http://lod.bco-dmo.org/id/dataset/528806
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
2014-09-25
ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data
ISO 19115-2:2009(E)
Seawater carbonate chemistry for brooded coral larval experiments, Taiwan, March 2011 and 2012 (Cumbo, 2013)(MCR LTER project, Climate_Coral_Larvae project)
2014-08-30
publication
2014-08-30
revision
BCO-DMO Linked Data URI
2014-08-30
creation
http://lod.bco-dmo.org/id/dataset/528806
Peter J. Edmunds
California State University Northridge
principalInvestigator
Dr Vivian R Cumbo
California State University Northridge
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: Edmunds, P. J., Cumbo, V. R. (2014) Seawater carbonate chemistry for brooded coral larval experiments, Taiwan, March 2011 and 2012 (Cumbo, 2013)(MCR LTER project, Climate_Coral_Larvae project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 2014-08-30) Version Date 2014-08-30 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/528806 [access date]
Seawater carbonate chemistry for brooded coral larval experiments, March 2011 & 2012 (Cumbo, 2013) Dataset Description: <p>To evaluate the effects of temperature and pCO2 on coral larvae, brooded larvae of Pocillopora damicornis from Nanwan Bay, Taiwan (21°56.179' N, 120°44.85' E), were exposed to ambient (419-470 µatm) and high (604-742 µatm) pCO2 at ~25 and ~29 °C in two experiments conducted in March 2010 and March 2012. Larvae were sampled from four consecutive lunar days (LD) synchronized with spawning following the new moon, incubated in treatments for 24 h, and measured for respiration, maximum photochemical efficiency of PSII (F v/F m), and mortality.</p>
<p>The most striking outcome was a strong effect of time (i.e., LD) on larvae performance: respiration was affected by an LD × temperature interaction in 2010 and 2012, as well as an LD × pCO2 × temperature interaction in 2012; F v/F m was affected by LD in 2010 (but not 2012); and mortality was affected by an LD × pCO2 interaction in 2010, and an LD × temperature interaction in 2012. There were no main effects of pCO2 in 2010, but in 2012, high pCO2 depressed metabolic rate and reduced mortality. Therefore, differences in larval performance depended on day of release and resulted in varying susceptibility to future predicted environmental conditions. These results underscore the importance of considering larval brood variation across days when designing experiments. Subtle differences in experimental outcomes between years suggest that transgenerational plasticity in combination with unique histories of exposure to physical conditions can modulate the response of brooded coral larvae to climate change and ocean acidification.</p>
<p>These data include the seawater carbonate chemistry monitored from the experimental tanks, March 2011 and 2012.</p>
<p><strong>Related datasets:</strong></p>
<p><a href="http://www.bco-dmo.org/dataset/528880">brooded coral larvae 2 - larval release March 2003-2008</a><br />
<a href="http://www.bco-dmo.org/dataset/528834">brooded coral larvae 2 - respiration_photosyth_mortality</a></p>
<p>These data are published in Vivian R Cumbo, Peter J Edmunds, Christopher B Wall, Tung-Yung Fan. (2013) Brooded coral larvae differ in their response to high temperature and elevated pCO2 depending on the day of release. Marine Biology. See Table 1.</p>
<p><a href="http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Cumbo_etal_2013_MarBio_BCODMO.xlsx" target="_blank">Download complete data for this publication (Excel file)</a><br />
