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        <gco:CharacterString>Doliolid Distribution Synthesis Dataset Description: &amp;lt;p&amp;gt;This dataset is a synthesis of doliolid imagery and oceanographic data from six ecosystems collected from multiple research cruises conducted between 2010 and 2019. The data are organized into the following folders/files:&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;1.DoliolidAbundances-All – This folder contains the calculated concentrations and average oceanographic variables in each bin from both automated (using computer vision) and manually verified data.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;2. DoliolidEnvironment-Automated – This folder contains the raw data from the different ecosystems generated with computer vision algorithms where each row is an individual doliolid and all of the oceanographic parameters associated with it.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;3. DoliolidEnvironment-Manual – This folder contains the manually verified doliolid identifications in the Gulf of Mexico and Southern California. Southern California had individual &amp;quot;casts&amp;quot; analyzed, so the times for these chunks of data are also contained in this folder&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;4. GulfofMexicoDoliolidImages-ManuallyClassified – This folder contains actual images identified to 3 different life stages of doliolids from the northern Gulf of Mexico.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;5. GulfPhysicalOceanographicData – This folder contains oceanographic sensor data from the towed imaging system, as well as linearly interpolated data used to make plots of the doliolid distributions in the paper.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;6. LiteratureReview-PSEM – This folder contains a compilation of data from two open-access databases used to make some calculations in the published manuscript. The folder also contains the data frame used to run the piecewise structural equation models (PSEM).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;7. R-Scripts – This folder contains the R-scripts used to conduct all analyses synthesizing these datasets&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;8. DolTransectLocations.csv&amp;amp;nbsp;– This file&amp;amp;nbsp;contains the Start and Stop latitudes and longitudes for all of the transects analyzed in the manuscript. This was used to generate the map in the manuscript. BCO-DMO converted this file from Microsoft Excel format to .csv.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The Supplemental File named &amp;quot;File_Descriptions.pdf&amp;quot; contains additional details on each file within each folder.&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;All methods below are excerpted from Greer et al. (2022). Please refer to the publication for a more complete description of the data collection and analysis methods.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Imaging system and field sampling:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
All high-resolution images were collected with a towed In Situ Ichthyoplankton Imaging System (ISIIS, Cowen and Guigand 2008). The ISIIS uses shadowgraph lighting and a line-scan camera (Teledyne DALSA) to image water with a 13 cm field of view over a depth of field of 50 centimeters. The system is towed at a speed of approximately 2.5 meters per second, using motor-controlled wings to undulate between about 1 meter from the surface and a maximum depth of about 120 meters (or 2–4 m from the benthos) in a &amp;quot;tow-yo&amp;quot; pattern. The camera scans approximately 35,000 pixel lines per second, producing a continuous strip of imaged ocean water that is parsed by acquisition software into 2048 px by 2048 px images (~17 Hz). The instrument is equipped with various oceanographic sensors, including conductivity, temperature, depth (SBE 49, Seabird Electronics), chlorophyll-a fluorescence (ECO FL-RT), and dissolved oxygen (SBE 43) to measure oceanographic conditions associated with each image. Transects were conducted in six different ecosystems (the Oregon shelf, northern California, southern California Bight, northern Gulf of Mexico, Straits of Florida, and Mediterranean Sea) and used similar towing methods (refer to Figure 1 of Greer et al., 2022)&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;To compare data among sampling sites, abundances and associated oceanographic data were summed or averaged over a consistent volume sampled. For organism counts, both stage-specific and total doliolids were summed across 7-second bins, which corresponded to approximately 1 cubic meter of imaged water. The oceanographic variables were also averaged over this volume. We were interested in doliolids and their different life stages: nurses, phorozooids, and gonozooids, all of which are relatively easy to distinguish.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;To evaluate the spatial changes in the accuracy of the automatically generated abundances for these three life stages, we leveraged a human-annotated dataset from the northern Gulf of Mexico. This matched the life stages classified in the automated datasets for a more robust comparison. These manual identifications were binned using the same procedure as the automated data.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Mean carbon biomass:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
We computed the mean carbon biomass of doliolids within the shallowest 100 m for all sites. Doliolid carbon biomass in cubic meters was then calculated using the average concentration of individuals in the upper 100 meters in each sampling region multiplied by the average individual weight.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Statistical analyses and modeling&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Data binning, summary statistics, and visualizations were performed in R (R Core Team 2019, v.3.6.1), with extensive use of the packages ggplot2, reshape2, and plyr (Wickham 2016). Patchiness or degree of aggregation was quantified using the Lloyd index of patchiness (Bez 2000).&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/859629.rdf" xlink:title="OCE-2023133" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-2023133 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=2023133</gmx:Anchor>
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                <gco:CharacterString>&amp;lt;p&amp;gt;All methods below are excerpted from Greer et al. (2022). Please refer to the publication for a more complete description of the data collection and analysis methods.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Imaging system and field sampling:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
