http://lod.bco-dmo.org/id/dataset/663524
eng; USA
utf8
dataset
Highest level of data collection, from a common set of sensors or instrumentation, usually within the same research project
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
2016-10-28
ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data
ISO 19115-2:2009(E)
Coral energy reserve data from Puerto Morelos, Mexico including calcification, chlorophyll a, stable isotopes, and health metrics
2016-10-28
publication
2016-10-28
revision
BCO-DMO Linked Data URI
2016-10-28
creation
http://lod.bco-dmo.org/id/dataset/663524
Andréa G. Grottoli
Ohio State University
principalInvestigator
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
publisher
Cite this dataset as: Grottoli, A. G. (2016) Coral energy reserve data from Puerto Morelos, Mexico including calcification, chlorophyll a, stable isotopes, and health metrics. Biological and Chemical Oceanography Data Management Office (BCO-DMO). Version Date 2016-10-28 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/663524 [access date]
Coral energy reserves; calcification, chlorophyll a, stable carbon isotopes, stable nitrogen isotopes Dataset Description: <p>This dataset includes metrics related to coral energy reserves. &nbsp;Fragments of coral species (<em>Orbicella faveolata</em>,&nbsp;<em>Porites astreoides</em>, and&nbsp;<em>Porites divaricata</em>)&nbsp;were analyzed for concentrations of lipids, proteins, carbohydrates, and chlorophyll a. Carbon isotopic ratios d13C and d15N were measured&nbsp;in both the host&nbsp;and endosymbiont. &nbsp;Health metrics are included&nbsp;which describe bleaching status.</p>
<p>These data were published in:</p>
<p>Schoepf V, Grottoli AG, Levas SJ, Aschaffenburg MD, Baumann J, Matsui Y, Warner ME. (2015) Annual coral bleaching can impair the long-term recovery capacity of corals. Proceedings of the Royal Society B 282: 20151887. <a href="http://dx.doi.org/10.1098/rspb.2015.1887" target="_blank">http://dx.doi.org/10.1098/rspb.2015.1887</a>.&nbsp;&nbsp;</p> Methods and Sampling: <p><strong>Experimental Design</strong> (text extracted from Grottoli et al., 2014. &nbsp;See publication for figures and full methods description)</p>
<p>In July 2009, 10 coral fragments from nine healthy colonies of Porites divaricata (branching morphology), Porites astreoides (mounding/encrusting morphology), and Orbicella faveolata (formerly Montastraea faveolata (large, mounding morphology) were collected near Puerto Morelos, Mexico (20 deg 500 N, 86 deg 520 W region). &nbsp;Parent colonies were all at least 10m apart and thus assumed to be genotypically different. &nbsp;Fragments were mounted on labeled PVC tiles, and randomly placed in 10 shaded (600 umol photons m(-2) &nbsp;s(-1) ) outdoor flow-through seawater tanks, allowed to acclimate for 5 days, and then buoyantly weighed. The temperature in five tanks was gradually raised to 31.5C +- 0.20C (single bleaching treatment) over 7 days then maintained at the elevated temperature, while the other five tanks received ambient reef water (controls; 30.6 C &nbsp;+- 0.24C) . After 15 days, one treatment and one control fragment from each parent colony of each species were buoyantly weighed and then frozen at 80 C (0 weeks on the reef). The remaining fragments were transplanted back to the reef at 4.9 m depth (20 deg 52.8150 N, 86 deg 50.9890 W). After 6 weeks on the reef, one additional treatment and control fragment from each colony of each species were collected, buoyantly weighed, and frozen at 80C, while the remaining fragments stayed on the reef for a full year at ambient reef temperatures.&nbsp;</p>