Data also available from PANGAEA: <a href="http://doi.pangaea.de/10.1594/PANGAEA.831612" target="_blank">DOI 10.1007/s00227-013-2280-y</a></p> Methods and Sampling: <p>To determine the dissolved inorganic carbon (DIC) chemistry of seawater in the treatments, total alkalinity (TA), pH on the total scale, temperature, and salinity were measured using standard procedures, and used to calculate pCO2 (uatm), HCO3 - (umolkg-1), CO3 2- (umolkg-1), and the aragonite saturation state (XArag) of seawater using CO2SYS (Pierrot et al. 2006). TA (umol kg-1) was measured through potentiometric titration (SOP 3b, Dickson et al. 2007) using an automatic titrator (DL50, Mettler Toledo) filled with certified acid titrant (0.1 M HCl, 0.6 NaCl, Dickson Laboratory, Scripps Institution of Oceanography). The pH probe (DG101-SC, Mettler Toledo) attached to the titrator was 3-point calibrated with pH 4.00, 7.00, and 10.00 buffers (Fisher, NBS). Certified reference material with a known TA (Batch 98, http://andrew.ucsd. edu/index.html) was titrated daily to determine the accuracy and precision of the analyses.&nbsp;</p>
<p>Seawater samples (50 mL) from the treatment tanks were brought to 25C, weighed and titrated in a waterjacketed beaker within 2-3 h of collection. The pH values and the titrant volumes (cm3) obtained from the titrations were sub-sampled for the range between pH 3.0 and 3.5 and inserted into a Microsoft Excel spreadsheet (Fangue et al. 2010), which calculated Gran’s function as a product of the mass of titrant added (Dickson et al. 2007). Treatment tank pH was determined spectrophotometrically using m-cresol purple dye (Sigma-Aldrich) following SOP 6b of Dickson et al. (2007) with modification (Fangue et al. 2010). Preliminary sampling of the seawater in the tanks throughout the day confirmed that the pCO2 treatments were stable over a 24-h period.</p>
<p><strong>References:</strong></p>
<p>Dickson AG, Sabine CL, Christian JR (eds) (2007) Guide to best practices for ocean CO2 measurements. PICES Special Publication 3, p 191</p>
<p>Fangue NA, O’Donnell MJ, Sewell MA, Matson PG, MacPherson AC, Hoffman GE (2010) A laboratory-based, experimental system for the study of ocean acidification effects on marine invertebrate larvae. Limnol Oceanogr Methods 8:441-452</p>
Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-0844785 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=0844785
completed
Peter J. Edmunds
California State University Northridge
818-677-2502
Department of Biology 18111 Nordhoff Street
Northridge
CA
91330-8303
USA
peter.edmunds@csun.edu
pointOfContact
Dr Vivian R Cumbo
California State University Northridge
Dept. of Biology 18111 Nordhoff Street
Northridge,
CA
91330-8303
pointOfContact
asNeeded
Dataset Version: 2014-08-30
Unknown
expt
lab
lat
lon
month
tank
date
pH
temp
sal
TA
pCO2
bicarbonate
carbonate
omega_Ara
Automatic titrator
theme
None, User defined
experiment id
laboratory
latitude
longitude
month of year
tank
date
pH
water temperature at measurement depth
salinity
total alkalinity (TA)
Partial pressure of CO2
bicarbonate concentration [HCO3]-
Carbonate concentration [CO3]2-
Aragonite Saturation State
featureType
BCO-DMO Standard Parameters
Titrator
instrument
BCO-DMO Standard Instruments
lab_Edmunds_NMMBA
service
Deployment Activity
National Museum of Marine Biology and Aquarium, Taiwan
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.
Long Term Ecological Research network
http://www.lternet.edu/
Long Term Ecological Research network
adapted from http://www.lternet.edu/
The National Science Foundation established the LTER program in 1980 to support research on long-term ecological phenomena in the United States. The Long Term Ecological Research (LTER) Network is a collaborative effort involving more than 1800 scientists and students investigating ecological processes over long temporal and broad spatial scales. The LTER Network promotes synthesis and comparative research across sites and ecosystems and among other related national and international research programs. The LTER research sites represent diverse ecosystems with emphasis on different research themes, and cross-site communication, network publications, and research-planning activities are coordinated through the LTER Network Office.
