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Row Type | Variable Name | Attribute Name | Data Type | Value |
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attribute | NC_GLOBAL | access_formats | String | .htmlTable,.csv,.json,.mat,.nc,.tsv,.esriCsv,.geoJson |
attribute | NC_GLOBAL | acquisition_description | String | Surface water samples (0-3m, n=195) for salinity, nutrients, total alkalinity\n(TA), and dissolved inorganic carbon (DIC) were collected from reef sites\nthroughout the Palauan archipelago at multiple time points between sunrise and\nsunset on September 19-24, 2011; March 28-April 7, 2012; December 7-9, 2012;\nand November 1-15, 2013 (detailed water sampling procedure in Shamberger et\nal. (2014)). Sampling was performed from small boats taken out daily from the\nPalau International Coral Reef Center (PICRC).\n \nIn situ temperature was measured in 2011 with TidbiT v2 water temperature data\nloggers produced by Onset with a manufacturer stated accuracy of 0.2 degrees\nC, in 2012 with a RBR XR-620 CTD with a manufacturer stated temperature\naccuracy of +/-0.002 degrees C, and in 2013 with a Sontek Castaway CTD with a\nmanufacturer stated temperature accuracy of +/-0.05 degrees C. Surface water\n(0-3 m) samples were collected multiple times a day between sunrise and sunset\nand on 3-9 separate days for each site from a Niskin bottle into 300 ml glass\nbottles (TA/DIC) and 125 ml glass bottles (salinity). Approximately 5 ml were\nremoved from each bottle to allow headspace for expansion and each TA/DIC\nsample was poisoned with 50 ul saturated mercuric chloride solution\nimmediately after collection to inhibit biological activity and then sealed\nwith screw tops and tape.\n \nTA and DIC analyses were performed using a Versatile Instrument for the\nDetermination of Total inorganic carbon and titration Alkalinity (VINDTA,\nMarianda Analytics and Data), which uses open cell potentiometric (TA) and\ncoulometric (DIC) titrations, and standardized using certified reference\nmaterials obtained from Andrew Dickson (Scripps Institution of Oceanography;\nDickson 2001, Dickson et al. 2007). Analysis of replicate samples (n=13)\nshowed a mean precision of ~2 umol/kg for TA and ~1 umol/kg for DIC. |
attribute | NC_GLOBAL | awards_0_award_nid | String | 54896 |
attribute | NC_GLOBAL | awards_0_award_number | String | OCE-1041106 |
attribute | NC_GLOBAL | awards_0_data_url | String | http://www.nsf.gov/awardsearch/showAward.do?AwardNumber=1041106 |
attribute | NC_GLOBAL | awards_0_funder_name | String | NSF Division of Ocean Sciences |
attribute | NC_GLOBAL | awards_0_funding_acronym | String | NSF OCE |
attribute | NC_GLOBAL | awards_0_funding_source_nid | String | 355 |
attribute | NC_GLOBAL | awards_0_program_manager | String | David L. Garrison |
attribute | NC_GLOBAL | awards_0_program_manager_nid | String | 50534 |
attribute | NC_GLOBAL | awards_1_award_nid | String | 520400 |
attribute | NC_GLOBAL | awards_1_award_number | String | OCE-1220529 |
attribute | NC_GLOBAL | awards_1_data_url | String | http://www.nsf.gov/awardsearch/showAward?AWD_ID=1220529 |
attribute | NC_GLOBAL | awards_1_funder_name | String | NSF Division of Ocean Sciences |
attribute | NC_GLOBAL | awards_1_funding_acronym | String | NSF OCE |
attribute | NC_GLOBAL | awards_1_funding_source_nid | String | 355 |
attribute | NC_GLOBAL | awards_1_program_manager | String | David L. Garrison |
attribute | NC_GLOBAL | awards_1_program_manager_nid | String | 50534 |
attribute | NC_GLOBAL | awards_2_award_nid | String | 560427 |
attribute | NC_GLOBAL | awards_2_award_number | String | OCE-1031971 |
attribute | NC_GLOBAL | awards_2_data_url | String | http://www.nsf.gov/awardsearch/showAward.do?AwardNumber=1031971 |
attribute | NC_GLOBAL | awards_2_funder_name | String | NSF Division of Ocean Sciences |
attribute | NC_GLOBAL | awards_2_funding_acronym | String | NSF OCE |
attribute | NC_GLOBAL | awards_2_funding_source_nid | String | 355 |
attribute | NC_GLOBAL | awards_2_program_manager | String | David L. Garrison |
attribute | NC_GLOBAL | awards_2_program_manager_nid | String | 50534 |
attribute | NC_GLOBAL | cdm_data_type | String | Other |
attribute | NC_GLOBAL | comment | String | Carbonate chemistry data from 13 coral reef sites in Palau \n PI: Anne Cohen (WHOI) \n Co-PIs: D. McCorkle (WHOI), A. Tarrant (WHOI), S. de Putron (BIOS), K. Karnauskas (WHOI) \n Contact: Hannah Barkley or Anne Cohen (WHOI); K. Shamberger (TAMU) \n Version History: \n updated/current version: 23 June 2015 \n original data submitted by K.Shamberger (TAMU): 29 Jan 2014 |
attribute | NC_GLOBAL | Conventions | String | COARDS, CF-1.6, ACDD-1.3 |
attribute | NC_GLOBAL | creator_email | String | info at bco-dmo.org |
attribute | NC_GLOBAL | creator_name | String | BCO-DMO |
attribute | NC_GLOBAL | creator_type | String | institution |
attribute | NC_GLOBAL | creator_url | String | https://www.bco-dmo.org/ |
attribute | NC_GLOBAL | data_source | String | extract_data_as_tsv version 2.3 19 Dec 2019 |