<p><strong>Chlorophyll a</strong> was determined according to Jeffrey &amp; Humphrey (1975)&nbsp; and standardized to surface area (Marsh 1970). Chlorophyll a values at 0 and 1.5 months on the reef following repeat bleaching are from Schoepf et al. (2011).</p>
<p><strong>Total soluble lipids</strong>, animal soluble protein and animal soluble carbohydrate were determined on ground, frozen coral fragments using established methods (Rodrigues &amp; Grottoli 2007; Schoepf et al 2013) and then converted to Joules per gram ash-free dry weight (Gnaiger &amp; Bitterlich 1984)).</p>
<p><strong>Net calcification</strong> was determined using the buoyant weight technique (Jokiel et al 1978) and standardized to surface area. Calcification rates at 0 and 1.5 months on the reef following repeat bleaching are from Grottoli et al. (2014).</p>
<p><strong>Tissue C and N isotopic analyses</strong> were performed on separated animal host and endosymbiont fractions using established methods (Rodrigues &amp; Grottoli 2006; Hughes et al 2010). &nbsp;The difference between d13Ch and d13Ce (i.e. d13Ch2e) was calculated to determine the relative contribution of photoautotrophic versus heterotrophic carbon to the coral (Rodrigues &amp; Grottoli 2006; Muscatine et al 1989). Repeated measurements of commercial standards (USGS-24, IAEA-N2) had a standard deviation of +- 0.04(permille)&nbsp;for d13C (n = 55) and +-0.11(permille) for d15N (n = 51).</p>
<p><strong>References:</strong></p>
<p>Gnaiger, E., and G. Bitterlich. "Proximate biochemical composition and caloric content calculated from elemental CHN analysis: a stoichiometric concept."&nbsp;<em>Oecologia</em>&nbsp;62.3 (1984): 289-298.&nbsp;<a href="http://dx.doi.org/10.1007/BF00384259">http://dx.doi.org/10.1007/BF00384259</a></p>
<p>Grottoli, Andréa G., et al. "The cumulative impact of annual coral bleaching can turn some coral species winners into losers."&nbsp;<em>Global change biology&nbsp;</em>20.12 (2014): 3823-3833.&nbsp;<a href="http://dx.doi.org/10.1111/gcb.12658">http://dx.doi.org/10.1111/gcb.12658</a></p>
<p>Hughes, A. D., et al. "Acquisition and assimilation of carbon in non-bleached and bleached corals."&nbsp;<em>Marine ecology progress series</em>&nbsp;420 (2010): 91-101.&nbsp;<a href="http://dx.doi.org/10.3354/meps08866">http://dx.doi.org/10.3354/meps08866</a></p>
<p>Jeffrey, SW T., and G. F. Humphrey. "New spectrophotometric equations for determining chlorophylls a, b, c1 and c2 in higher plants, algae and natural phytoplankton."&nbsp;<em>Biochem Physiol Pflanz BPP</em>&nbsp;(1975).</p>
<p>Jokiel, P. L., J. E. Maragos, and L. Franzisket. "Coral growth: buoyant weight technique."&nbsp;<em>Coral reefs: research methods. UNESCO, Paris</em>&nbsp;(1978): 529-541.</p>
<p>Marsh, James A. "Primary Productivity of Reef‐Building Calcareous Red Algae."&nbsp;Ecology&nbsp;51.2 (1970): 255-263.&nbsp;<a href="http://dx.doi.org/10.2307/1933661">http://dx.doi.org/10.2307/1933661</a></p>
<p>Muscatine, L., L. R. McCloskey, and R. E. Marian. "Estimating the daily contribution of carbon from zooxanthellae to coral animal respiration."&nbsp;<em>Oceanography</em>&nbsp;26.4 (1981).&nbsp;<a href="http://dx.doi.org/10.4319/lo.1981.26.4.0601">http://dx.doi.org/10.4319/lo.1981.26.4.0601</a></p>
<p>Rodrigues, Lisa J., and Andréa G. Grottoli. "Calcification rate and the stable carbon, oxygen, and nitrogen isotopes in the skeleton, host tissue, and zooxanthellae of bleached and recovering Hawaiian corals."&nbsp;<em>Geochimica et Cosmochimica Acta</em>&nbsp;70.11 (2006): 2781-2789.&nbsp;<a href="http://dx.doi.org/10.1016/j.gca.2006.02.014">http://dx.doi.org/10.1016/j.gca.2006.02.014</a></p>
