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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/660050.rdf" xlink:actuate="onRequest">Experimental data on growth rates of Pleurochrysis carterae analyzed at Bigelow Laboratory from 2013. (OA Copes Coccoliths project)</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Balch, W., Fields, D. (2016) Experimental data on growth rates of Pleurochrysis carterae analyzed at Bigelow Laboratory from 2013. (OA Copes Coccoliths project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2016-09-28 [if applicable, indicate subset used]. doi:10.1575/1912/bco-dmo.660050.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>Experimental data on growth rates of Pleurochrysis carterae Dataset Description: &amp;lt;p&amp;gt;Experimental results describing the growth rate of&amp;amp;nbsp;&amp;lt;em&amp;gt;Pleurochrysis carterae&amp;amp;nbsp;&amp;lt;/em&amp;gt;(NCMA strain 645). It was isolated from&amp;amp;nbsp;41.525 degrees North, 70.6736 degrees West (Woods Hole, Massachusetts USA), but has been maintained in culture since 1958.&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Cultures:&amp;amp;nbsp;&amp;lt;/strong&amp;gt;&amp;lt;em&amp;gt;Pleurochrysis&amp;lt;/em&amp;gt;&amp;amp;nbsp;&amp;lt;em&amp;gt;carterae&amp;lt;/em&amp;gt;&amp;amp;nbsp;cultures were maintained in exponential growth phase under axenic conditions in semi-continuous batch culture using L1-Si media prepared on 0.2 um-filtered, UV-sterilized, autoclaved seawater.&amp;amp;nbsp; Cultures were acclimated to one of three&amp;amp;nbsp;pCO2&amp;amp;nbsp;treatments for &amp;amp;gt; 9 generations before experiments were performed.&amp;amp;nbsp; Cultures were maintained in an incubator at 16.5 +/- 0.5 degrees C and 470 umol photons/m-2/s&amp;amp;nbsp;PAR on a 14-10 light-dark cycle.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;pCO2&amp;amp;nbsp;Treatments: &amp;lt;/strong&amp;gt;Carbonate chemistry was manipulated by bubbling cultures and prepared media with 500 mL/min&amp;amp;nbsp;with 0.2 um-filtered 280, 380, or 750 ppm&amp;amp;nbsp;pCO2&amp;amp;nbsp;air.&amp;amp;nbsp; The&amp;amp;nbsp;pCO2&amp;amp;nbsp;levels of the treatment air were established using two mass flow controllers (Aalborg, Orangeburg, NY, USA) for each treatment to precisely mix in-house compressed air and pure CO2&amp;amp;nbsp;(Maine Oxy, Auburn, ME, USA).&amp;amp;nbsp; The in-house compressed air was stripped of CO2&amp;amp;nbsp;to less than 10 ppm CO2&amp;amp;nbsp;using a Puregas VCD CO2&amp;amp;nbsp;Adsorber (Puregas, LLC, Broomfield, CO, USA).&amp;amp;nbsp; The&amp;amp;nbsp;pCO2&amp;amp;nbsp;of the gas mixtures was stable to +/- 8 ppm.&amp;amp;nbsp;&amp;amp;nbsp;pCO2&amp;amp;nbsp;values of the cultures may be different than the target levels due to biological activity.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Growth rate measurements:&amp;amp;nbsp;&amp;lt;/strong&amp;gt; At the same time each day, the cell density of each&amp;amp;nbsp;pCO2&amp;amp;nbsp;treatment culture was measured in order to calculate the growth rate.&amp;amp;nbsp; The data analyzed represent three consecutive growth cycles.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Cell density:&amp;amp;nbsp;&amp;lt;/strong&amp;gt;Culture density was measured using a Moxi Z mini automated cell counter (ORFLO Technologies, Ketchum, ID, USA), which has a coefficient of variation of 4%.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/514411.rdf" xlink:title="OCE-1220068" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1220068 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1220068</gmx:Anchor>
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NSF 13-586 was the final solicitation that will be released for this program.
PI Meetings:
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2nd U.S. Ocean Acidification PI Meeting(Sept. 18-20, 2013, Washington, DC)
3rd U.S. Ocean Acidification PI Meeting (June 9-11, 2015, Woods Hole, MA – Tentative)
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Press Release 10-186 NSF Awards Grants to Study Effects of Ocean Acidification
Discovery Blue Mussels &quot;Hang On&quot; Along Rocky Shores: For How Long?
