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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/1009817.rdf" xlink:actuate="onRequest">Results of a study examining how foundation species loss alters fDOM and heterotrophic bacteria counts based on sampling of tidepools in the Otter Rock Marine Reserve (ORMR) and Marine Garden, Oregon USA from June to August 2019</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Silbiger, N., Fields, J., Nelson, C. E., Wegley Kelly, L. (2026) Results of a study examining how foundation species loss alters fDOM and heterotrophic bacteria counts based on sampling of tidepools in the Otter Rock Marine Reserve (ORMR) and Marine Garden, Oregon USA from June to August 2019. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2026-10-13 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.1009817.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>Methods and Sampling: &amp;lt;p&amp;gt;&amp;amp;nbsp;fDOM samples were stored in amber glass vials at 4 °C until further processing. Heterotrophic bacterial counts were taken from 1.5 mL unfiltered seawater and stored in 0.5% paraformaldehyde (amended with 100 μL 8% ampulated paraformaldehyde, Electron MicroscopySciences, Hatfield, PA, USA) in a 2 mL polypropylene cryovial, mixed briefly and then frozen to -20 °C. All storage vials were triple rinsed with sample water prior to sample storage. fDOM samples were processed on a Horiba Aqualog scanning fluorometer with 1 cm quartz cuvettes at the University of Hawai’i at Mānoa following Nelson et al. (2015).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;All samples were brought to room temperature prior to analysis. Prior to running samples, cuvettes were washed thoroughly with DI water and wiped clear with Kim wipes. Cuvettes were triple rinsed with DI between each sample. A DI blank was run after every 7 samples. Excitation-Emission Matrices (EEMS) were generated with excitation values ranging from 240 nm to 500 nm and emission values were measured ranging from 250 nm to 825 nm.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Excitation wavelengths were increased at 5 nm increments and measurements were integrated over 4 s at each increment. Inner filter correction was applied to account for fluorescence quenching by absorbance (Kothawala &amp;lt;em&amp;gt;et al.&amp;lt;/em&amp;gt; 2013). Fluorescence values were scaled to Raman Units by dividing by the integrated emission range of 381 nm to 426 nm at an excitation of 350 nm in averaged DI blanks. The average blank EEMs, from DI blanks run immediately before and after each set of samples, were subtracted from the sample EEMs.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Two biogeochemical informative indices were calculated for this study which included M:C (the relative amount of marine to terrestrial humics) (Burdige &amp;lt;em&amp;gt;et al.&amp;lt;/em&amp;gt; 2004) and BIX (biological index) (Huguet &amp;lt;em&amp;gt;et al.&amp;lt;/em&amp;gt; 2009). Heterotrophic bacterial counts were analyzed using flow cytometry on an Attune Acoustic Focusing Cytometer with Autosampler Attachment (Life Technologies, Eugene, OR, USA) with methods following Nelson et al. (2015)&amp;lt;em&amp;gt;.&amp;lt;/em&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Flow cytometry samples were analyzed on fixed 1ml samples run on a Cytoflex Flow Cytometer stained with 7 μL of 40 μL mL&amp;lt;sup&amp;gt;−1&amp;lt;/sup&amp;gt; Hoechst 34580 (1 μg mL&amp;lt;sup&amp;gt;−1&amp;lt;/sup&amp;gt; , final concentration) following standard protocols (Nelson &amp;lt;em&amp;gt;et al.&amp;lt;/em&amp;gt; 2015; Selph 2021)&amp;lt;em&amp;gt;.&amp;lt;/em&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Stained cells were distinguished from instrument noise using stained and unstained blank water, and autofluorescent cells containing phytopigments were subtracted from the total to derive the subset of heterotrophic bacterioplankton.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/876575.rdf" xlink:title="OCE-2044837" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-2044837 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=2044837</gmx:Anchor>
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&lt;p&gt;The devastating impacts of global warming and ocean acidification (OA) on rocky intertidal ecosystems are expected to increase as the oceans continue to warm and acidify. Further, loss of critical foundation species as a result of anthropogenic stressors lead to changes in local conditions that alter ecosystem functioning. While data exist on the physiological response of individual organisms to OA and warming in rocky systems, far less research has been conducted on community and ecosystem-scale metabolic responses. The proposed work provides a critical step in understanding how altered environmental conditions affect ecosystem functioning in rocky intertidal systems through the combination of controlled laboratory studies, field experiments, and a synthetic modeling approach integrating experimental results with pre-existing time-series data. The proposed work is focused on the overarching question: How does shifting environmental variability and loss of foundation species interact to affect ecosystem functioning in rocky intertidal communities? The PI is integrating research with ecological and quantitative educational opportunities including classroom and hands-on training in lab/field methods in marine ecology, and data science and coding bootcamps for undergraduate students. Importantly, these opportunities financially and educationally support traditionally underrepresented students at one of the largest minority-serving institutions in the country. This project provides support for intensive mentoring and training for 35 undergraduate students (25 in data science and 10 in field/lab science, all paid), 2-3 masters students, and hands-on marine ecology opportunities in the classroom (~125 students). In addition to formal education, the PI is collaborating with an artist-in-residence to communicate science to the broader public through interactive and immersive art installations in Los Angeles.&lt;/p&gt;