<p>Rodrigues, Lisa J., and Andréa G. Grottoli. "Energy reserves and metabolism as indicators of coral recovery from bleaching."&nbsp;<em>Limnology and oceanography</em>52.5 (2007): 1874-1882.&nbsp;<a href="http://doi:10.4319/lo.2007.52.5.1874">http://doi:10.4319/lo.2007.52.5.1874</a></p>
<p>Schoepf, Verena, et al. "Short-term coral bleaching is not recorded by skeletal boron isotopes."&nbsp;PloS one&nbsp;9.11 (2014): e112011.&nbsp;<a href="http://dx.doi.org/10.1371/journal.pone.0112011">http://dx.doi.org/10.1371/journal.pone.0112011</a></p>
<p>Schoepf, V., et al. others (2013) "Coral energy reserves and calcification in a high-CO2 world at two temperatures."&nbsp;<em>PLoS ONE</em>&nbsp;8: e75049.&nbsp;<a href="http://dx.doi.org/75010.71371/journal.pone.0075049">http://dx.doi.org/75010.71371/journal.pone.0075049</a></p>
Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-0825413 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=0825413
completed
Andréa G. Grottoli
Ohio State University
614-292-5782
School of Earth Sciences 125 South Oval Mall
Columbus
OH
43210
United States
grottoli.1@osu.edu
pointOfContact
asNeeded
Unknown
coral_species
site_lat
site_lon
coral_id
treatment
months_until_rep
genotype
chl_a
lipid_J_gdw
protein_J_gdw
carbohdrate_J_gdw
calcification
d13C_h
d13C_e
d13C_h_e
d15N_h
d15N_e
lipid_g_gdw
protein_g_gdw
carbohydrate_g_gdw
health_0_months
health_1_5_months
health_11_months
Thermo-Finnigan Delta IV stable isotope mass spectrometer
theme
None, User defined
taxon
latitude
longitude
sample identification
treatment
time_elapsed
sample description
chlorophyll a
lipids in biota
protein concentration
carbohydrates
calcification
d13C measured in biota
d15N measured in biota
status
featureType
BCO-DMO Standard Parameters
Mass Spectrometer
instrument
BCO-DMO Standard Instruments
PM_2009_Grottoli
service
Deployment Activity
Puerto Morelos Reef National Park, Mexico
place
Locations
otherRestrictions
otherRestrictions
Access Constraints: none. Use Constraints: Please follow guidelines at: http://www.bco-dmo.org/terms-use Distribution liability: Under no circumstances shall BCO-DMO be liable for any direct, incidental, special, consequential, indirect, or punitive damages that result from the use of, or the inability to use, the materials in this data submission. If you are dissatisfied with any materials in this data submission your sole and exclusive remedy is to discontinue use.
Physiology and Biogeochemistry of Repeatedly Bleached and Recovering Caribbean Corals
https://osprey.bco-dmo.org/project/516103
Physiology and Biogeochemistry of Repeatedly Bleached and Recovering Caribbean Corals
<p><em>(Extracted from the NSF award abstract)</em></p>
<p>The overall stability and health of coral reefs is declining world-wide at an unprecedented rate. Mass coral bleaching, wherein exposure to elevated temperature leads to the loss of significant numbers of endosymbiotic dinoflagellates (Symbiodinium spp., commonly called zooxanthellae) and/or photosynthetic pigments, serves as a primary global example of how fragile this symbiosis is. While we have begun to understand the ecological and physiological impacts of bleaching, there remain key fundamental gaps in knowledge. In particular, it is becoming increasingly clear that a) not all corals either respond to, or recover from, bleaching events the same way, and that b) the impact of annual or repeated bleaching events on corals has not been examined in sufficient detail. Several non-mutually exclusive ecological and physiological pathways could impact how a particular coral species succumbs to or recovers from bleaching. Recent evidence suggests that the following features may play key roles for coral survival in the face of future seawater warming and mass bleaching events: 1) shifts in trophic partitioning (e.g., proportional reliance on autotrophy and heterotrophy) and energy reserve utilization, 2) enhanced thermal tolerance through host and algal-mediated physiological responses, and 3) harboring of different Symbiodinium phylotypes. However, these mechanisms have yet to be investigated in a unified approach that covers the entire coral holobiont system (algae, host tissue, and skeleton), or under scenarios of repeated bleaching.</p>