attribute | NC_GLOBAL | date_created | String | 2014-01-29T20:31:51Z |
attribute | NC_GLOBAL | date_modified | String | 2019-11-14T19:48:11Z |
attribute | NC_GLOBAL | defaultDataQuery | String | &time<now |
attribute | NC_GLOBAL | doi | String | 10.1575/1912/bco-dmo.489014.1 |
attribute | NC_GLOBAL | Easternmost_Easting | double | 134.557 |
attribute | NC_GLOBAL | geospatial_lat_max | double | 7.577 |
attribute | NC_GLOBAL | geospatial_lat_min | double | 7.158 |
attribute | NC_GLOBAL | geospatial_lat_units | String | degrees_north |
attribute | NC_GLOBAL | geospatial_lon_max | double | 134.557 |
attribute | NC_GLOBAL | geospatial_lon_min | double | 134.349 |
attribute | NC_GLOBAL | geospatial_lon_units | String | degrees_east |
attribute | NC_GLOBAL | infoUrl | String | https://www.bco-dmo.org/dataset/489014 |
attribute | NC_GLOBAL | institution | String | BCO-DMO |
attribute | NC_GLOBAL | instruments_0_acronym | String | Niskin bottle |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_description | String | Surface water (0-3 m) samples were collected multiple times a day between sunrise and sunset and on 3-9 separate days for each site from a Niskin bottle into 300 ml glass bottles (TA/DIC) and 125 ml glass bottles (salinity). |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_nid | String | 489282 |
attribute | NC_GLOBAL | instruments_0_description | String | A Niskin bottle (a next generation water sampler based on the Nansen bottle) is a cylindrical, non-metallic water collection device with stoppers at both ends. The bottles can be attached individually on a hydrowire or deployed in 12, 24 or 36 bottle Rosette systems mounted on a frame and combined with a CTD. Niskin bottles are used to collect discrete water samples for a range of measurements including pigments, nutrients, plankton, etc. |
attribute | NC_GLOBAL | instruments_0_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L22/current/TOOL0412/ |
attribute | NC_GLOBAL | instruments_0_instrument_name | String | Niskin bottle |
attribute | NC_GLOBAL | instruments_0_instrument_nid | String | 413 |
attribute | NC_GLOBAL | instruments_0_supplied_name | String | Niskin bottle |
attribute | NC_GLOBAL | instruments_1_acronym | String | Water Temp Sensor |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_description | String | In 2011, in situ temperature was measured with TidbiT v2 water temperature data loggers produced by Onset with a manufacturer stated accuracy of 0.2 degrees C. In 2012, in situ temperature was measured with a RBR XR-620 CTD with a manufacturer stated temperature accuracy of +/- 0.002 degrees C.\nInformation from the manufacturers:TidbiT v2 Temperature Data LoggerRBR XR-620 |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_nid | String | 489281 |
attribute | NC_GLOBAL | instruments_1_description | String | General term for an instrument that measures the temperature of the water with which it is in contact (thermometer). |
attribute | NC_GLOBAL | instruments_1_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/134/ |
attribute | NC_GLOBAL | instruments_1_instrument_name | String | Water Temperature Sensor |
attribute | NC_GLOBAL | instruments_1_instrument_nid | String | 647 |
attribute | NC_GLOBAL | instruments_1_supplied_name | String | Water Temperature Sensors |
attribute | NC_GLOBAL | instruments_2_acronym | String | inorganic carbon and alkalinity analyser |
attribute | NC_GLOBAL | instruments_2_dataset_instrument_description | String | TA and DIC analyses were performed with a Versatile INstrument for the Determination of Total inorganic carbon and titration Alkalinity (VINDTA) produced by Marianda Marine Analytics and Data. The VINDTA uses coulometric titration for DIC analysis and an open cell potentiometric titration for TA analysis. |
attribute | NC_GLOBAL | instruments_2_dataset_instrument_nid | String | 489284 |
attribute | NC_GLOBAL | instruments_2_description | String | The Versatile INstrument for the Determination of Total inorganic carbon and titration Alkalinity (VINDTA) 3C is a laboratory alkalinity titration system combined with an extraction unit for coulometric titration, which simultaneously determines the alkalinity and dissolved inorganic carbon content of a sample. The sample transport is performed with peristaltic pumps and acid is added to the sample using a membrane pump. No pressurizing system is required and only one gas supply (nitrogen or dry and CO2-free air) is necessary. The system uses a Metrohm Titrino 719S, an ORION-Ross pH electrode and a Metrohm reference electrode. The burette, the pipette and the analysis cell have a water jacket around them. Precision is typically +/- 1 umol/kg for TA and/or DIC in open ocean water. |
attribute | NC_GLOBAL | instruments_2_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L22/current/TOOL0481/ |
attribute | NC_GLOBAL | instruments_2_instrument_name | String | MARIANDA VINDTA 3C total inorganic carbon and titration alkalinity analyser |
attribute | NC_GLOBAL | instruments_2_instrument_nid | String | 686 |