2017 LTER research site map obtained from https://lternet.edu/site/lter-network/
LTER
largerWorkCitation
program
Moorea Coral Reef Long-Term Ecological Research site
http://mcr.lternet.edu/
Moorea Coral Reef Long-Term Ecological Research site
<p><strong>NSF Award Abstract: </strong></p>
<p>Coral reefs provide important benefits to society, from food to exceptional biodiversity to shoreline protection and recreation, but they are threatened by natural perturbations and human activities, including those causing global-scale changes. These pressures increasingly are causing coral reefs to undergo large, often abrupt, ecological changes where corals are being replaced by seaweeds or other undesirable organisms. Historically, the major agent of disturbance to coral reefs has been powerful storms, but in recent decades, episodes of mass coral bleaching from marine heat waves have become more frequent and severe as the temperature of ocean surface waters continues to rise. Coral reefs are further stressed by local human activities that cause nutrient pollution and deplete herbivorous fishes that control growth of seaweeds. Studying how coral reefs respond to these two types of disturbance under different levels of nutrient pollution and fishing provides essential information on what affects the ability of coral reefs to buffer environmental change and disturbances without collapsing to a persistent, degraded condition. The fundamental goals of the Moorea Coral Reef Long Term Ecological Research program (MCR LTER) are to understand how and why coral reefs change over time, to assess the consequences of these changes, and to contribute scientific knowledge needed to sustain coral reef ecosystems and the important societal services they provide. This research improves understanding and management of coral reefs, which benefits all groups concerned with the welfare of this ecologically, economically and culturally important ecosystem. In addition to academic communities, scientific findings are communicated to interested individuals, non-governmental organizations, island communities and governmental entities. These findings also are integrated into K-12, undergraduate, graduate and public education activities through a multi-pronged program that includes inquiry-based curricula, interactive and media-based public education programs, and internet-based resources. MCR?s research, training, education and outreach efforts all emphasize broadening participation in STEM fields and strengthening STEM literacy.</p>
<p>New research activities build on MCR LTER?s powerful foundation of long-term observations and broad ecological understanding of oceanic coral reefs to address the following core issues: How is the changing disturbance regime (recurrent heat waves in addition to cyclonic storms) altering the resilience of coral reefs, and what are the ecological consequences of altered resilience? Research activities are organized around a unifying framework that explicitly addresses how reef communities are affected by the nature and history of coral-killing disturbances, and how those responses to disturbance are influenced by the pattern of local human stressors. New studies answer three focal questions: (1) How do different disturbance types, which either remove (storms) or retain (heat waves) dead coral skeletons, affect community dynamics, abrupt changes in ecological state, and resilience? (2) How do local stressors interact with new disturbance regimes to create spatial heterogeneity in community dynamics, ecosystem processes, and spatial resilience? And (3) What attributes of coral and coral reef communities influence their capacity to remain resilient under current and future environmental conditions? These questions provide an unparalleled opportunity to test hypotheses and advance theory regarding ecological resilience and the causes and consequences of abrupt ecological change, which is broadly relevant across aquatic and terrestrial ecosystems.</p>
<p>This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.</p>
<p><strong>From <a href="http://www.lternet.edu/sites/mcr/">http://www.lternet.edu/sites/mcr/</a> and <a href="http://mcr.lternet.edu/">http://mcr.lternet.edu/</a></strong>:<br />