<p>The overall objectives of this study are as follows: 1) to determine the effect of single and repeated bleaching on the physiology, biogeochemistry, and recovery of some Caribbean coral species, and 2) to determine which Symbiodinium-type and host-species combinations are more resilient to single and repeated bleaching, what aspects of their physiology and biogeochemistry render them resilient, and to use this information to evaluate the long-term persistence of Caribbean coral reefs. To address these objectives, the following physiological variables will be measured: 1) Symbiodinium type, photochemical function and algal stress physiology, and 2) animal host energy reserves, defense enzyme concentration, skeletal growth, and feeding capacity in the corals Porites porites, Porites astreoides, and Montastraea faveolata. Corals will be examined immediately following thermal stress designed to approximate natural bleaching, and recovery will be monitored over short and long-term time scales. Next, the impact of repeated bleaching will be examined in the subsequent year, followed by examination over the next recovery period. This research is designed to simultaneously evaluate the symbiotic algae, coral host, and skeleton, and to identify patterns of physiological responses and recovery of each Symbiodinium-type and host-species combination that would be indicative of the resilience capacity of Caribbean corals to future more frequent thermal perturbations.</p>
repeat coral bleaching
largerWorkCitation
project
eng; USA
oceans
Puerto Morelos Reef National Park, Mexico
2016-10-28
Puerto Morelos, Mexico
0
BCO-DMO catalogue of parameters from Coral energy reserve data from Puerto Morelos, Mexico including calcification, chlorophyll a, stable isotopes, and health metrics
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
http://lod.bco-dmo.org/id/dataset-parameter/663580.rdf
Name: coral_species
Units: unitless
Description: <p>Scientific Name of coral</p>
http://lod.bco-dmo.org/id/dataset-parameter/663581.rdf
Name: site_lat
Units: decimal degrees
Description: <p>Latitude of sample site</p>
http://lod.bco-dmo.org/id/dataset-parameter/663582.rdf
Name: site_lon
Units: decimal degrees
Description: <p>Longitude of sample site; west is negative</p>
http://lod.bco-dmo.org/id/dataset-parameter/663583.rdf
Name: coral_id
Units: unitless
Description: <p>Coral identifier</p>
http://lod.bco-dmo.org/id/dataset-parameter/663584.rdf
Name: treatment
Units: unitless
Description: <p>Treatment (control=non-bleached; treatment=repeat bleached)</p>
http://lod.bco-dmo.org/id/dataset-parameter/663585.rdf
Name: months_until_rep
Units: unitless
Description: <p>Months on the reef following repeat bleaching</p>
http://lod.bco-dmo.org/id/dataset-parameter/663586.rdf
Name: genotype
Units: unitless
Description: <p>Parent colony genotype (each species has genotypes 1-9)</p>
http://lod.bco-dmo.org/id/dataset-parameter/663587.rdf
Name: chl_a
Units: micrograms per centimeter squared (ug/cm2)
Description: <p>Chlorophyll a content of the endosymbiont fraction standardized to surface area of the coral fragment</p>