attribute | NC_GLOBAL | instruments_2_supplied_name | String | VINDTA |
attribute | NC_GLOBAL | keywords | String | altimetry, ammonia, ammonium, bco, bco-dmo, bicarbonate, biological, carbon, carbon dioxide, carbonate, chemical, chemistry, co2, CO2_diss, co3, concentration, data, dataset, date, dic, dioxide, diss, dmo, earth, Earth Science > Oceans > Ocean Chemistry > Ammonia, Earth Science > Oceans > Ocean Chemistry > Nitrate, Earth Science > Oceans > Ocean Chemistry > pH, Earth Science > Oceans > Ocean Chemistry > Phosphate, erddap, laboratory, latitude, longitude, management, mass, mass_concentration_of_phosphate_in_sea_water, mole, mole_concentration_of_ammonium_in_sea_water, mole_concentration_of_nitrate_in_sea_water, n02, name, nh4, nitrate, no3, NO3_NO2, ocean, oceanography, oceans, office, omega, omega_Ar, omega_Ca, pCO2, phosphate, po4, preliminary, reported, sal, satellite, scale, science, sea, sea_water_ph_reported_on_total_scale, seawater, site, site_name, temperature, time, time2, total, water |
attribute | NC_GLOBAL | keywords_vocabulary | String | GCMD Science Keywords |
attribute | NC_GLOBAL | license | String | https://www.bco-dmo.org/dataset/489014/license |
attribute | NC_GLOBAL | metadata_source | String | https://www.bco-dmo.org/api/dataset/489014 |
attribute | NC_GLOBAL | Northernmost_Northing | double | 7.577 |
attribute | NC_GLOBAL | param_mapping | String | {'489014': {'lat': 'master - latitude', 'lon': 'master - longitude'}} |
attribute | NC_GLOBAL | parameter_source | String | https://www.bco-dmo.org/mapserver/dataset/489014/parameters |
attribute | NC_GLOBAL | people_0_affiliation | String | Woods Hole Oceanographic Institution |
attribute | NC_GLOBAL | people_0_affiliation_acronym | String | WHOI |
attribute | NC_GLOBAL | people_0_person_name | String | Anne L Cohen |
attribute | NC_GLOBAL | people_0_person_nid | String | 51428 |
attribute | NC_GLOBAL | people_0_role | String | Lead Principal Investigator |
attribute | NC_GLOBAL | people_0_role_type | String | originator |
attribute | NC_GLOBAL | people_1_affiliation | String | Bermuda Institute of Ocean Sciences |
attribute | NC_GLOBAL | people_1_affiliation_acronym | String | BIOS |
attribute | NC_GLOBAL | people_1_person_name | String | Samantha J. de Putron |
attribute | NC_GLOBAL | people_1_person_nid | String | 51431 |
attribute | NC_GLOBAL | people_1_role | String | Co-Principal Investigator |
attribute | NC_GLOBAL | people_1_role_type | String | originator |
attribute | NC_GLOBAL | people_2_affiliation | String | Woods Hole Oceanographic Institution |
attribute | NC_GLOBAL | people_2_affiliation_acronym | String | WHOI |
attribute | NC_GLOBAL | people_2_person_name | String | Kristopher Karnauskas |
attribute | NC_GLOBAL | people_2_person_nid | String | 560431 |
attribute | NC_GLOBAL | people_2_role | String | Co-Principal Investigator |
attribute | NC_GLOBAL | people_2_role_type | String | originator |
attribute | NC_GLOBAL | people_3_affiliation | String | Woods Hole Oceanographic Institution |
attribute | NC_GLOBAL | people_3_affiliation_acronym | String | WHOI |
attribute | NC_GLOBAL | people_3_person_name | String | Daniel C McCorkle |
attribute | NC_GLOBAL | people_3_person_nid | String | 51429 |
attribute | NC_GLOBAL | people_3_role | String | Co-Principal Investigator |
attribute | NC_GLOBAL | people_3_role_type | String | originator |
attribute | NC_GLOBAL | people_4_affiliation | String | Woods Hole Oceanographic Institution |
attribute | NC_GLOBAL | people_4_affiliation_acronym | String | WHOI |
attribute | NC_GLOBAL | people_4_person_name | String | Ann M. Tarrant |
attribute | NC_GLOBAL | people_4_person_nid | String | 51430 |
attribute | NC_GLOBAL | people_4_role | String | Co-Principal Investigator |
attribute | NC_GLOBAL | people_4_role_type | String | originator |
attribute | NC_GLOBAL | people_5_affiliation | String | Woods Hole Oceanographic Institution |
attribute | NC_GLOBAL | people_5_affiliation_acronym | String | WHOI |
attribute | NC_GLOBAL | people_5_person_name | String | Hannah Barkley |
attribute | NC_GLOBAL | people_5_person_nid | String | 560803 |
attribute | NC_GLOBAL | people_5_role | String | Contact |
attribute | NC_GLOBAL | people_5_role_type | String | related |
attribute | NC_GLOBAL | people_6_affiliation | String | Texas A&M University |
attribute | NC_GLOBAL | people_6_affiliation_acronym | String | TAMU |
attribute | NC_GLOBAL | people_6_person_name | String | Kathryn E.F. Shamberger |
attribute | NC_GLOBAL | people_6_person_nid | String | 488857 |
attribute | NC_GLOBAL | people_6_role | String | Contact |
attribute | NC_GLOBAL | people_6_role_type | String | related |
attribute | NC_GLOBAL | people_7_affiliation | String | Woods Hole Oceanographic Institution |
attribute | NC_GLOBAL | people_7_affiliation_acronym | String | WHOI BCO-DMO |
attribute | NC_GLOBAL | people_7_person_name | String | Shannon Rauch |
attribute | NC_GLOBAL | people_7_person_nid | String | 51498 |
attribute | NC_GLOBAL | people_7_role | String | BCO-DMO Data Manager |