All high-resolution images were collected with a towed In Situ Ichthyoplankton Imaging System (ISIIS, Cowen and Guigand 2008). The ISIIS uses shadowgraph lighting and a line-scan camera (Teledyne DALSA) to image water with a 13 cm field of view over a depth of field of 50 centimeters. The system is towed at a speed of approximately 2.5 meters per second, using motor-controlled wings to undulate between about 1 meter from the surface and a maximum depth of about 120 meters (or 2–4 m from the benthos) in a &amp;quot;tow-yo&amp;quot; pattern. The camera scans approximately 35,000 pixel lines per second, producing a continuous strip of imaged ocean water that is parsed by acquisition software into 2048 px by 2048 px images (~17 Hz). The instrument is equipped with various oceanographic sensors, including conductivity, temperature, depth (SBE 49, Seabird Electronics), chlorophyll-a fluorescence (ECO FL-RT), and dissolved oxygen (SBE 43) to measure oceanographic conditions associated with each image. Transects were conducted in six different ecosystems (the Oregon shelf, northern California, southern California Bight, northern Gulf of Mexico, Straits of Florida, and Mediterranean Sea) and used similar towing methods (refer to Figure 1 of Greer et al., 2022)&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;To compare data among sampling sites, abundances and associated oceanographic data were summed or averaged over a consistent volume sampled. For organism counts, both stage-specific and total doliolids were summed across 7-second bins, which corresponded to approximately 1 cubic meter of imaged water. The oceanographic variables were also averaged over this volume. We were interested in doliolids and their different life stages: nurses, phorozooids, and gonozooids, all of which are relatively easy to distinguish.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;To evaluate the spatial changes in the accuracy of the automatically generated abundances for these three life stages, we leveraged a human-annotated dataset from the northern Gulf of Mexico. This matched the life stages classified in the automated datasets for a more robust comparison. These manual identifications were binned using the same procedure as the automated data.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Mean carbon biomass:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
We computed the mean carbon biomass of doliolids within the shallowest 100 m for all sites. Doliolid carbon biomass in cubic meters was then calculated using the average concentration of individuals in the upper 100 meters in each sampling region multiplied by the average individual weight.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Statistical analyses and modeling&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Data binning, summary statistics, and visualizations were performed in R (R Core Team 2019, v.3.6.1), with extensive use of the packages ggplot2, reshape2, and plyr (Wickham 2016). Patchiness or degree of aggregation was quantified using the Lloyd index of patchiness (Bez 2000).&amp;lt;/p&amp;gt;</gco:CharacterString>
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                <gco:CharacterString>&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Data Processing:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Doliolids were enumerated manually in the images, or they were identified automatically using different versions of a convolutional neural network. All data were analyzed and processed in R (v.3.6.1) using a variety of packages detailed in the accompanying code.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;BCO-DMO Processing:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
- BCO-DMO converted &amp;quot;DolTransectLocations.xlsx&amp;quot; to .csv format and changed the stop longitude values for San Diego to be negative.&amp;lt;/p&amp;gt;</gco:CharacterString>
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                <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/instrument/655602.rdf" xlink:title="In Situ Ichtyoplankton Imaging System" xlink:actuate="onRequest">In situ Ichthyoplankton Imaging System (ISIIS)</gmx:Anchor>
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            <gco:CharacterString>In situ Ichthyoplankton Imaging System (ISIIS)</gco:CharacterString>
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            <gco:CharacterString>PI Supplied Instrument Name: In situ Ichthyoplankton Imaging System (ISIIS) PI Supplied Instrument Description:In situ Ichthyoplankton Imaging System (ISIIS), which includes a camera system with a 13 centimeter (cm) field of view and 50 cm depth of field. The camera scans approximately 35,000 pixel (px) lines per second, producing a continuous strip of imaged ocean water that is parsed by acquisition software into 2048 px by 2048 px images (~17 Hz). The instrument is equipped with various oceanographic sensors, including conductivity, temperature, depth (SBE 49, Seabird Electronics), chlorophyll-a fluorescence (ECO FL-RT), and dissolved oxygen (SBE 43) to measure oceanographic conditions associated with each image. Instrument Name: In Situ Ichtyoplankton Imaging System Instrument Short Name:ISIIS   Instrument Description: The In Situ Ichthyoplankton Imaging System (ISIIS) is an underwater imaging system aimed at capturing in situ, real time images of marine zooplankton of relatively low abundance such as fish larvae and fragile gelatinous organisms. The first prototype, delivered in 2007, was attached to a relatively simple vehicle towed by an oceanographic vessel at a speed of five knots. The vehicle, and associated imaging system and sensors, was moved up and down through the water column by paying cable in and out via an oceanographic winch. Subsequently, a new vehicle has been designed with the capacity of self undulation using motor actuated dive fins. 

The ISIIS system utilizes a high-resolution line-scanning camera with a Light Emitting Diode (LED) light source, modified by plano-convex optics, to create a collimated light field to back-light a parcel of water.

ISIIS was developed in collaboration between the University of Miami's Rosenstiel School of Atmospheric and Marine Science (RSMAS) and the subsea engineering company, Bellamare, LLC, located in San Diego CA. See complete description from RSMAS.

Reference:
Cowen RK and Guigand CM. 2008. In situ Ichthyoplankton Imaging System (ISIIS): system design and preliminary results. Limnol. Oceanogr. Methods. 6:126-132. doi:10.4319/lom.2008.6.126</gco:CharacterString>
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