The Moorea Coral Reef LTER site encompasses the coral reef complex that surrounds the island of Moorea, French Polynesia (17°30'S, 149°50'W). Moorea is a small, triangular volcanic island 20 km west of Tahiti in the Society Islands of French Polynesia. An offshore barrier reef forms a system of shallow (mean depth ~ 5-7 m), narrow (~0.8-1.5 km wide) lagoons around the 60 km perimeter of Moorea. All major coral reef types (e.g., fringing reef, lagoon patch reefs, back reef, barrier reef and fore reef) are present and accessible by small boat.</p>
<p>The MCR LTER was established in 2004 by the US National Science Foundation (NSF) and is a partnership between the University of California Santa Barbara and California State University, Northridge. MCR researchers include marine scientists from the UC Santa Barbara, CSU Northridge, UC Davis, UC Santa Cruz, UC San Diego, CSU San Marcos, Duke University and the University of Hawaii. Field operations are conducted from the UC Berkeley Richard B. Gump South Pacific Research Station on the island of Moorea, French Polynesia.</p>
<p><strong>MCR LTER Data:</strong> The Moorea Coral Reef (MCR) LTER data are managed by and available directly from the MCR project data site URL shown above. The datasets listed below were collected at or near the MCR LTER sampling locations, and funded by NSF OCE as ancillary projects related to the MCR LTER core research themes.</p>
<p><strong>This project is supported by continuing grants with slight name variations:</strong></p>
<ul>
<li>LTER: Long-Term Dynamics of a Coral Reef Ecosystem</li>
<li>LTER: MCR II - Long-Term Dynamics of a Coral Reef Ecosystem</li>
<li>LTER: MCR IIB: Long-Term Dynamics of a Coral Reef Ecosystem</li>
<li>LTER: MCR III: Long-Term Dynamics of a Coral Reef Ecosystem</li>
<li>LTER: MCR IV: Long-Term Dynamics of a Coral Reef Ecosystem</li>
</ul>
MCR LTER
largerWorkCitation
project
The ecophysiological basis of the response of coral larvae and early life history stages to global climate change
https://osprey.bco-dmo.org/project/2235
The ecophysiological basis of the response of coral larvae and early life history stages to global climate change
<p><span style="font-size:13px">Tropical coral reefs face a suite of environmental assaults ranging from anchor damage to the effects of global climate change (GCC). The consequences are evident throughout the tropics, where many coral reefs have lost a substantial fraction of their coral cover in a few decades. Notwithstanding the importance of reducing the impacts of environmental stresses, the only means by which these ecosystems can recover (or simply persist) is through the recruitment of scleractinians, which is a function of successful larval development, delivery, settlement, metamorphosis, and post-settlement events. Despite wide recognition of the importance of these processes, there are few pertinent empirical data, and virtually none that address the mechanisms mediating the success of early coral life stages in a physical environmental varying at multiple spatio-temporal scales.</span></p>
<p>The objective of this research is to complete one of the first comprehensive ecophysiological analyses of the early life stages of corals through a description of: (1) their functionality under 'normal' conditions, and (2) their response to the main drivers of GCC. These analyses will be completed for 2 species representative of a brooding life history strategy, and the experiments will be completed in two locations, one (Taiwan) that provides unrivalled experience in coral reproductive biology, and superb microcosm facilities, and the other (Moorea), with access to a relatively pristine environment, a well described ecological and oceanographic context (through the MCR-LTER), and the capacity to bring a strong biogeographic contrast to the project. The results of the study will be integrated through modeling to explore the effects of GCC on coral community structure over the next century.</p>
<p><strong>The following publications and data resulted from this project:</strong></p>
<p>2013 Wall CB, Fan TY, Edmunds PJ. Ocean acidification has no effect on thermal bleaching in the coral <em>Seriatopora caliendrum</em>. Coral Reefs 33: 119-130.<br />
<a href="http://www.bco-dmo.org/dataset/522591" target="_blank">Symbiodinium_Seriatopora photosynthesis</a><br />
<a href="http://www.bco-dmo.org/dataset/522737" target="_blank">Symbiodinium_Seriatopora PI curve</a><br />
<a href="http://www.bco-dmo.org/dataset/522697" target="_blank">Symbiodinium_Seriatopora temp-salinity-light</a><br />
<a href="http://www.bco-dmo.org/dataset/522631" target="_blank">Symbiodinium_Seriatopora water chemistry</a><br />