attribute | NC_GLOBAL | people_7_role_type | String | related |
attribute | NC_GLOBAL | project | String | OA Nutrition and Coral Calcification,Coral Reef Ecosystem OA Impact,Thermal Thresholds and Projections |
attribute | NC_GLOBAL | projects_0_acronym | String | OA Nutrition and Coral Calcification |
attribute | NC_GLOBAL | projects_0_description | String | The project description is a modification of the original NSF award abstract.\nThis research project is part of the larger NSF funded CRI-OA collaborative research initiative and was funded as an Ocean Acidification-Category 1, 2010 award. Over the course of this century, all tropical coral reef ecosystems, whether fringing heavily populated coastlines or lining remote islands and atolls, face unprecedented threat from ocean acidification caused by rising levels of atmospheric CO2. In many laboratory experiments conducted to date, calcium carbonate production (calcification) by scleractinian (stony) corals showed an inverse correlation to seawater saturation state OMEGAar), whether OMEGAar was manipulated by acid or CO2 addition. Based on these data, it is predicted that coral calcification rates could decline by up to 80% of modern values by the end of this century. A growing body of new experimental data however, suggests that the coral calcification response to ocean acidification may be less straightforward and a lot more variable than previously recognized. In at least 10 recent experiments including our own, 8 different tropical and temperate species reared under nutritionally-replete but significantly elevated CO2 conditions (780-1200 ppm, OMEAGar ~1.5-2), continued to calcify at rates comparable to conspecifics reared under ambient CO2. These experimental results are consistent with initial field data collected on reefs in the eastern Pacific and southern Oman, where corals today live and accrete their skeletons under conditions equivalent to 2X and 3X pre-industrial CO2. On these high CO2, high nutrient reefs (where nitrate concentrations typically exceed 2.5 micro-molar), coral growth rates rival, and sometimes even exceed, those of conspecifics in low CO2, oligotrophic reef environments.\nThe investigators propose that a coral's energetic status, tightly coupled to the availability of inorganic nutrients and/or food, is a key factor in the calcification response to CO2-induced ocean acidification. Their hypothesis, if confirmed by the proposed laboratory investigations, implies that predicted changes in coastal and open ocean nutrient concentrations over the course of this century, driven by both climate impacts on ocean stratification and by increased human activity in coastal regions, could play a critical role in exacerbating and in some areas, modulating the coral reef response to ocean acidification. This research program builds on the investigators initial results and observations. The planned laboratory experiments will test the hypothesis that: (1) The coral calcification response to ocean acidification is linked to the energetic status of the coral host. The relative contribution of symbiont photosynthesis and heterotrophic feeding to a coral's energetic status varies amongst species. Enhancing the energetic status of corals reared under high CO2, either by stimulating photosynthesis with inorganic nutrients or by direct heterotrophic feeding of the host lowers the sensitivity of calcification to decreased seawater OMEGAar; (2) A species-specific threshold CO2 level exists over which enhanced energetic status can no longer compensate for decreased OMEGAar of the external seawater. Similarly, we will test the hypothesis that a nutrient threshold exists over which nutrients become detrimental for calcification even under high CO2 conditions; and (3) Temperature-induced reduction of algal symbionts is one stressor that can reduce the energetic reserve of the coral host and exacerbate the calcification response to ocean acidification.\nThe investigator's initial findings highlight the critical importance of energetic status in the coral calcification response to ocean acidification. Verification of these findings in the laboratory, and identification of nutrient and CO2 thresholds for a range of species will have immediate, direct impact on predictions of reef resilience in a high CO2 world. The research project brings together a diverse group of expertise in coral biogeochemistry, chemical oceanography, molecular biology and coral reproductive ecology to focus on a problem that has enormous societal, economic and conservation relevance. |
attribute | NC_GLOBAL | projects_0_end_date | String | 2013-09 |
attribute | NC_GLOBAL | projects_0_geolocation | String | global; experimental |
attribute | NC_GLOBAL | projects_0_name | String | An Investigation of the Role of Nutrition in the Coral Calcification Response to Ocean Acidification |
attribute | NC_GLOBAL | projects_0_project_nid | String | 2183 |
attribute | NC_GLOBAL | projects_0_start_date | String | 2010-10 |
attribute | NC_GLOBAL | projects_1_acronym | String | Coral Reef Ecosystem OA Impact |
