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            <gco:CharacterString>Cite this dataset as: Takeshita, Y., Martz, T., McGillis, W., Price, N., Smith, J. (2016) Benthic Ecosystem and Acidification Measuring System (BEAMS) data from two sites on the western terrace of the Palmyra Atoll collected during 2014 (BEAMS project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2016-11-29 [if applicable, indicate subset used]. doi:10.1575/1912/bco-dmo.666280.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>BEAMS data from two sites on the western terrace on Palmyra Atoll during 2014. Dataset Description: &amp;lt;p&amp;gt;Benthic Ecosystem and Acidification Measuring System (BEAMS) data from two sites (LL and RT4) on the western terrace of the Palmyra Atoll. The data was collected in 2014.&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;This dataset was collected using the Benthic Ecosystem and Acidification Measuring System (BEAMS). The details of this technique and dataset can be in the reference provided below. BEAMS uses autonomous sensors to quantify mean gradients of pH and O2&amp;amp;nbsp;and the current velocity profile in the BBL to calculate benthic fluxes of O2&amp;amp;nbsp;(NCP) and TA (NCC). The NCP and NCC provided here represent metabolic rates under completely natural (e.g. flow and light) conditions.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/651860.rdf" xlink:title="OCE-1316006" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1316006 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1316006</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/651864.rdf" xlink:title="OCE-1316047" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1316047 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1316047</gmx:Anchor>
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Rising sea surface temperatures and ocean acidification (OA) may threaten the ability of calcified organisms to build carbonate reefs, but it is unclear if particular reefs have the capacity to tolerate global change. Current understanding of the effects of OA on coral reefs originates from single-species laboratory studies largely focused on scleractinian corals. Traditionally, these experiments attempt to mimic static future conditions under the assumption that coastal regimes are as constant as -- and will acidify at the same rate as -- open ocean surface waters. Predictions based on these oversimplified scenarios are unrealistic because numerous benthic organisms, including calcifiers and primary producers, significantly alter the bulk seawater carbonate chemistry over a diurnal cycle. Further, the prevalence of recently appreciated extreme diel fluctuations in pH across some reefs suggests that benthic species may be acclimated to future carbonate conditions.&lt;/p&gt;
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http://lod.bco-dmo.org/id/dataset-parameter/666473.rdf
	Name: pH_0_5m
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http://lod.bco-dmo.org/id/dataset-parameter/666474.rdf
	Name: pH_0_3m
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	Description: &lt;p&gt;In situ pH on the total hydrogen ion scale; 3 x n matrix; data collected at 0.3m above the benthos.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/666475.rdf
	Name: temp_1_1m
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http://lod.bco-dmo.org/id/dataset-parameter/666476.rdf
	Name: temp_0_5m
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	Description: &lt;p&gt;Temperature in Celsius; 3 x n matrix; data collected at 0.5m above the benthos.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/666477.rdf
	Name: temp_0_3m
	Units: celsius
	Description: &lt;p&gt;Temperature in Celsius; 3 x n matrix; data collected at 0.3m above the benthos.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/666478.rdf
	Name: DO_1_1m
	Units: umol/kg
	Description: &lt;p&gt;Dissolved O2; 3 x n matrix; data collected at 1.1m above the benthos.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/666479.rdf
	Name: DO_0_5m
	Units: umol/kg
	Description: &lt;p&gt;Dissolved O2; 3 x n matrix; data collected at 0.5m above the benthos.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/666480.rdf
	Name: DO_0_3m
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	Description: &lt;p&gt;Dissolved O2; 3 x n matrix; data collected at 0.3m above the benthos.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/666481.rdf
	Name: OMEGA_1_1m
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http://lod.bco-dmo.org/id/dataset-parameter/666482.rdf
	Name: OMEGA_0_5m
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	Description: &lt;p&gt;Aragonite Saturation State; 3 x n matrix; data collected at 0.5m above the benthos.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/666483.rdf
	Name: OMEGA_0_3m
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	Description: &lt;p&gt;Aragonite Saturation State; 3 x n matrix; data collected at 0.3m above the benthos.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/666484.rdf
	Name: PAR
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http://lod.bco-dmo.org/id/dataset-parameter/666485.rdf
	Name: pressure
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http://lod.bco-dmo.org/id/dataset-parameter/666486.rdf
	Name: current_speed
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http://lod.bco-dmo.org/id/dataset-parameter/666487.rdf
	Name: salinity
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http://lod.bco-dmo.org/id/dataset-parameter/666488.rdf
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http://lod.bco-dmo.org/id/dataset-parameter/666489.rdf
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http://lod.bco-dmo.org/id/dataset-parameter/666490.rdf
	Name: NCC_Q_0_9
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http://lod.bco-dmo.org/id/dataset-parameter/666491.rdf
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http://lod.bco-dmo.org/id/dataset-parameter/666492.rdf
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                <gco:CharacterString>&amp;lt;p&amp;gt;Questionable rates have been removed through a quality control procedure described in detail in the reference above. Briefly, 1) measurements when the benthic boundary layer was stratified were removed, and 2) Spikes in the data were removed based on the observed DeltapH/DeltaO2&amp;amp;nbsp;relationship.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;BCO-DMO Data Processing Notes:&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;-combined 2 datasets (one from each site) into one file&amp;lt;br /&amp;gt;
-replaced &amp;quot;NaN&amp;quot; with &amp;quot;nd&amp;quot;&amp;lt;br /&amp;gt;
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                          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/person/651875.rdf" xlink:actuate="onRequest">Yuichiro Takeshita</gmx:Anchor>
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