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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/522697.rdf" xlink:actuate="onRequest">Seriatopora bleaching expt: temperature, salinity, light in tanks, Taiwan 2010 (MCR LTER project, Climate_Coral_Larvae project)</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Edmunds, P. J., Fan, T. (2014) Seriatopora bleaching expt: temperature, salinity, light in tanks, Taiwan 2010 (MCR LTER project, Climate_Coral_Larvae project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 2014-08-12) Version Date 2014-08-12 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/522697 [access date]</gco:CharacterString>
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        <gco:CharacterString>Seriatopora bleaching expt: temperature, salinity, light in tanks Dataset Description: &amp;lt;p&amp;gt;We hypothesized that ocean acidification would cause bleaching as defined by decreased photochemical efficiency, reduced photosynthetic capacity and efficiency, depressed chlorophyll a content, and lowered&amp;amp;nbsp;&amp;lt;em&amp;gt;Symbiodinium&amp;lt;/em&amp;gt;&amp;amp;nbsp;densities and that these effects would be exacerbated with high temperature.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Related Datasets:&amp;lt;br /&amp;gt;
&amp;lt;a href=&amp;quot;http://www.bco-dmo.org/dataset/522591&amp;quot;&amp;gt;Symbiodinium_Seriatopora photosynthesis&amp;lt;/a&amp;gt;&amp;lt;br /&amp;gt;
&amp;lt;a href=&amp;quot;http://www.bco-dmo.org/dataset/522737&amp;quot;&amp;gt;Symbiodinium_Seriatopora PI curve&amp;lt;/a&amp;gt;&amp;lt;br /&amp;gt;
&amp;lt;a href=&amp;quot;http://www.bco-dmo.org/dataset/522631&amp;quot;&amp;gt;Symbiodinium_Seriatopora water chemistry&amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;These data were published in C. B. Wall, T.-Y. Fan, P. J. Edmunds (2014) Ocean acidification has no effect on thermal bleaching in the coral. Coral Reefs 33:119-13. doi:&amp;amp;nbsp;&amp;lt;a href=&amp;quot;http://dx.doi.org/10.1007/s00338-013-1085-2&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;http://dx.doi.org/10.1007/s00338-013-1085-2&amp;lt;/a&amp;gt;.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;a href=&amp;quot;http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Wall_Fan_Edmunds_for_Taiwan_Bleaching_data2013_BCODMO.xlsx&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;Download complete data for this publication (Excel file)&amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Experimental design&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Four treatments contrasted high and low temperature and pCO2:&amp;lt;br /&amp;gt;
Ambient temperature = 27.5 oC&amp;lt;br /&amp;gt;
Ambient pCO2 = 39.0 Pa&amp;lt;br /&amp;gt;
High temperature = 30.5 oC&amp;lt;br /&amp;gt;
High pCO2 = 86 Pa&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Juvenile&amp;amp;nbsp;&amp;lt;em&amp;gt;Seriatopora&amp;amp;nbsp;caliendrum&amp;lt;/em&amp;gt;&amp;amp;nbsp;were collected from Hobihu Reef, Nanwan Bay, Taiwan, and kept at the National Museum of Marine Biology and Aquarium (NMMBA), where they were placed randomly into the treatment tanks for incubations lasting 14 days.&amp;amp;nbsp;Corals were exposed to treatments in 8 tanks filled with filtered seawater. Treatments were maintained at a salinity of 33 and were monitored daily for temperature, salinity, irradiance, pH and carbonate chemistry.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Photochemical efficiency:&amp;amp;nbsp;&amp;lt;/strong&amp;gt;The effects of temperature and pCO2 on photochemical efficiency were tested by measuring the maximum photochemical efficiency of open RCIIs (Type II reaction centers) in the dark (Fv/Fm) and the effective photochemical efficiency of RCII in the light (deltaF/Fm') using pulse amplitude modulation (PAM) fluorometry.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Photosynthesis-irradiance (P/I) curves:&amp;amp;nbsp;&amp;lt;/strong&amp;gt;To test for the effects of pCO2 and temperature on the ability for&amp;amp;nbsp;&amp;lt;em&amp;gt;Symbiodinium&amp;lt;/em&amp;gt;&amp;amp;nbsp;to utilize light and perform photosynthesis, net photosynthesis (P^net), determined from changes in O2 concentrations in seawater, was measured under different irradiances using three corals selected randomly from each treatment tank.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Chlorophyll-a concentration and&amp;amp;nbsp;&amp;lt;em&amp;gt;Symbiodinium&amp;lt;/em&amp;gt;&amp;amp;nbsp;density:&amp;amp;nbsp;&amp;lt;/strong&amp;gt;Chlorophyll-a concentration and&amp;amp;nbsp;&amp;lt;em&amp;gt;Symbiodinium&amp;lt;/em&amp;gt;&amp;amp;nbsp;density were determined.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Relevant References:&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;For full details see&amp;amp;nbsp;&amp;lt;a href=&amp;quot;http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Wall_etal_2014_Methodology.pdf&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;Methodology&amp;lt;/a&amp;gt;, from C. B. Wall, T.-Y. Fan, P. J. Edmunds (2014) Ocean acidification has no effect on thermal bleaching in the coral. Coral Reefs 33:119-13&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/55016.rdf" xlink:title="OCE-0844785" xlink:actuate="onRequest">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</gmx:Anchor>