attribute | NC_GLOBAL | projects_1_description | String | text copied from the NSF award abstract: \nMuch of our understanding of the impact of ocean acidification on coral reef calcification comes from laboratory manipulation experiments in which reef organisms are removed from their natural habitat and reared under conditions of calcium carbonate saturation (Omega) predicted for the tropical oceans at the end of this century. By comparison, there is a paucity of in situ data describing the sensitivity of coral reef ecosystems to changes in calcium carbonate saturation. Yet emerging evidence suggests there may be critical differences between the calcification response of organisms in culture and the net calcification response of a coral reef ecosystem, to the same degree of change in calcium carbonate saturation. In the majority of cases, the sensitivity of net reef calcification to changing calcium carbonate saturation is more severe than laboratory manipulation experiments predict. Clearly, accurate predictions of the response of coral reef ecosystems to 21st century ocean acidification will depend on a robust characterization of ecosystem-scale responses and an understanding of the fundamental processes that shape them. Using existing data, the investigators show that the sensitivity of coral reef ecosystem calcification to Delta calcium carbonate saturation conforms to the empirical rate equation R=k(Aragonite saturation state -1)n, which also describes the relationship between the rate of net abiogenic CaCO3 precipitation (R) and the degree of Aragonite supersaturation (Aragonite saturation state-1). By implication, the net ecosystem calcification (NEC) response to ocean acidification is governed by fundamental laws of physical chemistry and is potentially predictable across space and time. When viewed this way, the existing, albeit sparse, dataset of NEC reveals distinct patterns that, if verified, have important implications for how different coral reef ecosystems will respond to 21st century ocean acidification. The investigators have outlined a research program designed to build on this proposition. The project expands the currently sparse dataset of ecosystem-scale observations at four strategically placed reef sites: 2 sites in the Republic of Palau, Caroline Islands, Micronesia, western Pacific Ocean; a third at Dongsha Atoll, Pratas Islands, South China Sea; and the fourth at Kingman Reef, US Northern Line Islands, 6 deg. 23 N, 162 deg. 25 W. The four selected sites will allow investigators to test the following hypotheses: (1) The sensitivity (\"n\" in the rate equation) of coral reef ecosystem calcification to Delta Aragonite saturation state decreases with decreasing Aragonite saturation state. By implication, the rate at which reef calcification declines will slow as ocean acidification progresses over the course of this century. (2) The energetic status of the calcifying community is a key determinant of absolute rates of net ecosystem calcification (\"k\" in the rate equation), which, combined with n, defines the Aragonite saturation state value at which NEC approaches zero. By implication, the shift from net calcification to net dissolution will be delayed in healthy, energetically replete coral reef ecosystems and accelerated in perturbed, energetically depleted ecosystems. and (3) The calcification response of individual colonies of dominant reef calcifiers (corals and algae) is weaker than the measured ecosystem-scale response to the same change in Aragonite saturation state. By implication, processes not adequately captured in laboratory experiments, such as bioerosion and dissolution, will play an important role in the coral reef response to ocean acidification.\nBroader Impacts: Ocean acidification threatens the livelihoods of 500 million people worldwide who depend on coral reefs to provide habitable and agricultural land, food, building materials, coastal protection and income from tourism. Yet data emerging from ocean acidification (OA) studies point to critical gaps in our knowledge of reef ecosystem-scale responses to OA that currently limit our ability to predict the timing and severity of its impact on different reefs in different parts of the world. Using existing data generated by the investigators and others, this project will address a series of related hypotheses, which, if verified by the research, will have an immediate, direct impact on predictions of coral reef resilience in a high CO2 world. This project brings together expertise in coral reef biogeochemistry, chemical oceanography and physical oceanography to focus on a problem that has enormous societal, economic and conservation relevance. In addition to sharing the resultant data via BCO-DMO, project data will also be contributed to the Ocean Acidification International Coordination Centre (OA-ICC) data collection hosted at the PANGAEA Open Access library (http://www.pangaea.de). |
attribute | NC_GLOBAL | projects_1_end_date | String | 2015-08 |