http://lod.bco-dmo.org/id/dataset-parameter/663588.rdf
Name: lipid_J_gdw
Units: Joules per g ash-free dry weight (J/gdw)
Description: <p>Lipid concentration of the coral fragment</p>
http://lod.bco-dmo.org/id/dataset-parameter/663589.rdf
Name: protein_J_gdw
Units: Joules per g ash-free dry weight (J/gdw)
Description: <p>Protein concentration of the coral fragment</p>
http://lod.bco-dmo.org/id/dataset-parameter/663590.rdf
Name: carbohdrate_J_gdw
Units: Joules per g ash-free dry weight (J/gdw)
Description: <p>Carbohydrate concentration of the coral fragment</p>
http://lod.bco-dmo.org/id/dataset-parameter/663591.rdf
Name: calcification
Units: milligrams per day per centimeter squared (mg/day/cm2)
Description: <p>The daily calcification rate measured using the buoyant weight</p>
http://lod.bco-dmo.org/id/dataset-parameter/663592.rdf
Name: d13C_h
Units: per mil (o/oo)
Description: <p>Carbon isotopic ration (13C:12C) of the animal host "h" tissue</p>
http://lod.bco-dmo.org/id/dataset-parameter/663593.rdf
Name: d13C_e
Units: per mil (o/oo)
Description: <p>Carbon isotopic ratio (13C:12C) of the endosymbiont "e" tissue</p>
http://lod.bco-dmo.org/id/dataset-parameter/663594.rdf
Name: d13C_h_e
Units: per mil (o/oo)
Description: <p>Difference between the carbon isotopic composition of the animal host and that of the endosymbiont</p>
http://lod.bco-dmo.org/id/dataset-parameter/663595.rdf
Name: d15N_h
Units: per mil (o/oo)
Description: <p>Nitrogen isotopic composition of the animal host tissue</p>
http://lod.bco-dmo.org/id/dataset-parameter/663596.rdf
Name: d15N_e
Units: per mil (o/oo)
Description: <p>Nitrogen isotopic composition of the animal endosymbiont tissue</p>
http://lod.bco-dmo.org/id/dataset-parameter/663597.rdf
Name: lipid_g_gdw
Units: grams per g ash-free dry weight (g/gdw)
Description: <p>Lipid concentration of the coral fragment</p>
http://lod.bco-dmo.org/id/dataset-parameter/663598.rdf
Name: protein_g_gdw
Units: grams per g ash-free dry weight (g/gdw)
Description: <p>Protein concentration of the coral fragment</p>
http://lod.bco-dmo.org/id/dataset-parameter/663599.rdf
Name: carbohydrate_g_gdw
Units: grams per g ash-free dry weight (g/gdw)
Description: <p>Carbohydrate concentration of the coral fragment</p>
http://lod.bco-dmo.org/id/dataset-parameter/663600.rdf
Name: health_0_months
Units: unitless
Description: <p>Health status at 0 months (1=non-bleached; 2=partially bleached; 3=bleached; 4=partially dead non-bleached; 5=partially dead bleached; 6=dead)</p>
http://lod.bco-dmo.org/id/dataset-parameter/663601.rdf
Name: health_1_5_months
Units: unitless
Description: <p>Health status at 1.5 months (1=non-bleached; 2=partially bleached; 3=bleached; 4=partially dead non-bleached; 5=partially dead bleached; 6=dead)</p>
http://lod.bco-dmo.org/id/dataset-parameter/663602.rdf
Name: health_11_months
Units: unitless
Description: <p>Health status at 11 months (1=non-bleached; 2=partially bleached; 3=bleached; 4=partially dead non-bleached; 5=partially dead bleached; 6=dead)</p>
GB/NERC/BODC > British Oceanographic Data Centre, Natural Environment Research Council, United Kingdom
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
26703
https://datadocs.bco-dmo.org/file/oAAmoRMS8DmZ1L/coral_energy.csv
coral_energy.csv
Primary data file for dataset ID 663524
download
https://osprey.bco-dmo.org/dataset/663524/data/download
download
onLine
dataset
<p><strong>Experimental Design</strong> (text extracted from Grottoli et al., 2014. &nbsp;See publication for figures and full methods description)</p>
