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            <gco:CharacterString>Cite this dataset as: Lomas, M. W., Martiny, A. (2020) Global ocean Particulate Organic Matter (POM) ratios from 1971-2014 (Biological C:N:P ratios project, Global POM project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 2) Version Date 2020-12-21 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.526747.2 [access date]</gco:CharacterString>
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        <gco:CharacterString>Global Ocean POM Data Ratios Dataset Description: &amp;lt;p&amp;gt;Concentrations and ratios of particulate organic carbon, nitrogen, and phosphorus in the global ocean.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;When using this data, please cite the original publication:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Martiny AC, Vrugt JA, Lomas MW (2014) Concentrations and ratios of particulate organic carbon, nitrogen, and phosphorus in the global ocean. Scientific Data 1:140048. &amp;lt;a href=&amp;quot;http://dx.doi.org/10.1038/sdata.2014.48&amp;quot;&amp;gt;http://dx.doi.org/10.1038/sdata.2014.48&amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Additionally, please cite the Dryad data package:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Martiny AC, Vrugt JA, Lomas MW (2014) Data from: Concentrations and ratios of particulate organic carbon, nitrogen, and phosphorus in the global ocean. Dryad Digital Repository. &amp;lt;a href=&amp;quot;http://dx.doi.org/10.5061/dryad.d702p&amp;quot;&amp;gt;http://dx.doi.org/10.5061/dryad.d702p&amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;Marine particulate organic carbon (POC), nitrogen (PON), and phosphorus (POP) from 70 cruises or time-series during the last 40 years are reported.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Nearly all POC and PON measurements were done by collecting seawater particles onto glass-fibers filters (i.e., GF/F) and quantified using a combustion GC-IR based elemental analyzer68. The only exceptions were ‘EUMELI’ and ‘OLIPAC’, where PON was measured using a chemical oxidation technique38. Particulate phosphorus was quantified using the ash-hydrolysis method26,69. We operationally defined station IDs as samples taken within a 1°×1° area on the same day11.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The data was gathered by searching available databases (i.e., PANGAEA, BCO-DMO, JGOFS, and IFREMER) as well as published literature. We aggregated all available datasets in order to create the most exhaustive global description of particulate organic nutrients and thus did not exclude any specific cruises or time-series. The only data excluded were samples subjected to a prior manipulation or incubation.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/54877.rdf" xlink:title="OCE-1046297" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1046297 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1046297</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/54927.rdf" xlink:title="OCE-0752366" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-0752366 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=0752366</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/54939.rdf" xlink:title="OCE-1045966" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1045966 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1045966</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/526780.rdf" xlink:title="OCE-0928544" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-0928544 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=0928544</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/526868.rdf" xlink:title="OCE-1258836" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1258836 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1258836</gmx:Anchor>
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&lt;p&gt;The conceptual hypotheses for this study are as follows: 1. The C:N:P ratio of a cell is constrained by its broad taxonomic group, which determines, for example, whether it has an outer shell, its size, functional metabolism, membrane lipid composition. 2. Within a taxon, there is high genetic diversity. Some of this genetic diversity is potentially laterally transferred, or can be lost within taxa, and confers various functional abilities (organic phosphate assimilation, nitrate assimilation, photoheterotrophy, etc.). Functional diversity provides the cell with further flexibility, such as the ability to respond to varying nutrient supply rates/ratios, and affects a cell's C:N:P ratio within the range specified by the taxon. 3. Given these taxonomic and genetic constraints, a cell is physiologically plastic and modifies how it allocates cellular resources in response to nutrient supply rates/ratios in the environment. 4. The microbial diversity (taxonomic, genetic, and functional) of the surface ocean varies over time and space, driven by many factors in addition to nutrients. The sum of this mixture composes the ecosystem C:N:P, the ratio that Redfield described.&lt;/p&gt;