attribute | NC_GLOBAL | projects_1_geolocation | String | Republic of Palau, Caroline Islands, Micronesia, western Pacific Ocean; Dongsha Atoll, Pratas Islands, South China Sea; Kingman Reef, US Northern Line Islands, 6 deg. 23 N, 162 deg. 25 W |
attribute | NC_GLOBAL | projects_1_name | String | Toward Predicting the Impact of Ocean Acidification on Net Calcification by a Broad Range of Coral Reef Ecosystems: Identifying Patterns and Underlying Causes |
attribute | NC_GLOBAL | projects_1_project_nid | String | 520413 |
attribute | NC_GLOBAL | projects_1_start_date | String | 2012-09 |
attribute | NC_GLOBAL | projects_2_acronym | String | Thermal Thresholds and Projections |
attribute | NC_GLOBAL | projects_2_description | String | Description from NSF award abstract:\nSea surface temperature (SST) across much of the global tropics has increased by 0.5-1 degrees C in the past 4 decades and, with it, the frequency and geographic extent of coral bleaching events and reef mortality. As levels of atmospheric CO2 continue to rise, there is mounting concern that CO2-induced climate change will pose the single greatest threat to the survival of coral reefs. Averaged output of 21 IPCC climate models for a mid-range CO2 emissions scenario predicts that tropical SSTs will increase another 1.5-3 degrees C by the end of this century. Combined with current estimates of thermal thresholds for coral bleaching, the outlook for the future of coral-reef ecosystems, worldwide, appears bleak. There are several key issues that limit accurate predictions of the full and lasting impact of rising SSTs. These include (1) level of confidence in the spatial and temporal patterns of the predicted warming, (2) knowledge of thermal thresholds of different reef-building coral species, and (3) the potential for corals to increase resistance to thermal stress through repeated exposure to high temperature events.\nNew skeletal markers have been developed that constrain the thermal thresholds and adaptive potential of multiple, individual coral colonies across 3-D space and through time. The method, based on 3-D CAT scan reconstructions of coral skeletons, has generated initial data from two coral species in the Red Sea, Great Barrier Reef and Phoenix Islands. Results showed that large, abrupt declines in skeletal growth occur at thresholds of accumulated heat stress defined by NOAA's Degree Heating Weeks Index (DHWs). In addition, there was a significant correlation between host lipid reserve, an independent measure of stress and mortality risk, and rates of skeletal growth. Because the coral skeleton archives the history of each coral's response to and recovery from successive, documented thermal anomalies, this approach pinpoints the thermal thresholds for sub-lethal impacts, the recovery time (if any) following a return to normal oceanographic conditions, and tests for a dampened response following successive events, indicative of acclimation.\nThis research program builds on initial work, focusing on method refinement and application to corals on two central Pacific reefs. With contrasting thermal histories, these reefs are considered at greatest risk from future ocean warming. In parallel, new experiments will be run on an ocean general-circulation model (OGCM) that is well suited to the tropical Pacific and of sufficiently high resolution, both horizontal and vertical, to maximize projections of thermal stress on specific central Pacific Reef sites over the next few decades. The OGCM output will also be of sufficient temporal resolution to compute DHWs, thus addressing a major limitation of the direct application of global climate model output (as archived for the IPCC AR4) toward coral-reef studies. Specifically, this study will: (1) collect multiple new, medium-length (15-30 yrs) cores and branches from two dominant reef-building species at 1-30m depth in the Gilbert and Jarvis Islands, central tropical Pacific; (2) apply 3-D CAT scanning and image analysis techniques to quantify systematically thermal thresholds, rates of recovery and resilience for each species, at each reef site and with depth; (3) quantify energetic reserve and symbiont genotype amongst thermally more- and less- resilient colonies, establishing a quantitative link between calcification stress and mortality risk, and determining the physiological basis for calcification responses to thermal stress; (4) use an OGCM specifically tailored to the tropical Pacific to produce a dynamically consistent set of forecasts for near-term climate change at the target reef sites; and (5) combine coral data with model output and refine the projected thermal stress forecast, in degree heating weeks, for corals in this central Pacific Island group over the 21st century. |
attribute | NC_GLOBAL | projects_2_end_date | String | 2014-09 |
attribute | NC_GLOBAL | projects_2_name | String | Constraining Thermal Thresholds and Projections of Temperature Stress on Pacific Coral Reefs Over the 21st Century: Method Refinement and Application |