<p>In July 2009, 10 coral fragments from nine healthy colonies of Porites divaricata (branching morphology), Porites astreoides (mounding/encrusting morphology), and Orbicella faveolata (formerly Montastraea faveolata (large, mounding morphology) were collected near Puerto Morelos, Mexico (20 deg 500 N, 86 deg 520 W region). &nbsp;Parent colonies were all at least 10m apart and thus assumed to be genotypically different. &nbsp;Fragments were mounted on labeled PVC tiles, and randomly placed in 10 shaded (600 umol photons m(-2) &nbsp;s(-1) ) outdoor flow-through seawater tanks, allowed to acclimate for 5 days, and then buoyantly weighed. The temperature in five tanks was gradually raised to 31.5C +- 0.20C (single bleaching treatment) over 7 days then maintained at the elevated temperature, while the other five tanks received ambient reef water (controls; 30.6 C &nbsp;+- 0.24C) . After 15 days, one treatment and one control fragment from each parent colony of each species were buoyantly weighed and then frozen at 80 C (0 weeks on the reef). The remaining fragments were transplanted back to the reef at 4.9 m depth (20 deg 52.8150 N, 86 deg 50.9890 W). After 6 weeks on the reef, one additional treatment and control fragment from each colony of each species were collected, buoyantly weighed, and frozen at 80C, while the remaining fragments stayed on the reef for a full year at ambient reef temperatures.&nbsp;</p>
<p><strong>Chlorophyll a</strong> was determined according to Jeffrey &amp; Humphrey (1975)&nbsp; and standardized to surface area (Marsh 1970). Chlorophyll a values at 0 and 1.5 months on the reef following repeat bleaching are from Schoepf et al. (2011).</p>
<p><strong>Total soluble lipids</strong>, animal soluble protein and animal soluble carbohydrate were determined on ground, frozen coral fragments using established methods (Rodrigues &amp; Grottoli 2007; Schoepf et al 2013) and then converted to Joules per gram ash-free dry weight (Gnaiger &amp; Bitterlich 1984)).</p>
<p><strong>Net calcification</strong> was determined using the buoyant weight technique (Jokiel et al 1978) and standardized to surface area. Calcification rates at 0 and 1.5 months on the reef following repeat bleaching are from Grottoli et al. (2014).</p>
<p><strong>Tissue C and N isotopic analyses</strong> were performed on separated animal host and endosymbiont fractions using established methods (Rodrigues &amp; Grottoli 2006; Hughes et al 2010). &nbsp;The difference between d13Ch and d13Ce (i.e. d13Ch2e) was calculated to determine the relative contribution of photoautotrophic versus heterotrophic carbon to the coral (Rodrigues &amp; Grottoli 2006; Muscatine et al 1989). Repeated measurements of commercial standards (USGS-24, IAEA-N2) had a standard deviation of +- 0.04(permille)&nbsp;for d13C (n = 55) and +-0.11(permille) for d15N (n = 51).</p>
<p><strong>References:</strong></p>
<p>Gnaiger, E., and G. Bitterlich. "Proximate biochemical composition and caloric content calculated from elemental CHN analysis: a stoichiometric concept."&nbsp;<em>Oecologia</em>&nbsp;62.3 (1984): 289-298.&nbsp;<a href="http://dx.doi.org/10.1007/BF00384259">http://dx.doi.org/10.1007/BF00384259</a></p>
<p>Grottoli, Andréa G., et al. "The cumulative impact of annual coral bleaching can turn some coral species winners into losers."&nbsp;<em>Global change biology&nbsp;</em>20.12 (2014): 3823-3833.&nbsp;<a href="http://dx.doi.org/10.1111/gcb.12658">http://dx.doi.org/10.1111/gcb.12658</a></p>
<p>Hughes, A. D., et al. "Acquisition and assimilation of carbon in non-bleached and bleached corals."&nbsp;<em>Marine ecology progress series</em>&nbsp;420 (2010): 91-101.&nbsp;<a href="http://dx.doi.org/10.3354/meps08866">http://dx.doi.org/10.3354/meps08866</a></p>