Discovery nsf.gov - National Science Foundation (NSF) Discoveries - Trouble in Paradise: Ocean Acidification This Way Comes - US National Science Foundation (NSF)
Press Release 12-179 nsf.gov - National Science Foundation (NSF) News - Ocean Acidification: Finding New Answers Through National Science Foundation Research Grants - US National Science Foundation (NSF)
Press Release 13-102 World Oceans Month Brings Mixed News for Oysters
Press Release 13-108 nsf.gov - National Science Foundation (NSF) News - Natural Underwater Springs Show How Coral Reefs Respond to Ocean Acidification - US National Science Foundation (NSF)
Press Release 13-148 Ocean acidification: Making new discoveries through National Science Foundation research grants
Press Release 13-148 - Video nsf.gov - News - Video - NSF Ocean Sciences Division Director David Conover answers questions about ocean acidification. - US National Science Foundation (NSF)
Press Release 14-010 nsf.gov - National Science Foundation (NSF) News - Palau's coral reefs surprisingly resistant to ocean acidification - US National Science Foundation (NSF)
Press Release 14-116 nsf.gov - National Science Foundation (NSF) News - Ocean Acidification: NSF awards $11.4 million in new grants to study effects on marine ecosystems - US National Science Foundation (NSF)</gco:CharacterString>
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&lt;p&gt;Ocean acidification is one of the most pressing marine science issues of our time, with potential biological impacts spanning all marine phyla and potential societal impacts affecting man's relationship to the sea. Rising levels of atmospheric pCO2 are increasing the acidity of the world oceans. It is generally held that average surface ocean pH has already declined by 0.1 pH units relative to the pre-industrial level (Orr et al., 2005), and is projected to decrease 0.3 to 0.46 units by the end of this century, depending on CO2 emission scenarios (Caldeira and Wickett, 2005). The overall goal of this research is to parameterize how changes in pCO2 levels could alter the biological and alkalinity pumps of the world ocean. Specifically, the direct and indirect effects of ocean acidification will be examined within a simple, controlled predator/prey system containing a single prey phytoplankton species (the coccolithophore, Emiliania huxleyi) and a single predator (the oceanic metazoan grazer, Calanus finmarchicus). The experiments are designed to elucidate both direct effects (i.e. effects of ocean acidification on the individual organisms only) and interactive effects (i.e. effects on the combined predator/prey system). Interactive experiments with phytoplankton prey and zooplankton predator are a critical starting point for predicting the overall impact of ocean acidification in marine ecosystems. To meet these goals, a state-of-the-art facility will be constructed with growth chambers that are calibrated and have highly-controlled pH and alkalinity levels. The strength of this approach lies in meticulous calibration and redundant measurements that will be made to ensure that conditions within the chambers are well described and tightly monitored for DIC levels. Growth and calcification rates in coccolithophores and the developmental rates, morphological and behavioral effects on copepods will be measured. The PIC and POC in the algae and the excreted fecal pellets will be monitored for changes in the PIC/POC ratio, a key parameter for modeling feedback mechanisms for rising pCO2 levels. In addition, 14C experiments are planned to measure calcification rates in coccolithophores and dissolution rates as a result of grazing. These key experiments will verify closure in the mass balance of PIC, allowing the determination of actual dissolution rates of PIC within the guts of copepod grazers.&lt;/p&gt;</gco:CharacterString>
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http://lod.bco-dmo.org/id/dataset-parameter/660123.rdf
	Name: cell_density
	Units: cell per milliliter cells/mL
	Description: &lt;p&gt;Cell density of the culture as measured by the Moxi Z Automated Cell Counter.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/660124.rdf
	Name: ln_cellDensity
	Units: ln(cells/mL)
	Description: &lt;p&gt;The natural log of the cell density.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/660125.rdf
	Name: linest_slope
	Units: (ln(cells/mL))/day
	Description: &lt;p&gt;The slope resulting from the excel function LINEST which calculates the statistics for a line by using the 'least squares' method to calculate a straight line that best fits the data. One line is calculated for each growth cycle and the slope represents the growth rate of the algae during that growth cycle. In this case the line was calculated from ln(cell density) and day.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/660126.rdf
