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            <gco:CharacterString>Cite this dataset as: Crotteau, M., Raven, M. R., Martinez, A., Evans, N., Karagiannis, M., Fishburn, J., Neibauer, J. A. (2026) Porewater geochemistry data from sediment cores collected on R/V Rachel Carson cruise RC0107 in Clayoquot Sound, Vancouver Island, British Columbia during October 2023. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2026-01-21 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.992752.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>Porewater geochemistry Dataset Description: &amp;lt;p&amp;gt;This dataset is one of three datasets presenting marine biogeochemistry data from four sites in Clayoquot Sound, Vancouver Island, British Columbia from water, sediment, and porewater samples that were collected aboard the R/V Rachel Carson in October 2023. These sites were selected because they represent hotspots of organic carbon burial spanning a range of geochemical conditions. They represent a range of oxic to historically anoxic water columns, and receive organic matter inputs varying from predominantly terrestrial to predominantly marine sources. Together, these datasets provide a framework to evaluate the controls and drivers of organic matter preservation in fjord sediments. See the &amp;quot;Related Datasets&amp;quot; section for the other datasets.&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;Three sediment cores were collected at each of three sites in Clayoquot Sound, Vancouver Island, Canada in October 2023. One core was used for porewater sampling; this core was sampled immediately with Rhizon samplers. A second core was extruded under argon for geochemical measurements. (See &amp;quot;Related Datasets&amp;quot; for the sediment geochemical data.) 1 milliliter (mL) of sediment was added to a cryovial and frozen at -20 degrees Celsius (°C) for future DNA extraction. 5 mL of sediment was added to an exetainer containing 5 mL of 1 N NaOH to measure sediment methane concentrations. The remaining sediment from each extruded interval was added immediately to falcon tubes containing 10 mL of 20% zinc acetate to precipitate sulfides and halt microbial activity. A third archive core was immediately frozen at -20°C.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Porewater samples from each core were aliquoted to measure pH and the concentrations of dissolved Fe(II), sulfate, and sulfide. pH was determined using the dye meta-cresol purple via a UV-Vis spectrophotometer (Genesys 150) (Clayton and Byrne 1993). Fe(II) was determined using a ferrozine assay (Jeitner 2014). Sulfate was measured via ion chromatography (Metrohm 930 Compact IC Flex). Sulfide was precipitated as zinc sulfide in the field by adding 4 mL of porewater to 4 mL of sparged 20% zinc acetate solution. To avoid sulfate contamination, porewater zinc sulfide samples were subjected to a strong acid hydrolysis (6 N HCl, 60°C, 2 hours) under N₂ to volatilize zinc sulfides; sulfide was trapped as zinc sulfide in 5% zinc acetate solution, oxidized to sulfate with 30% H₂O₂, and measured via ion chromatography (Metrohm 930 Compact IC Flex).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Samples analyzed in this study were collected within Ahousaht Territory, on the west coast of Vancouver Island, British Columbia. We respectfully acknowledge the Ahousaht Nation and the Maaqutusiis Hahoulthee Stewardship Society for their stewardship of these lands and for the opportunity to conduct research within their territory.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/920982.rdf" xlink:title="OCE-2143817" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-2143817 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=2143817</gmx:Anchor>
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&lt;p&gt;Areas of the ocean without dissolved oxygen are called anoxic zones. These environments are increasing due to human activities and climate change. Large amounts of organic carbon are buried in sediments below anoxic zones. However, we do not fully understand why organic carbon is preserved in these zones. This project seeks to understand a newly discovered process that may contribute to carbon preservation in anoxic zones. The process is called organic matter sulfurization. Through this process, organic matter is transformed and effectively 'pickled' by reacting with sulfide. Rapid sulfurization reactions were identified for the first time in sinking marine particles and may have larger effect on carbon burial in sediments than previously thought. This project will be the first to provide measurements of the scale and significance of rapid organic matter sulfurization in modern anoxic zones. This project includes field and laboratory studies. The research will involve a team of students, including a graduate student and six undergraduates, who will be supported through a peer mentorship program. Undergraduate researchers will be recruited from the inaugural class of a newly developed Practical Research Skills course (Earth 101A) at the University of California Santa Barbara. It seeks to help undergraduates develop critical thinking and observational skills that have broad applicability. This project will launch a self-sustaining and vigorous research program in marine biogeochemistry, heavily invested in undergraduate research education, with impacts that will outlast its five-year duration.&lt;/p&gt;
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&amp;lt;p&amp;gt;Samples analyzed in this study were collected within Ahousaht Territory, on the west coast of Vancouver Island, British Columbia. We respectfully acknowledge the Ahousaht Nation and the Maaqutusiis Hahoulthee Stewardship Society for their stewardship of these lands and for the opportunity to conduct research within their territory.&amp;lt;/p&amp;gt;</gco:CharacterString>
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