Dataset: Calcification data from outdoor flume experiments with coral Acropora hyacinthus at the UCB Gump Research Station Moorea, French Polynesia in September and October of 2012

ValidatedFinal no updates expectedDOI: 10.26008/1912/bco-dmo.754703.1Version 1 (2020-11-17)Dataset Type:Other Field Results

Principal Investigator: Robert Carpenter (California State University Northridge)

Co-Principal Investigator, Contact: Steeve Comeau (California State University Northridge)

Co-Principal Investigator: Peter J. Edmunds (California State University Northridge)

Technician: Griffin Srednick (California State University Northridge)

BCO-DMO Data Manager: Amber D. York (Woods Hole Oceanographic Institution)


Program: Long Term Ecological Research network (LTER)

Program: Science, Engineering and Education for Sustainability NSF-Wide Investment (SEES): Ocean Acidification (formerly CRI-OA) (SEES-OA)

Program: Science, Engineering and Education for Sustainability NSF-Wide Investment (SEES): Ocean Acidification (formerly CRI-OA) (SEES-OA)

Project: Moorea Coral Reef Long-Term Ecological Research site (MCR LTER)

Project: RUI: Ocean Acidification- Category 1- The effects of ocean acidification on the organismic biology and community ecology of corals, calcified algae, and coral reefs (OA_Corals)

Project: Collaborative Research: Ocean Acidification and Coral Reefs: Scale Dependence and Adaptive Capacity (OA coral adaptation)


Abstract

Coral calcification data from outdoor flumes at the UCB Gump Research Station Moorea, French Polynesia in September and October of 2012. These data were collected as part of a study of investigating how diel pCO2 oscillations modulate the response of the coral Acropora hyacinthus to ocean acidification. See Comeau et al. (2014) for details of this study.

Seven nubbins from upstream and downstream habitats were placed randomly in each of the 6 treatments, and calcification was measured over the 6 wk period using buoyant weighing (Davies 1989). Buoyant weight (±1 mg) was recorded at the beginning of the incubation and weekly thereafter to test for acclimation to the treatments. The difference in buoyant weight between each week of incubation was converted to dry weight using the density of aragonite (2.93 g cm−3) and used to calculate weekly rates of calcification. Calcification was normalized to surface area of the coral tissue (mg cm−2 d−1) determined using wax dipping (Stimson & Kinzie 1991). 

Parameters of the carbonate system were calculated from salinity, temperature, AT, and pHT using the R package seacarb (Lavigne and Gattuso, 2011).

Refer to publication Comeau et al. (2014) for specific methodology.


Related Datasets

IsRelatedTo

Dataset: Comeau 2014 MEPS: carbonate chemistry
Relationship Description: Carbonate chemistry data from the same study.
Carpenter, R., Edmunds, P. J. (2020) Carbonate chemistry from outdoor flume experiments with coral Acropora hyacinthus at the UCB Gump Research Station Moorea, French Polynesia in September and October of 2012. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2020-11-17 doi:10.26008/1912/bco-dmo.754736.1

Related Publications

Results

Comeau, S., Edmunds, P., Spindel, N., & Carpenter, R. (2014). Diel pCO2 oscillations modulate the response of the coral Acropora hyacinthus to ocean acidification. Marine Ecology Progress Series, 501, 99–111. doi:10.3354/meps10690
Methods

Davies, P.S. (1989). Short-term growth measurements of corals using an accurate buoyant weighing technique. Marine Biology, 101(3), 389–395. doi:10.1007/bf00428135
Methods

Stimson, J., & Kinzie, R. A. (1991). The temporal pattern and rate of release of zooxanthellae from the reef coral Pocillopora damicornis (Linnaeus) under nitrogen-enrichment and control conditions. Journal of Experimental Marine Biology and Ecology, 153(1), 63–74. doi:10.1016/s0022-0981(05)80006-1