	Name: linest_intercept
	Units: unitless
	Description: &lt;p&gt;The intercept resulting from the excel function LINEST which calculates the statistics for a line by using the &amp;#039;least squares&amp;#039; method to calculate a straight line that best fits the data.  One line is calculated for each growth cycle.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/660127.rdf
	Name: growthRate
	Units: u/day
	Description: &lt;p&gt;The growth rate for the given growth cycle. This is the slope of the line fit to the ln(cell density) and day data. One growth rate is calculated for each growth cycle.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/660128.rdf
	Name: mean_growthRate
	Units: u/day
	Description: &lt;p&gt;The average growth rate from the three growth cycles.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/660129.rdf
	Name: stdev_growthRate
	Units: day-1
	Description: &lt;p&gt;The standard deviation of the growth rates from the three growth cycles.&lt;/p&gt; 
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&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;pCO2&amp;amp;nbsp;Treatments: &amp;lt;/strong&amp;gt;Carbonate chemistry was manipulated by bubbling cultures and prepared media with 500 mL/min&amp;amp;nbsp;with 0.2 um-filtered 280, 380, or 750 ppm&amp;amp;nbsp;pCO2&amp;amp;nbsp;air.&amp;amp;nbsp; The&amp;amp;nbsp;pCO2&amp;amp;nbsp;levels of the treatment air were established using two mass flow controllers (Aalborg, Orangeburg, NY, USA) for each treatment to precisely mix in-house compressed air and pure CO2&amp;amp;nbsp;(Maine Oxy, Auburn, ME, USA).&amp;amp;nbsp; The in-house compressed air was stripped of CO2&amp;amp;nbsp;to less than 10 ppm CO2&amp;amp;nbsp;using a Puregas VCD CO2&amp;amp;nbsp;Adsorber (Puregas, LLC, Broomfield, CO, USA).&amp;amp;nbsp; The&amp;amp;nbsp;pCO2&amp;amp;nbsp;of the gas mixtures was stable to +/- 8 ppm.&amp;amp;nbsp;&amp;amp;nbsp;pCO2&amp;amp;nbsp;values of the cultures may be different than the target levels due to biological activity.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Growth rate measurements:&amp;amp;nbsp;&amp;lt;/strong&amp;gt; At the same time each day, the cell density of each&amp;amp;nbsp;pCO2&amp;amp;nbsp;treatment culture was measured in order to calculate the growth rate.&amp;amp;nbsp; The data analyzed represent three consecutive growth cycles.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Cell density:&amp;amp;nbsp;&amp;lt;/strong&amp;gt;Culture density was measured using a Moxi Z mini automated cell counter (ORFLO Technologies, Ketchum, ID, USA), which has a coefficient of variation of 4%.&amp;lt;/p&amp;gt;</gco:CharacterString>
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                <gco:CharacterString>&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Growth Rate:&amp;amp;nbsp; &amp;lt;/strong&amp;gt;Growth rate (u) with units d-1&amp;amp;nbsp;(per day) was calculated using the Excel function LINEST, which calculates the statistics for a line by using the ‘least squares’ method to calculate a straight line that best fits the data. &amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The equation for the line is:&amp;amp;nbsp; y =&amp;amp;nbsp;mx&amp;amp;nbsp;+ b. &amp;amp;nbsp; &amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The syntax is:&amp;amp;nbsp; LINEST(known_y’s, [known_x’s], [const], [stats])&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;In this case, the ‘known_y’s’ were the ln(cell density); the ‘known_x’s’ were the days of the growth cycle; [const] was set to ‘TRUE’ which calculates the intercept (b) instead of forcing it to zero; and [stats] was set to ‘TRUE’ in order to return the regression statistics of the line.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The slope of the line represents the growth rate for the given growth cycle and is analogous to using the standard growth rate equation, except that it incorporates all data points during the growth cycle, not simply the first (0) and last (n) data points.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;DMO notes:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
- added underscores and removed spaces and units from column names&amp;lt;br /&amp;gt;
- changed column names to comply with BCO-DMO standards.&amp;lt;br /&amp;gt;
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</gmi:platform>
          </gmi:MI_AcquisitionInformation>
  </gmi:acquisitionInformation>
</gmi:MI_Metadata>