<a href="http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Wall_Fan_Edmunds_for_Taiwan_Bleaching_data2013_BCODMO.xlsx" target="_blank">- Download complete data for this publication (Excel file)</a></p>
<p>2013 Wall CB, Edmunds PJ. <em>In situ </em>effects of low pH and elevated HCO3- on juvenile <em>Porites</em> spp. in Moorea, French Polynesia. Biological Bulletin 225:92-101.<br />
Data at <a href="http://mcr.lternet.edu/" target="_blank">MCR</a> and PANGEA: <a href="http://doi.pangaea.de/10.1594/PANGAEA.833913" target="_blank">doi.pangaea.de/10.1594/PANGAEA.833913</a><br />
<a href="http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Wall_Edmunds_2013_BioBull_BCODMO.xlsx" target="_blank">- Download complete data for this publication (Excel file)</a></p>
<p>2013 Vivian R Cumbo, Peter J Edmunds, Christopher B Wall, Tung-Yung Fan. Brooded coral larvae differ in their response to high temperature and elevated pCO2 depending on the day of release. Marine Biology DOI 10.1007/s00227-013-2280-y.<br />
Data also at PANGEA: <a href="http://doi.pangaea.de/10.1594/PANGAEA.831612" target="_blank">doi.pangaea.de/10.1594/PANGAEA.831612</a><br />
<a href="http://www.bco-dmo.org/dataset/528806">brooded coral larvae 2 - carbonate chemistry</a><br />
<a href="http://www.bco-dmo.org/dataset/528880">brooded coral larvae 2 - larval release March 2003-2008</a><br />
<a href="http://www.bco-dmo.org/dataset/528834">brooded coral larvae 2 - respiration_photosyth_mortality</a><br />
<a href="http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Cumbo_etal_2013_MarBio_BCODMO.xlsx" target="_blank">- Download complete data for this publication (Excel file)</a></p>
<p>2013 Edmunds PJ, Cumbo VR, Fan TY. Metabolic costs of larval settlement and metamorphosis in the coral <em>Seriatopora caliendrum</em> under ambient and elevated pCO2. Journal Experimental Marine Biology and Ecology 443: 33-38 Data also at PANGEA: <a href="http://doi.pangaea.de/10.1594/PANGAEA.821644" target="_blank">doi:10.1594/PANGAEA.821644</a><br />
<a href="http://www.bco-dmo.org/dataset/526674" target="_blank">Coral post-settlement physiology</a><br />
<a href="http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Edmunds_etal_2013_JEMBE443_BCODMO.xls" target="_blank">- Download complete data for this publication (Excel file)</a></p>
<p>2013 Aaron M Dufault, Aaron Ninokawa, Lorenzo Bramanti, Vivian R Cumbo, Tung-Yung Fan, Peter J Edmunds. The role of light in mediating the effects of ocean acidification on coral calcification. Journal of Experimental Biology 216: 1570-1577.<br />
<a href="http://www.bco-dmo.org/dataset/527500">coral-light expt.- PAR</a><br />
<a href="http://www.bco-dmo.org/dataset/527752">coral-light expt.- carbonate chemistry</a><br />
<a href="http://www.bco-dmo.org/dataset/527729">coral-light expt.- temp_salinity</a><br />
<a href="http://www.bco-dmo.org/dataset/527816">coral-light expt.- growth</a><br />
<a href="http://www.bco-dmo.org/dataset/527782">coral-light expt.- protein</a><br />
<a href="http://www.bco-dmo.org/dataset/527851">coral-light expt.- survival</a><br />
<a href="http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Dufault_etal_2013_JEB_BCODMO.xlsx" target="_blank">- Download complete data for this publication (Excel file)</a></p>
<p>2012 Cumbo, VR, Fan TY, Edmunds PJ. Effects of exposure duration on the response of <em>Pocillopora damicornis</em> larvae to elevated temperature and high pCO2. J Exp Mar Biol Ecol 439: 100-107.<br />
Data is also at PANGEA: <a href="http://doi.pangaea.de/10.1594/PANGAEA.823582" target="_blank">doi:10.1594/PANGAEA.823582</a><br />
<a href="http://www.bco-dmo.org/dataset/535163">brooded coral larvae 3 - carbonate chemistry</a><br />
<a href="http://www.bco-dmo.org/dataset/535219">brooded coral larvae 3 - light</a><br />
<a href="http://www.bco-dmo.org/dataset/535462">brooded coral larvae 3 - mortality</a><br />
<a href="http://www.bco-dmo.org/dataset/535425">brooded coral larvae 3 - protein</a><br />
<a href="http://www.bco-dmo.org/dataset/535328">brooded coral larvae 3 - respiration and protein</a><br />
<a href="http://www.bco-dmo.org/dataset/535266">brooded coral larvae 3 - respiration raw data</a><br />
<a href="http://www.bco-dmo.org/dataset/535358">brooded coral larvae 3 - symbiont density</a><br />
<a href="http://www.bco-dmo.org/dataset/535244">brooded coral larvae 3 - tank temperature</a><br />
<a href="http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Cumbo_etal_2012_JEMBE_data1_BCODMO.xls" target="_blank">- Download part 1 of data for this publication (Excel file)</a><br />