<p>Jeffrey, SW T., and G. F. Humphrey. "New spectrophotometric equations for determining chlorophylls a, b, c1 and c2 in higher plants, algae and natural phytoplankton."&nbsp;<em>Biochem Physiol Pflanz BPP</em>&nbsp;(1975).</p>
<p>Jokiel, P. L., J. E. Maragos, and L. Franzisket. "Coral growth: buoyant weight technique."&nbsp;<em>Coral reefs: research methods. UNESCO, Paris</em>&nbsp;(1978): 529-541.</p>
<p>Marsh, James A. "Primary Productivity of Reef‐Building Calcareous Red Algae."&nbsp;Ecology&nbsp;51.2 (1970): 255-263.&nbsp;<a href="http://dx.doi.org/10.2307/1933661">http://dx.doi.org/10.2307/1933661</a></p>
<p>Muscatine, L., L. R. McCloskey, and R. E. Marian. "Estimating the daily contribution of carbon from zooxanthellae to coral animal respiration."&nbsp;<em>Oceanography</em>&nbsp;26.4 (1981).&nbsp;<a href="http://dx.doi.org/10.4319/lo.1981.26.4.0601">http://dx.doi.org/10.4319/lo.1981.26.4.0601</a></p>
<p>Rodrigues, Lisa J., and Andréa G. Grottoli. "Calcification rate and the stable carbon, oxygen, and nitrogen isotopes in the skeleton, host tissue, and zooxanthellae of bleached and recovering Hawaiian corals."&nbsp;<em>Geochimica et Cosmochimica Acta</em>&nbsp;70.11 (2006): 2781-2789.&nbsp;<a href="http://dx.doi.org/10.1016/j.gca.2006.02.014">http://dx.doi.org/10.1016/j.gca.2006.02.014</a></p>
<p>Rodrigues, Lisa J., and Andréa G. Grottoli. "Energy reserves and metabolism as indicators of coral recovery from bleaching."&nbsp;<em>Limnology and oceanography</em>52.5 (2007): 1874-1882.&nbsp;<a href="http://doi:10.4319/lo.2007.52.5.1874">http://doi:10.4319/lo.2007.52.5.1874</a></p>
<p>Schoepf, Verena, et al. "Short-term coral bleaching is not recorded by skeletal boron isotopes."&nbsp;PloS one&nbsp;9.11 (2014): e112011.&nbsp;<a href="http://dx.doi.org/10.1371/journal.pone.0112011">http://dx.doi.org/10.1371/journal.pone.0112011</a></p>
<p>Schoepf, V., et al. others (2013) "Coral energy reserves and calcification in a high-CO2 world at two temperatures."&nbsp;<em>PLoS ONE</em>&nbsp;8: e75049.&nbsp;<a href="http://dx.doi.org/75010.71371/journal.pone.0075049">http://dx.doi.org/75010.71371/journal.pone.0075049</a></p>
Specified by the Principal Investigator(s)
<p>Details of the statistical analysis methods are in <a href="http://dx.doi.org/10.1098/rspb.2015.1887" target="_blank">Schoepf et al 2015</a>.</p>
<p>BCO-DMO Processing Notes:</p>
<ul>
<li>added conventional header with dataset name, PI name, version date</li>
<li>modified parameter names to conform with BCO-DMO naming conventions</li>
<li>replaced blanks with underscores</li>
<li>added lat and lon&nbsp;of sampling locations based on coordinates in Grottoli et al. 2014.&nbsp;</li>
</ul>
Specified by the Principal Investigator(s)
asNeeded
7.x-1.1
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
Thermo-Finnigan Delta IV stable isotope mass spectrometer
Thermo-Finnigan Delta IV stable isotope mass spectrometer
PI Supplied Instrument Name: Thermo-Finnigan Delta IV stable isotope mass spectrometer PI Supplied Instrument Description:Costech Elemental Analyzer coupled to a Thermo-Finnigan Delta IV stable isotope mass spectrometer the Grottoli laboratory at Ohio State University. Instrument Name: Mass Spectrometer Instrument Short Name:Mass Spec Instrument Description: General term for instruments used to measure the mass-to-charge ratio of ions; generally used to find the composition of a sample by generating a mass spectrum representing the masses of sample components. Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/LAB16/
Deployment: PM_2009_Grottoli
PM_2009_Grottoli
Puerto_Morelos_Reef
shoreside
PM_2009_Grottoli
Andréa G. Grottoli
Ohio State University
Puerto_Morelos_Reef
shoreside