impacts of ocean acidification (OA) on coral reef calcifiers and bioeroders. Here, we subjected common zooxanthellate (Cliona varians) and azooxanthellate (Pione lampa) Caribbean sponges to four pH treatments: pre-industrial (8.15), present-day (8.05) and two future OA scenarios (7.85 and 7.75). Total bioerosion (buoyant weight), chemical bioerosion, and mechanical bioerosion rates were measured to evaluate trends related to seawater pH. We identified a parabolic relationship between OA and sponge bioerosion, with the highest rates measured in the moderate OA treatment (7.85 pH) and decreasing under the more extreme OA treatment (7.75 pH). This suggests that sponges may become physiologically impaired under prolonged exposure to extreme OA, resulting in diminished bioerosion potential. These data reveal that carbonate dissolution is likely to increase in the upcoming decades as a result of OA-enhanced sponge bioerosion, but that the long-term persistence of reef habitat may benefit from reduced sponge bioerosion under late century OA scenarios.
Complete Metadata
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| description | Coral reef ecosystems are experiencing increased rates of dissolution due to the impacts of ocean acidification (OA) on coral reef calcifiers and bioeroders. Here, we subjected common zooxanthellate (Cliona varians) and azooxanthellate (Pione lampa) Caribbean sponges to four pH treatments: pre-industrial (8.15), present-day (8.05) and two future OA scenarios (7.85 and 7.75). Total bioerosion (buoyant weight), chemical bioerosion, and mechanical bioerosion rates were measured to evaluate trends related to seawater pH. We identified a parabolic relationship between OA and sponge bioerosion, with the highest rates measured in the moderate OA treatment (7.85 pH) and decreasing under the more extreme OA treatment (7.75 pH). This suggests that sponges may become physiologically impaired under prolonged exposure to extreme OA, resulting in diminished bioerosion potential. These data reveal that carbonate dissolution is likely to increase in the upcoming decades as a result of OA-enhanced sponge bioerosion, but that the long-term persistence of reef habitat may benefit from reduced sponge bioerosion under late century OA scenarios. |
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| identifier | gov.noaa.nodc:0276485 |
| issued | 2023-01-30T00:00:00.000+00:00 |
| keyword |
[
"0276485",
"ANIMALS - INDIVIDUAL - MASS",
"BIOEROSION",
"DISSOLVED INORGANIC CARBON (DIC)",
"INVERTEBRATE SPECIES",
"pH",
"SALINITY",
"total alkalinity",
"WATER TEMPERATURE",
"calipers",
"scale",
"temperature probe",
"chemical",
"laboratory analyses",
"physical",
"NOAA Atlantic Oceanographic and Meteorological Laboratory",
"NOAA Atlantic Oceanographic and Meteorological Laboratory",
"Coral Reef Conservation Program (CRCP)",
"CORAL REEF STUDIES",
"Coastal Waters of Florida",
"Florida Keys National Marine Sanctuary",
"North Atlantic Ocean",
"oceanography",
"DOC/NOAA/OAR/AOML > Atlantic Oceanographic and Meteorological Laboratory, OAR, NOAA, U.S. Department of Commerce",
"Numeric Data Sets > Bioerosion",
"Numeric Data Sets > Chemistry",
"EARTH SCIENCE > Biosphere > Zoology > Sponges",
"EARTH SCIENCE > Oceans > Coastal Processes > Coral Reefs",
"EARTH SCIENCE > Oceans > Coastal Processes > Erosion > Bioerosion",
"EARTH SCIENCE > Oceans > Marine Biology > Macroinvertebrates",
"EARTH SCIENCE > Oceans > Ocean Chemistry > Alkalinity",
"EARTH SCIENCE > Oceans > Ocean Chemistry > Dissolved Inorganic Carbon",
"EARTH SCIENCE > Oceans > Ocean Chemistry > Ocean Acidification",
"EARTH SCIENCE > Oceans > Ocean Chemistry > pH",
"EARTH SCIENCE > Oceans > Ocean Temperature > Water Temperature",
"EARTH SCIENCE > Oceans > Salinity/Density > Salinity",
"EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > ANIMALS/INVERTEBRATES",
"EARTH SCIENCE > OCEANS > OCEAN CHEMISTRY > ALKALINITY",
"EARTH SCIENCE > OCEANS > OCEAN CHEMISTRY > INORGANIC CARBON",
"EARTH SCIENCE > OCEANS > OCEAN CHEMISTRY > PH",
"EARTH SCIENCE > OCEANS > OCEAN TEMPERATURE > WATER TEMPERATURE",
"EARTH SCIENCE > OCEANS > SALINITY/DENSITY > SALINITY",
"buoyant weight",
"diameter",
"height",
"TEMPERATURE PROBES > TEMPERATURE PROBES",
"Anton Paar densitometer",
"Apollo SciTech, AS-ALK2",
"Apollo SciTech, AS-C3",
"Digi-Sense temperature probe",
"Ohaus analytical balance",
"COUNTRY/TERRITORY > United States of America > Florida > Monroe County > Florida Keys (24N081W0007)",
"COUNTRY/TERRITORY > United States of America > Florida > Upper Florida Keys (24N080W0018)",
"OCEAN BASIN > Atlantic Ocean > North Atlantic Ocean > Florida Reef Tract > Florida Keys (24N081W0007)",
"OCEAN BASIN > Atlantic Ocean > North Atlantic Ocean > Florida Reef Tract > Upper Florida Keys > Upper Florida Keys (24N080W0018)",
"OCEAN > ATLANTIC OCEAN > NORTH ATLANTIC OCEAN",
"OCEAN > ATLANTIC OCEAN > NORTH ATLANTIC OCEAN > GULF OF AMERICA",
"OCEAN > ATLANTIC OCEAN > NORTH ATLANTIC OCEAN > GULF OF MEXICO",
"Florida Keys",
"Miami Dade State Waters",
"CH9TDF"
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|
| landingPage | https://www.ncei.noaa.gov/contact |
| language |
[]
|
| license | https://creativecommons.org/publicdomain/zero/1.0/ |
| modified | 2023-08-22T00:00:00.000+00:00 |
| publisher |
{
"name": "NOAA National Centers for Environmental Information",
"@type": "org:Organization"
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|
| rights | otherRestrictions |
| spatial | -80.59028492,24.88029428,-80.609664228,24.902329724 |
| temporal | 2019-11-20T00:00:00+00:00/2020-10-16T00:00:00+00:00 |
| title | Buoyant weight, chemical bioerosion, and mechanical bioerosion from sponge ocean acidification study; sponges collected in Florida Keys and State Waters of Miami Dade (NCEI Accession 0276485) |