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            <gco:CharacterString>Cite this dataset as: Brush, M. J., Anderson, I. C., Reece, K. S., Song, B. (2025) Watershed concentrations of dissolved inorganic carbon, dissolved organic carbon, and particulate organic carbon in the York River Estuary sampled in 2019-2021. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2025-09-23 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.962507.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>Watershed carbon concentrations Dataset Description:  Methods and Sampling: &amp;lt;p&amp;gt;Three of the four stations were accessed by land.&amp;amp;nbsp; The two USGS gauge sites (Pamunkey Gauge, PG; Mattaponi Gauge, MG) were sampled by lowering a bucket from the bridges crossing the rivers at the gauge locations. &amp;amp;nbsp;The other site (Walkerton Landing Bridge, WLB) was sampled from a floating dock.&amp;amp;nbsp; The White House station (WH) was not accessible from the road; this station is a long-term monitoring site of the Chesapeake Bay National Estuarine Research Reserve in Virginia (CBNERRVA) and was sampled for us by CBNERRVA staff.&amp;amp;nbsp; Sample dates were the same except for two dates when WH was sampled one day before or after the other sites.&amp;amp;nbsp; Samples were collected from the surface at all stations.&amp;amp;nbsp; Water temperature and salinity were measured in the field with a YSI EXO2 datasonde.&amp;amp;nbsp; Carbon samples were collected in triplicate and filtered immediately in the field at PG, MG, and WLB; samples from WH were kept on ice and returned to the lab for filtration.&amp;amp;nbsp; DIC samples were filtered through 0.2 um polycarbonate filters into 8-mL hungate tubes and refrigerated underwater until analysis on an Apollo SciTech AS-C3 analyzer coupled to a LI-COR LI-7000 infrared gas analyzer.&amp;amp;nbsp; DOC samples were filtered through 0.45 um polyethersulfone filters and frozen prior to analysis on a Shimadzu TOC-V organic carbon analyzer.&amp;amp;nbsp; POC samples were filtered onto pre-combusted 0.7 um glass fiber filters, dried at 60°C, and stored in a dessicator prior to analysis. &amp;amp;nbsp;Beginning in August 2019, samples were fumed with HCl to remove any inorganic carbon.&amp;amp;nbsp; Samples through June 2019 were measured on a Thermo 1110 CHN Analyzer; subsequent samples were measured on a Costech 4010 CHN Analyzer.&amp;amp;nbsp; A series of blank filters were also measured to correct for background POC concentrations.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/747587.rdf" xlink:title="OCE-1737258" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1737258 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1737258</gmx:Anchor>
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Estuaries, coastal water bodies where rivers mix with ocean water, are hotspots for the processing of carbon and nutrients moving from land to the coastal ocean. Within estuaries land-based nutrient inputs can cause intense blooms of single-celled algae called phytoplankton, which can have significant impacts on the ecosystem. As blooms move down-estuary some of the phytoplankton material is buried on the bottom, and some is decomposed, resulting in low oxygen conditions (hypoxia), harmful to marine life, and production of carbon dioxide (CO2), the major greenhouse gas, which can exchange with the atmosphere. The remaining phytoplankton material can be exported to the ocean. The type and amount of carbon exported from the estuary depend both on its biological activity and physical factors such as fresh water discharge, temperature, and light availability. If phytoplankton production is greater than decomposition, the estuary will take up atmospheric CO2 and export phytoplankton carbon to the coastal ocean. On the other hand, if decomposition is greater than production the estuary will be a source of CO2 to the atmosphere and dissolved CO2 to the coastal ocean. The investigators expect that intense phytoplankton blooms will greatly amplify carbon exchanges with the atmosphere, coastal ocean, and bottom sediments. As intense phytoplankton blooms increase in the future due to increased nutrient inputs and temperature, low oxygen events may become more frequent with potential negative impacts on fisheries and increased export of carbon to the coastal ocean and atmosphere. This study will fill critical gaps identified by the Coastal Carbon Synthesis Program in knowledge of how microtidal estuaries transform and export C to the atmosphere, benthos, and coastal ocean. In addition, there will be a strong teaching and training component to this project, with support for graduate and undergraduate students. The graduate student will be partnered with secondary teachers to gain teaching experience and enrich the middle school educational programs. Summer undergraduate interns will be recruited for a summer program from Hampton University, a historically Black college. There will be public outreach through participation in existing programs at VIMS.&lt;/p&gt;