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&lt;p&gt;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.&lt;/p&gt;
&lt;p&gt;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.&lt;/p&gt;
&lt;p&gt;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.&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;From &lt;a href=&quot;http://www.lternet.edu/sites/mcr/&quot;&gt;http://www.lternet.edu/sites/mcr/&lt;/a&gt; and &lt;a href=&quot;http://mcr.lternet.edu/&quot;&gt;http://mcr.lternet.edu/&lt;/a&gt;&lt;/strong&gt;:&lt;br /&gt;
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.&lt;/p&gt;
&lt;p&gt;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.&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;MCR LTER Data:&lt;/strong&gt; 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.&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;This project is supported by continuing grants with slight name variations:&lt;/strong&gt;&lt;/p&gt;
&lt;ul&gt;
&lt;li&gt;LTER: Long-Term Dynamics of a Coral Reef Ecosystem&lt;/li&gt;
&lt;li&gt;LTER: MCR II - Long-Term Dynamics of a Coral Reef Ecosystem&lt;/li&gt;
&lt;li&gt;LTER: MCR IIB: Long-Term Dynamics of a Coral Reef Ecosystem&lt;/li&gt;
&lt;li&gt;LTER: MCR III: Long-Term Dynamics of a Coral Reef Ecosystem&lt;/li&gt;
&lt;li&gt;LTER: MCR IV: Long-Term Dynamics of a Coral Reef Ecosystem&lt;/li&gt;
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                            <gco:CharacterString>&lt;p&gt;&lt;span style=&quot;font-size:13px&quot;&gt;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.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;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.&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;The following publications and data resulted from this project:&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;2013    Wall CB, Fan TY, Edmunds PJ.  Ocean acidification has no effect on thermal bleaching in the coral &lt;em&gt;Seriatopora caliendrum&lt;/em&gt;.  Coral Reefs 33: 119-130.&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/522591&quot; target=&quot;_blank&quot;&gt;Symbiodinium_Seriatopora photosynthesis&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/522737&quot; target=&quot;_blank&quot;&gt;Symbiodinium_Seriatopora PI curve&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/522697&quot; target=&quot;_blank&quot;&gt;Symbiodinium_Seriatopora temp-salinity-light&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/522631&quot; target=&quot;_blank&quot;&gt;Symbiodinium_Seriatopora water chemistry&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Wall_Fan_Edmunds_for_Taiwan_Bleaching_data2013_BCODMO.xlsx&quot; target=&quot;_blank&quot;&gt;- Download complete data for this publication (Excel file)&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;2013    Wall CB, Edmunds PJ. &lt;em&gt;In situ &lt;/em&gt;effects of low pH and elevated HCO3- on juvenile &lt;em&gt;Porites&lt;/em&gt; spp. in Moorea, French Polynesia.  Biological Bulletin 225:92-101.&lt;br /&gt;
Data at &lt;a href=&quot;http://mcr.lternet.edu/&quot; target=&quot;_blank&quot;&gt;MCR&lt;/a&gt; and PANGEA: &lt;a href=&quot;http://doi.pangaea.de/10.1594/PANGAEA.833913&quot; target=&quot;_blank&quot;&gt;doi.pangaea.de/10.1594/PANGAEA.833913&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Wall_Edmunds_2013_BioBull_BCODMO.xlsx&quot; target=&quot;_blank&quot;&gt;- Download complete data for this publication (Excel file)&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;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.&lt;br /&gt;