&lt;p&gt;Based on this framework, the CoPIs will make field observations of taxon-specific stoichiometry and growth rates, genomic analyses, and conduct laboratory chemostat experiments to improve understanding of how ocean taxonomic, genetic, and functional biodiversity control the stoichiometry of the surface ocean plankton. Their analyses of these data would lead to a mechanistic understanding of variations in the Redfield ratio, both spatially and temporally.&lt;/p&gt;
&lt;p&gt;This study will greatly expand knowledge of the genomic diversity among ocean microbes and how this diversity affects biogeochemistry. The stoichiometry of the ocean's microbes is a parameter that nearly every chemical or biological oceanographer uses, from converting measurements made in one element to another, to estimating regional and global nitrogen budgets. The research also has important implications for the global carbon budget and any changes that might result from climate change.&lt;/p&gt;
&lt;p&gt;To understand mechanistically temporal and spatial variability of the plankton C:N:P ratio, biodiversity must be studied not only at the traditional taxonomic level, but at the genetic and functional levels which dictate organism response to their environment. Data will be integrated into a combined ocean ecological, evolutionary, and biogeochemical model, with flexible stoichiometry, including cellular biochemical allocations. Seeding a coupled physical-biological model of the oceans with multiple competing genotypes enables the exploration of ecological and evolutionary patterns of resource acquisition and C:N:P ratios. Developing a more mechanistic examination of the course of ecology and evolution, in which laboratory and field data define tradeoffs between different growth and nutrient acquisition strategies, would estabblish the framework of adaptive dynamics for determining &quot;evolutionarily convergence&quot;. Finally, model outcomes will be evaluated against field data.&lt;/p&gt;
&lt;p&gt;The field work planned for this project includes several cruises: BV46 (September/October 2011), BV48 (September 2012), a June 2013 cruise from Bermuda to the Labrador Sea, and a cruise from Hawaii to Tahiti (May 2014). Additionally, samples will be be acquired during cruises of opportunity.&lt;/p&gt;</gco:CharacterString>
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                            <gco:CharacterString>&lt;p&gt;Knowledge of concentrations and elemental ratios of suspended particles are important for understanding many biogeochemical processes in the ocean. These include patterns of phytoplankton nutrient limitation as well as linkages between the cycles of carbon and nitrogen or phosphorus. To further enable studies of ocean biogeochemistry, we here present a global dataset consisting of 100,605 total measurements of particulate organic carbon, nitrogen, or phosphorus analyzed as part of 70 cruises or time-series. The data are globally distributed and represent all major ocean regions as well as different depths in the water column. The global median C:P, N:P, and C:N ratios are 163, 22, and 6.6, respectively, but the data also includes extensive variation between samples from different regions. Thus, this compilation will hopefully assist in a wide range of future studies of ocean elemental ratios.&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;Related References:&lt;/strong&gt;&lt;br /&gt;
&lt;a href=&quot;http://data.bco-dmo.org/Global_POM/Martiny_et_al_2013_latitudinal_CN_patterns.pdf&quot; target=&quot;_blank&quot;&gt;Martiny, A. C., Vrugt, J. A., Primeau, F. W. &amp;amp; Lomas, M. W. Regional variation in the particulate organic carbon to nitrogen ratio in the surface ocean. Global Biogeochem. Cycles 27, 723–731 (2013).&lt;/a&gt;&lt;/p&gt;
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&amp;amp;nbsp;- Generated from original file: &amp;quot;CNP_data.xlsx&amp;quot; contributed by Adam Martiny&amp;lt;br /&amp;gt;
&amp;amp;nbsp;- Single column for Date inserted with combined Year, Month, Day formatted as YYYYMMDD&amp;lt;br /&amp;gt;
&amp;amp;nbsp;- Parameter names edited to conform to BCO-DMO naming convention found at &amp;lt;a href=&amp;quot;http://usjgofs.whoi.edu/naming-guidelines.html&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;Choosing Parameter Name&amp;lt;/a&amp;gt;&amp;lt;br /&amp;gt;
&amp;amp;nbsp;- Identified “Station” column as “Dataset_Station” since the station ids here don't agree with other data from similarly named datasets&amp;lt;br /&amp;gt;
&amp;amp;nbsp;- Padded decimal places to two places where appropriate&amp;lt;br /&amp;gt;
&amp;amp;nbsp;- Standardized bad data value at “nd”&amp;lt;br /&amp;gt;
&amp;amp;nbsp;&amp;lt;strong&amp;gt;- Note: Some non standard dates/times contained in original data contributed were changed to 'nd (no datda).&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt;</gco:CharacterString>
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