&lt;p&gt;Estuaries serve as critical hotspots for the processing of carbon (C) as it transits from land to the coastal ocean. Recent attempts to synthesize what is known about sources and fates of C in estuaries have noted large data gaps; thus, the role of estuaries, especially those that are microtidal, as important sources of carbon dioxide (CO2) to the atmosphere and total organic carbon (TOC) and dissolved inorganic carbon (DIC) to the coastal ocean, or as a C sink in bottom sediments, remains uncertain. Intensive phytoplankton blooms are becoming increasingly frequent in many estuaries and are likely to have important and yet unknown impacts on the C cycle. The trophic status of an estuary will determine in large part the species of C exported to the atmosphere, bottom sediments, and coastal ocean. The overarching objective of this project is to identify the impacts of intense phytoplankton blooms on C speciation, net C fluxes and exchanges in the Lower York River Estuary (LYRE), a representative mesotrophic, microtidal mid-Atlantic estuary. Metabolic processes are hypothesized to be spatially and temporally dynamic, driving the speciation, abundance, and fates of C in the LYRE. High spatiotemporal resolution sampling in the LYRE will capture rates of C cycling under both baseline conditions throughout most of the year, and during periods when the estuary is perturbed by widespread and intense, but patchy, late summer phytoplankton blooms. The short-term effects of physical drivers (wind, temperature, salinity, fresh water discharge, nutrient and organic carbon loads) and biological drivers (metabolic rates, bacterial and phytoplankton abundances and composition) on C transformations, speciation, and exchanges will be assessed. Expected longer term variations in the C cycle due to anthropogenic and natural disturbances will be predicted through use of modeling. In addition, laboratory manipulations will examine the impacts of specific organisms dominating intensive phytoplankton blooms on benthic metabolism, processing of organic C by the microbial community, and C fluxes to the water column.&lt;/p&gt;</gco:CharacterString>
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            <gco:CharacterString>PI Supplied Instrument Name: Shimadzu TOC-V organic carbon PI Supplied Instrument Description:DOC concentrations were measured on a Shimadzu TOC-V organic carbon analyzer.  Instrument Name: Shimadzu TOC-V Analyzer Instrument Short Name:Shimadzu TOC-V   Instrument Description: A Shimadzu TOC-V Analyzer measures DOC by high temperature combustion method. Community Standard Description: http://onto.nerc.ac.uk/CAST/124</gco:CharacterString>
          </gmi:description>
        </gmi:MI_Instrument>
      </gmi:instrument>
      <gmi:instrument>
        <gmi:MI_Instrument>
          <gmi:identifier>
            <gmd:MD_Identifier>
              <gmd:code>
                <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/instrument/768595.rdf" xlink:title="YSI EXO multiparameter water quality sondes" xlink:actuate="onRequest">YSI EXO2</gmx:Anchor>
              </gmd:code>
            </gmd:MD_Identifier>
          </gmi:identifier>
          <gmi:type>
            <gco:CharacterString>YSI EXO2</gco:CharacterString>
          </gmi:type>
          <gmi:description>
            <gco:CharacterString>PI Supplied Instrument Name: YSI EXO2 PI Supplied Instrument Description:Water temperature and salinity were measured with a YSI EXO2 datasonde.  Instrument Name: YSI EXO multiparameter water quality sondes Instrument Short Name:YSI EXO   Instrument Description: Comprehensive multi-parameter, water-quality monitoring sondes designed for long-term monitoring, profiling and spot sampling. The EXO sondes are split into several categories: EXO1 Sonde, EXO2 Sonde, EXO3 Sonde. Each category has a slightly different design purpose with the EXO2 and EXO3 containing more sensor ports than the EXO1. Data are collected using up to four user-replaceable sensors and an integral pressure transducer. Users communicate with the sonde via a field cable to an EXO Handheld, via Bluetooth wireless connection to a PC, or a USB connection to a PC. Typical parameter specifications for relevant sensors include dissolved oxygen with ranges of 0-50 mg/l, with a resolution of +/- 0.1 mg/l, an accuracy of 1 percent of reading for values between 0-20 mg/l and an accuracy of +/- 5 percent of reading for values 20-50 mg/l. Temp ranges are from-5 to +50 degC, with an accuracy of +/- 0.001 degC. Conductivity has a range of 0-200 mS/cm, with an accuracy of +/-0.5 percent of reading + 0.001 mS/cm and a resolution of 0.0001 - 0.01 mS/cm.</gco:CharacterString>
          </gmi:description>
        </gmi:MI_Instrument>
      </gmi:instrument>
      </gmi:MI_AcquisitionInformation>
  </gmi:acquisitionInformation>
</gmi:MI_Metadata>