Data also at PANGEA: &lt;a href=&quot;http://doi.pangaea.de/10.1594/PANGAEA.831612&quot; target=&quot;_blank&quot;&gt;doi.pangaea.de/10.1594/PANGAEA.831612&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/528806&quot;&gt;brooded coral larvae 2 - carbonate chemistry&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/528880&quot;&gt;brooded coral larvae 2 - larval release March 2003-2008&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/528834&quot;&gt;brooded coral larvae 2 - respiration_photosyth_mortality&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Cumbo_etal_2013_MarBio_BCODMO.xlsx&quot; target=&quot;_blank&quot;&gt;- Download complete data for this publication (Excel file)&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;2013    Edmunds PJ, Cumbo VR, Fan TY. Metabolic costs of larval settlement and metamorphosis in the coral &lt;em&gt;Seriatopora caliendrum&lt;/em&gt; under ambient and elevated pCO2.  Journal Experimental Marine Biology and Ecology 443: 33-38 Data also at PANGEA: &lt;a href=&quot;http://doi.pangaea.de/10.1594/PANGAEA.821644&quot; target=&quot;_blank&quot;&gt;doi:10.1594/PANGAEA.821644&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/526674&quot; target=&quot;_blank&quot;&gt;Coral post-settlement physiology&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Edmunds_etal_2013_JEMBE443_BCODMO.xls&quot; target=&quot;_blank&quot;&gt;- Download complete data for this publication (Excel file)&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;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.&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/527500&quot;&gt;coral-light expt.- PAR&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/527752&quot;&gt;coral-light expt.- carbonate chemistry&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/527729&quot;&gt;coral-light expt.- temp_salinity&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/527816&quot;&gt;coral-light expt.- growth&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/527782&quot;&gt;coral-light expt.- protein&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/527851&quot;&gt;coral-light expt.- survival&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Dufault_etal_2013_JEB_BCODMO.xlsx&quot; target=&quot;_blank&quot;&gt;- Download complete data for this publication (Excel file)&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;2012    Cumbo, VR, Fan TY, Edmunds PJ. Effects of exposure duration on the response of &lt;em&gt;Pocillopora damicornis&lt;/em&gt; larvae to elevated temperature and high pCO2.  J Exp Mar Biol Ecol 439: 100-107.&lt;br /&gt;
Data is also at PANGEA: &lt;a href=&quot;http://doi.pangaea.de/10.1594/PANGAEA.823582&quot; target=&quot;_blank&quot;&gt;doi:10.1594/PANGAEA.823582&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/535163&quot;&gt;brooded coral larvae 3 - carbonate chemistry&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/535219&quot;&gt;brooded coral larvae 3 - light&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/535462&quot;&gt;brooded coral larvae 3 - mortality&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/535425&quot;&gt;brooded coral larvae 3 - protein&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/535328&quot;&gt;brooded coral larvae 3 - respiration and protein&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/535266&quot;&gt;brooded coral larvae 3 - respiration raw data&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/535358&quot;&gt;brooded coral larvae 3 - symbiont density&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/535244&quot;&gt;brooded coral larvae 3 - tank temperature&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Cumbo_etal_2012_JEMBE_data1_BCODMO.xls&quot; target=&quot;_blank&quot;&gt;- Download part 1 of data for this publication (Excel file)&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Cumbo_etal_2012_JEMBE_Tank Parameters_BCODMO.xlsx&quot; target=&quot;_blank&quot;&gt;- Download tank parameters data for this publication (Excel file)&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;2012    Cumbo, VR, Fan TY, Edmunds PJ.  Physiological development of brooded larvae from two pocilloporid corals in Taiwan.  Marine Biology 159: 2853-2866.&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/528781&quot;&gt;brooded coral - carbonate chemistry&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/528641&quot;&gt;brooded coral - release&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/528695&quot;&gt;brooded coral - respiration&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/528728&quot;&gt;brooded coral - settlement competency&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/528761&quot;&gt;brooded coral - size_July&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/528661&quot;&gt;brooded coral - size_protein_symbionts_photosynth&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Cumbo_etal_2012_MarBio_BCODMO .xlsx&quot; target=&quot;_blank&quot;&gt;- Download complete data for this publication (Excel file)&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;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&lt;br /&gt;