attribute | NC_GLOBAL | projects_2_project_nid | String | 560428 |
attribute | NC_GLOBAL | projects_2_start_date | String | 2010-10 |
attribute | NC_GLOBAL | publisher_name | String | Biological and Chemical Oceanographic Data Management Office (BCO-DMO) |
attribute | NC_GLOBAL | publisher_type | String | institution |
attribute | NC_GLOBAL | sourceUrl | String | (local files) |
attribute | NC_GLOBAL | Southernmost_Northing | double | 7.158 |
attribute | NC_GLOBAL | standard_name_vocabulary | String | CF Standard Name Table v55 |
attribute | NC_GLOBAL | summary | String | Seawater carbonate chemistry from 13 sites in Palau collected from small boats in the Palauan archipelago from 2011-2013. |
attribute | NC_GLOBAL | title | String | [Palau carbonate chemistry] - Seawater carbonate chemistry from 13 sites in Palau collected from small boats in the Palauan archipelago from 2011-2013 (An Investigation of the Role of Nutrition in the Coral Calcification Response to Ocean Acidification) |
attribute | NC_GLOBAL | version | String | 1 |
attribute | NC_GLOBAL | Westernmost_Easting | double | 134.349 |
attribute | NC_GLOBAL | xml_source | String | osprey2erddap.update_xml() v1.3 |
variable | site_name | String | ||
attribute | site_name | bcodmo_name | String | Site_Desig |
attribute | site_name | description | String | Name of the site. |
attribute | site_name | long_name | String | Site Name |
attribute | site_name | units | String | dimensionless |
variable | latitude | double | ||
attribute | latitude | _CoordinateAxisType | String | Lat |
attribute | latitude | _FillValue | double | NaN |
attribute | latitude | actual_range | double | 7.158, 7.577 |
attribute | latitude | axis | String | Y |
attribute | latitude | bcodmo_name | String | latitude |
attribute | latitude | colorBarMaximum | double | 90.0 |
attribute | latitude | colorBarMinimum | double | -90.0 |
attribute | latitude | description | String | Latitude of the sampling location. |
attribute | latitude | ioos_category | String | Location |
attribute | latitude | long_name | String | Latitude |
attribute | latitude | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P09/current/LATX/ |
attribute | latitude | standard_name | String | latitude |
attribute | latitude | units | String | degrees_north |
variable | longitude | double | ||
attribute | longitude | _CoordinateAxisType | String | Lon |
attribute | longitude | _FillValue | double | NaN |
attribute | longitude | actual_range | double | 134.349, 134.557 |
attribute | longitude | axis | String | X |
attribute | longitude | bcodmo_name | String | longitude |
attribute | longitude | colorBarMaximum | double | 180.0 |
attribute | longitude | colorBarMinimum | double | -180.0 |
attribute | longitude | description | String | Longitude of the sampling location. |
attribute | longitude | ioos_category | String | Location |
attribute | longitude | long_name | String | Longitude |
attribute | longitude | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P09/current/LONX/ |
attribute | longitude | standard_name | String | longitude |
attribute | longitude | units | String | degrees_east |
variable | date | int | ||
attribute | date | _FillValue | int | 2147483647 |
attribute | date | actual_range | int | 20110919, 20131112 |
attribute | date | bcodmo_name | String | date_local |
attribute | date | description | String | Date (as year-month-day); in local time zone. in YYYYmmdd format. |
attribute | date | long_name | String | Date |
attribute | date | units | String | unitless |
variable | time2 | String | ||
attribute | time2 | bcodmo_name | String | time_local |
attribute | time2 | description | String | Time (hours and minutes); 24-hour clock; local time zone. |
attribute | time2 | long_name | String | Time |
attribute | time2 | units | String | HHMM |
variable | TA | float | ||
attribute | TA | _FillValue | float | NaN |
attribute | TA | actual_range | float | 1858.702, 2245.173 |
attribute | TA | bcodmo_name | String | TALK |
attribute | TA | description | String | Total alkalinity. |
attribute | TA | long_name | String | TA |
attribute | TA | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/MDMAP014/ |
attribute | TA | units | String | micromoles per kilogram (umol/kg) |
variable | DIC | float | ||
attribute | DIC | _FillValue | float | NaN |
attribute | DIC | actual_range | float | 1705.471, 1947.879 |
attribute | DIC | bcodmo_name | String | DIC |
attribute | DIC | description | String | Dissolved inorganic carbon. |
attribute | DIC | long_name | String | DIC |
attribute | DIC | units | String | micromoles per kilogram (umol/kg) |
variable | sal | float | ||
attribute | sal | _FillValue | float | NaN |
attribute | sal | actual_range | float | 30.022, 34.137 |
attribute | sal | bcodmo_name | String | sal |
attribute | sal | description | String | Salinity. |
attribute | sal | long_name | String | Sal |
attribute | sal | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/PSALST01/ |
attribute | sal | units | String | dimensionless |
variable | temp | float | ||