<a href="http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Cumbo_etal_2012_JEMBE_Tank Parameters_BCODMO.xlsx" target="_blank">- Download tank parameters data for this publication (Excel file)</a></p>
<p>2012 Cumbo, VR, Fan TY, Edmunds PJ. Physiological development of brooded larvae from two pocilloporid corals in Taiwan. Marine Biology 159: 2853-2866.<br />
<a href="http://www.bco-dmo.org/dataset/528781">brooded coral - carbonate chemistry</a><br />
<a href="http://www.bco-dmo.org/dataset/528641">brooded coral - release</a><br />
<a href="http://www.bco-dmo.org/dataset/528695">brooded coral - respiration</a><br />
<a href="http://www.bco-dmo.org/dataset/528728">brooded coral - settlement competency</a><br />
<a href="http://www.bco-dmo.org/dataset/528761">brooded coral - size_July</a><br />
<a href="http://www.bco-dmo.org/dataset/528661">brooded coral - size_protein_symbionts_photosynth</a><br />
<a href="http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Cumbo_etal_2012_MarBio_BCODMO .xlsx" target="_blank">- Download complete data for this publication (Excel file)</a></p>
<p>2012 Dufault, Aaron M; Vivian R Cumbo; Tung-Yung Fan; Peter J Edmunds. Effects of diurnally oscillating pCO2 on the calcification and survival of coral recruits. Royal Society of London (B) 279: 2951-2958. doi:10.1098/rspb.2011.2545<br />
Data is also at PANGEA: <a href="http://doi.pangaea.de/10.1594/PANGAEA.830185" target="_blank">doi:10.1594/PANGAEA.830185</a><br />
<a href="http://www.bco-dmo.org/dataset/514198" target="_blank">recruit_growth_area</a><br />
<a href="http://www.bco-dmo.org/dataset/506245" target="_blank">recruit_growth_weight</a><br />
<a href="http://www.bco-dmo.org/dataset/516783" target="_blank">recruit_seawater_chemistry</a><br />
<a href="http://www.bco-dmo.org/dataset/516529" target="_blank">recruit_survival</a><br />
<a href="http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Dufault_etal_2012_RoyProcB_BCODMO.xlsx" target="_blank">- Download complete data for this publication (Excel file)</a></p>
<p>2011 Edmunds PJ, Cumbo V, Fan TY. Effects of temperature on the respiration of brooded larvae from tropical reef corals. Journal of Experimental Biology 214: 2783-2790. <br />
<a href="http://www.bco-dmo.org/dataset/3790" target="_blank">CoralLarvae_comparison_respir</a><br />
<a href="http://www.bco-dmo.org/dataset/3809" target="_blank">CoralLarvae_release</a><br />
<a href="http://www.bco-dmo.org/dataset/3802" target="_blank">CoralLarvae_respir</a><br />
<a href="http://www.bco-dmo.org/dataset/3795" target="_blank">CoralLarvae_size</a><br />
<a href="http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Edmunds_etal_2011_JEB_BCODMO.xls" target="_blank">- Download complete data for this publication (Excel file)</a></p>
Climate_Coral_Larvae
largerWorkCitation
project
eng; USA
oceans
National Museum of Marine Biology and Aquarium, Taiwan
2014-08-30
From projects that focused on the following 2 locations: 1. Island of Moorea, French Polynesia 2. Moorea, French Polynesia; Southern Taiwan; California State University Northridge
0
BCO-DMO catalogue of parameters from Seawater carbonate chemistry for brooded coral larval experiments, Taiwan, March 2011 and 2012 (Cumbo, 2013)(MCR LTER project, Climate_Coral_Larvae 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
http://lod.bco-dmo.org/id/dataset-parameter/528819.rdf
Name: expt
Units: unitless
Description: <p>experiment id</p>
http://lod.bco-dmo.org/id/dataset-parameter/528820.rdf
Name: lab
Units: unitless
Description: <p>laboratory</p>
http://lod.bco-dmo.org/id/dataset-parameter/528821.rdf
Name: lat
Units: decimal degrees
Description: <p>latitude; north is positive</p>
http://lod.bco-dmo.org/id/dataset-parameter/528822.rdf
Name: lon
Units: decimal degrees
Description: <p>longitude; east is positive</p>
http://lod.bco-dmo.org/id/dataset-parameter/528823.rdf
Name: month
Units: unitless
Description: <p>experiment month</p>
http://lod.bco-dmo.org/id/dataset-parameter/528824.rdf
Name: tank
Units: tank
Description: <p>tank id number</p>
http://lod.bco-dmo.org/id/dataset-parameter/528825.rdf
Name: date
Units: yyyy-mm-dd
Description: <p>local date of measurement</p>
http://lod.bco-dmo.org/id/dataset-parameter/528826.rdf
Name: pH
Units: pH scale
Description: <p>pH: The measure of the acidity or basicity of an aqueous solution</p>
http://lod.bco-dmo.org/id/dataset-parameter/528827.rdf
Name: temp