Data is also at PANGEA: &lt;a href=&quot;http://doi.pangaea.de/10.1594/PANGAEA.830185&quot; target=&quot;_blank&quot;&gt;doi:10.1594/PANGAEA.830185&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/514198&quot; target=&quot;_blank&quot;&gt;recruit_growth_area&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/506245&quot; target=&quot;_blank&quot;&gt;recruit_growth_weight&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/516783&quot; target=&quot;_blank&quot;&gt;recruit_seawater_chemistry&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/516529&quot; target=&quot;_blank&quot;&gt;recruit_survival&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Dufault_etal_2012_RoyProcB_BCODMO.xlsx&quot; target=&quot;_blank&quot;&gt;- Download complete data for this publication (Excel file)&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;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. &lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/3790&quot; target=&quot;_blank&quot;&gt;CoralLarvae_comparison_respir&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/3809&quot; target=&quot;_blank&quot;&gt;CoralLarvae_release&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/3802&quot; target=&quot;_blank&quot;&gt;CoralLarvae_respir&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://www.bco-dmo.org/dataset/3795&quot; target=&quot;_blank&quot;&gt;CoralLarvae_size&lt;/a&gt;&lt;br /&gt;
&lt;a href=&quot;http://dmoserv3.whoi.edu/data_docs/Climate_Coral_Larvae/Edmunds_etal_2011_JEB_BCODMO.xls&quot; target=&quot;_blank&quot;&gt;- Download complete data for this publication (Excel file)&lt;/a&gt;&lt;/p&gt;</gco:CharacterString>
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&amp;lt;p&amp;gt;Juvenile&amp;amp;nbsp;&amp;lt;em&amp;gt;Seriatopora&amp;amp;nbsp;caliendrum&amp;lt;/em&amp;gt;&amp;amp;nbsp;were collected from Hobihu Reef, Nanwan Bay, Taiwan, and kept at the National Museum of Marine Biology and Aquarium (NMMBA), where they were placed randomly into the treatment tanks for incubations lasting 14 days.&amp;amp;nbsp;Corals were exposed to treatments in 8 tanks filled with filtered seawater. Treatments were maintained at a salinity of 33 and were monitored daily for temperature, salinity, irradiance, pH and carbonate chemistry.&amp;lt;/p&amp;gt;

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&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Photosynthesis-irradiance (P/I) curves:&amp;amp;nbsp;&amp;lt;/strong&amp;gt;To test for the effects of pCO2 and temperature on the ability for&amp;amp;nbsp;&amp;lt;em&amp;gt;Symbiodinium&amp;lt;/em&amp;gt;&amp;amp;nbsp;to utilize light and perform photosynthesis, net photosynthesis (P^net), determined from changes in O2 concentrations in seawater, was measured under different irradiances using three corals selected randomly from each treatment tank.&amp;lt;/p&amp;gt;

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                <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/instrument/712.rdf" xlink:title="Mass Flow Controller" xlink:actuate="onRequest">MFC</gmx:Anchor>
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                <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/instrument/647.rdf" xlink:title="Water Temperature Sensor" xlink:actuate="onRequest">Water Temp Sensor</gmx:Anchor>
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                  <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/deployment/58892.rdf" xlink:title="Deployment" xlink:actuate="onRequest">lab_Edmunds_NMMBA</gmx:Anchor>
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         <gmx:Anchor xlink:href="http://www.nmmba.gov.tw/english/ResearchA/Research_Introduction_" xlink:actuate="onRequest">Natl Museum Mar. Bio. and Aquar. Taiwan</gmx:Anchor>
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                  <gmd:MD_ProgressCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#MD_ProgressCode" codeListValue="completed"/>
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                      <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/deployment/58892.rdf" xlink:title="Deployment" xlink:actuate="onRequest">lab_Edmunds_NMMBA</gmx:Anchor>
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                          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/affiliation/292.rdf" xlink:title="Affiliation" xlink:actuate="onRequest">California State University Northridge</gmx:Anchor>
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      <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/platform/54244.rdf" xlink:title="Natl Museum Mar. Bio. and Aquar. Taiwan" xlink:actuate="onRequest">laboratory</gmx:Anchor>
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