attribute | temp | _FillValue | float | NaN |
attribute | temp | actual_range | float | 26.842, 32.092 |
attribute | temp | bcodmo_name | String | temperature |
attribute | temp | description | String | Water temperature. |
attribute | temp | long_name | String | Temperature |
attribute | temp | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/TEMPP901/ |
attribute | temp | units | String | degrees Celsius ( C) |
variable | pH | float | ||
attribute | pH | _FillValue | float | NaN |
attribute | pH | actual_range | float | 7.78, 8.164 |
attribute | pH | bcodmo_name | String | pH |
attribute | pH | colorBarMaximum | double | 9.0 |
attribute | pH | colorBarMinimum | double | 7.0 |
attribute | pH | description | String | pH. |
attribute | pH | long_name | String | Sea Water Ph Reported On Total Scale |
attribute | pH | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/PHXXZZXX/ |
attribute | pH | units | String | dimensionless |
variable | pCO2 | float | ||
attribute | pCO2 | _FillValue | float | NaN |
attribute | pCO2 | actual_range | float | 264.613, 717.26 |
attribute | pCO2 | bcodmo_name | String | pCO2 |
attribute | pCO2 | description | String | Partial pressure of carbon dioxide. |
attribute | pCO2 | long_name | String | P CO2 |
attribute | pCO2 | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/PCO2C101/ |
attribute | pCO2 | units | String | micro-atmospheres (uatm) |
variable | CO2_diss | float | ||
attribute | CO2_diss | _FillValue | float | NaN |
attribute | CO2_diss | actual_range | float | 6.842, 18.124 |
attribute | CO2_diss | bcodmo_name | String | unknown |
attribute | CO2_diss | description | String | Dissolved carbon dioxide (CO2). |
attribute | CO2_diss | long_name | String | CO2 Diss |
attribute | CO2_diss | units | String | micromoles per kilogram (umol/kg) |
variable | bicarbonate | float | ||
attribute | bicarbonate | _FillValue | float | NaN |
attribute | bicarbonate | actual_range | float | 1470.431, 1758.909 |
attribute | bicarbonate | bcodmo_name | String | bicarbonate |
attribute | bicarbonate | description | String | Bicarbonate ion (HCO3-) concentration. |
attribute | bicarbonate | long_name | String | Bicarbonate |
attribute | bicarbonate | units | String | micromoles per kilogram (umol/kg) |
variable | carbonate | float | ||
attribute | carbonate | _FillValue | float | NaN |
attribute | carbonate | actual_range | float | 112.525, 267.699 |
attribute | carbonate | bcodmo_name | String | carbonate |
attribute | carbonate | description | String | Carbonate ion (CO3-) concentration. |
attribute | carbonate | long_name | String | Carbonate |
attribute | carbonate | units | String | micromoles per kilogram (umol/kg) |
variable | omega_Ca | float | ||
attribute | omega_Ca | _FillValue | float | NaN |
attribute | omega_Ca | actual_range | float | 2.836, 6.553 |
attribute | omega_Ca | bcodmo_name | String | Calcite Saturation State |
attribute | omega_Ca | description | String | The saturation state of seawater with respect to calcite. |
attribute | omega_Ca | long_name | String | Omega Ca |
attribute | omega_Ca | units | String | dimensionless |
variable | omega_Ar | float | ||
attribute | omega_Ar | _FillValue | float | NaN |
attribute | omega_Ar | actual_range | float | 1.86, 4.365 |
attribute | omega_Ar | bcodmo_name | String | OM_ar |
attribute | omega_Ar | description | String | The saturation state of seawater with respect to aragonite. |
attribute | omega_Ar | long_name | String | Omega Ar |
attribute | omega_Ar | units | String | dimensionless |
variable | NH4 | float | ||
attribute | NH4 | _FillValue | float | NaN |
attribute | NH4 | actual_range | float | 0.015, 1.884 |
attribute | NH4 | bcodmo_name | String | Ammonium |
attribute | NH4 | colorBarMaximum | double | 5.0 |
attribute | NH4 | colorBarMinimum | double | 0.0 |
attribute | NH4 | description | String | Ammonium (NH4+) concentration. |
attribute | NH4 | long_name | String | Mole Concentration Of Ammonium In Sea Water |
attribute | NH4 | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/AMONAAZX/ |
attribute | NH4 | units | String | micromolar (uM) |
variable | PO4 | float | ||
attribute | PO4 | _FillValue | float | NaN |
attribute | PO4 | actual_range | float | 0.009, 5.689 |
attribute | PO4 | bcodmo_name | String | PO4 |
attribute | PO4 | description | String | Phosphate (PO4---) concentration. |
attribute | PO4 | long_name | String | Mass Concentration Of Phosphate In Sea Water |
attribute | PO4 | units | String | micromolar (uM) |
variable | NO3_NO2 | float | ||
attribute | NO3_NO2 | _FillValue | float | NaN |
attribute | NO3_NO2 | actual_range | float | 0.015, 1.878 |
attribute | NO3_NO2 | bcodmo_name | String | NO3_NO2 |
attribute | NO3_NO2 | colorBarMaximum | double | 50.0 |
attribute | NO3_NO2 | colorBarMinimum | double | 0.0 |
attribute | NO3_NO2 | description | String | Nitrate/nitrite (NO3-/NO2-) concentration. |
attribute | NO3_NO2 | long_name | String | Mole Concentration Of Nitrate In Sea Water |
attribute | NO3_NO2 | units | String | micromolar (uM) |