&lt;p&gt;Because rocky intertidal systems provide important ecosystem services including food production, coastal protection, and tourism, it is critical to understand how warming (both air and ocean), acidification, and altered community states affect reef-scale ecosystem metabolism. While information exists on responses of a variety of individual intertidal taxa to temperature stress, ocean acidification, and habitat loss, there is notably less on the response of ecosystem metabolism (e.g. NEP and NEC) to these stressors. This proposed work is focused on a series of conceptual knowledge gaps and tests mechanisms through which different warming regimes, lowered pH, and community disturbance lead to altered community metabolism and ultimately affect ecosystem function. Specifically, this study: 1) Describes community thermal performance curves of multiple ecosystem functions under differing pH conditions in experimental mesocosms, 2) characterizes drivers of ecosystem functioning (e.g. Net Ecosystem Production [NEP] and Net Ecosystem Calcification [NEC]) in situ using natural changes in environmental variability before and after a disturbance, and 3) integrates 16 years of publicly available community composition and environmental time-series data with lab and field data to hindcast ecosystem metabolic rates and predict how ecosystem metabolism may change in the future.&lt;/p&gt;
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                <gco:CharacterString>&amp;lt;p&amp;gt;&amp;amp;nbsp;fDOM samples were stored in amber glass vials at 4 °C until further processing. Heterotrophic bacterial counts were taken from 1.5 mL unfiltered seawater and stored in 0.5% paraformaldehyde (amended with 100 μL 8% ampulated paraformaldehyde, Electron MicroscopySciences, Hatfield, PA, USA) in a 2 mL polypropylene cryovial, mixed briefly and then frozen to -20 °C. All storage vials were triple rinsed with sample water prior to sample storage. fDOM samples were processed on a Horiba Aqualog scanning fluorometer with 1 cm quartz cuvettes at the University of Hawai’i at Mānoa following Nelson et al. (2015).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;All samples were brought to room temperature prior to analysis. Prior to running samples, cuvettes were washed thoroughly with DI water and wiped clear with Kim wipes. Cuvettes were triple rinsed with DI between each sample. A DI blank was run after every 7 samples. Excitation-Emission Matrices (EEMS) were generated with excitation values ranging from 240 nm to 500 nm and emission values were measured ranging from 250 nm to 825 nm.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Excitation wavelengths were increased at 5 nm increments and measurements were integrated over 4 s at each increment. Inner filter correction was applied to account for fluorescence quenching by absorbance (Kothawala &amp;lt;em&amp;gt;et al.&amp;lt;/em&amp;gt; 2013). Fluorescence values were scaled to Raman Units by dividing by the integrated emission range of 381 nm to 426 nm at an excitation of 350 nm in averaged DI blanks. The average blank EEMs, from DI blanks run immediately before and after each set of samples, were subtracted from the sample EEMs.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Two biogeochemical informative indices were calculated for this study which included M:C (the relative amount of marine to terrestrial humics) (Burdige &amp;lt;em&amp;gt;et al.&amp;lt;/em&amp;gt; 2004) and BIX (biological index) (Huguet &amp;lt;em&amp;gt;et al.&amp;lt;/em&amp;gt; 2009). Heterotrophic bacterial counts were analyzed using flow cytometry on an Attune Acoustic Focusing Cytometer with Autosampler Attachment (Life Technologies, Eugene, OR, USA) with methods following Nelson et al. (2015)&amp;lt;em&amp;gt;.&amp;lt;/em&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Flow cytometry samples were analyzed on fixed 1ml samples run on a Cytoflex Flow Cytometer stained with 7 μL of 40 μL mL&amp;lt;sup&amp;gt;−1&amp;lt;/sup&amp;gt; Hoechst 34580 (1 μg mL&amp;lt;sup&amp;gt;−1&amp;lt;/sup&amp;gt; , final concentration) following standard protocols (Nelson &amp;lt;em&amp;gt;et al.&amp;lt;/em&amp;gt; 2015; Selph 2021)&amp;lt;em&amp;gt;.&amp;lt;/em&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Stained cells were distinguished from instrument noise using stained and unstained blank water, and autofluorescent cells containing phytopigments were subtracted from the total to derive the subset of heterotrophic bacterioplankton.&amp;lt;/p&amp;gt;</gco:CharacterString>
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- Converted sampling_day to a date formatted as %Y-%m-%d and sampling_time to a time formatted as %H:%M:%S. Renamed these fields to sampling_date and sampling_time_local, respectively.
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- Removed the intermediate taxon_level, status, and rand columns and finalized the column order and data types.
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Calibration: Instrument performance was verified using the manufacturer's daily quality control (QC) procedures with fluorescent calibration beads according to Beckman Coulter recommendations prior to sample analysis.
  Instrument Name: Flow Cytometer Instrument Short Name:Flow Cytometer   Instrument Description: Flow cytometers (FC or FCM) are automated instruments that quantitate properties of single cells, one cell at a time. They can measure cell size, cell granularity, the amounts of cell components such as total DNA, newly synthesized DNA, gene expression as the amount messenger RNA for a particular gene, amounts of specific surface receptors, amounts of intracellular proteins, or transient signalling events in living cells. Description from: http://www.bio.umass.edu/micro/immunology/facs542/facswhat.htm Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/LAB37/</gco:CharacterString>
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