Units: degees Celsius
Description: <p>temperature</p>
http://lod.bco-dmo.org/id/dataset-parameter/528828.rdf
Name: sal
Units: PSU scale
Description: <p>salinity</p>
http://lod.bco-dmo.org/id/dataset-parameter/528829.rdf
Name: TA
Units: umol/kg
Description: <p>total alkalinity</p>
http://lod.bco-dmo.org/id/dataset-parameter/528830.rdf
Name: pCO2
Units: uatm
Description: <p>partial pressure of carbon dioxide by computation from pH and alkalinity</p>
http://lod.bco-dmo.org/id/dataset-parameter/528831.rdf
Name: bicarbonate
Units: umol/kg
Description: <p>concentration of bicarbonate ion ([HCO3]-) in seawater</p>
http://lod.bco-dmo.org/id/dataset-parameter/528832.rdf
Name: carbonate
Units: umol/kg
Description: <p>concentration of carbonate ion ([CO3]2-)</p>
http://lod.bco-dmo.org/id/dataset-parameter/528833.rdf
Name: omega_Ara
Units: unitless
Description: <p>the saturation state of seawater with respect to aragonite</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
6138
https://datadocs.bco-dmo.org/file/3YY3qzPIxO0JmQ/brood2_carb_chem.csv
brood2_carb_chem.csv
Primary data file for dataset ID 528806
download
https://osprey.bco-dmo.org/dataset/528806/data/download
download
onLine
dataset
<p>To determine the dissolved inorganic carbon (DIC) chemistry of seawater in the treatments, total alkalinity (TA), pH on the total scale, temperature, and salinity were measured using standard procedures, and used to calculate pCO2 (uatm), HCO3 - (umolkg-1), CO3 2- (umolkg-1), and the aragonite saturation state (XArag) of seawater using CO2SYS (Pierrot et al. 2006). TA (umol kg-1) was measured through potentiometric titration (SOP 3b, Dickson et al. 2007) using an automatic titrator (DL50, Mettler Toledo) filled with certified acid titrant (0.1 M HCl, 0.6 NaCl, Dickson Laboratory, Scripps Institution of Oceanography). The pH probe (DG101-SC, Mettler Toledo) attached to the titrator was 3-point calibrated with pH 4.00, 7.00, and 10.00 buffers (Fisher, NBS). Certified reference material with a known TA (Batch 98, http://andrew.ucsd. edu/index.html) was titrated daily to determine the accuracy and precision of the analyses.&nbsp;</p>
<p>Seawater samples (50 mL) from the treatment tanks were brought to 25C, weighed and titrated in a waterjacketed beaker within 2-3 h of collection. The pH values and the titrant volumes (cm3) obtained from the titrations were sub-sampled for the range between pH 3.0 and 3.5 and inserted into a Microsoft Excel spreadsheet (Fangue et al. 2010), which calculated Gran’s function as a product of the mass of titrant added (Dickson et al. 2007). Treatment tank pH was determined spectrophotometrically using m-cresol purple dye (Sigma-Aldrich) following SOP 6b of Dickson et al. (2007) with modification (Fangue et al. 2010). Preliminary sampling of the seawater in the tanks throughout the day confirmed that the pCO2 treatments were stable over a 24-h period.</p>
<p><strong>References:</strong></p>
<p>Dickson AG, Sabine CL, Christian JR (eds) (2007) Guide to best practices for ocean CO2 measurements. PICES Special Publication 3, p 191</p>
<p>Fangue NA, O’Donnell MJ, Sewell MA, Matson PG, MacPherson AC, Hoffman GE (2010) A laboratory-based, experimental system for the study of ocean acidification effects on marine invertebrate larvae. Limnol Oceanogr Methods 8:441-452</p>
Specified by the Principal Investigator(s)
<p><strong>BCO-DMO processing notes:</strong></p>
<p>- added conventional header with dataset name, PI name, version date, reference information<br />
- added lab, lat, lon, expt columns<br />
- renamed parameters to BCO-DMO standard<br />
- combined data from Table 1, 2012 and 2012 - sorted by date, temp, treatment</p>
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
Automatic titrator
Automatic titrator
PI Supplied Instrument Name: Automatic titrator PI Supplied Instrument Description:Model DL50, Mettler-Toledo, Columbus, OH, USA Instrument Name: Titrator Instrument Short Name:Titrator Instrument Description: Titrators are instruments that incrementally add quantified aliquots of a reagent to a sample until the end-point of a chemical reaction is reached. Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/LAB12/
Deployment: lab_Edmunds_NMMBA
lab_Edmunds_NMMBA
Natl Museum Mar. Bio. and Aquar. Taiwan
Natl Museum Mar. Bio. and Aquar. Taiwan
laboratory
lab_Edmunds_NMMBA
Peter J. Edmunds
California State University Northridge
Natl Museum Mar. Bio. and Aquar. Taiwan
Natl Museum Mar. Bio. and Aquar. Taiwan
laboratory