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            <gco:CharacterString>Cite this dataset as: Roche, K. M., Church, I., Sterling, A., Rynearson, T. A., Bertin, M., Kim, A., Kirk, R., Jenkins, B. D. (2024) Amplicon sequence variants (ASVs) and taxonomy of Pseudo-nitzschia spp. from Narragansett Bay in Rhode Island, USA and the Northeast U.S. Shelf (NES-LTER transect) from 2018-2023. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2024-10-11 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.936849.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>Dataset Description: &amp;lt;p&amp;gt;Acknowledgement:&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;We acknowledge the NSF RI C-AIM EPSCoR Cooperative Agreement (OIA-1004057) for research support. Sequencing was performed at the University of Rhode Island Molecular Informatics Core supported by the Institutional Development Award (IDeA) Network for Biomedical Research Excellence from the National Institute of General Medical Sciences of the National Institutes of Health (P20GM103430).&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;Samples were selected from the NES-LTER transect and various time series sites in &amp;lt;/span&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0); font-family:helvetica,arial,sans-serif; font-size:14.4px&amp;quot;&amp;gt;Narragansett Bay, Rhode Island (&amp;lt;/span&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;NB) during winter and summer periods from January 2018 through February 2023 to compare seasonal and regional patterns of &amp;lt;em&amp;gt;Pseudo-nitzschia&amp;lt;/em&amp;gt; species composition and DA, as well as environmental drivers. NB and NES will henceforth be referred to as subregions of the larger Northeast U.S. Continental Shelf region, with NES specifically referring to the area spanned by the NES-LTER transect. Samples were collected on NES-LTER cruises (&amp;lt;em&amp;gt;R/V&amp;lt;/em&amp;gt; Endeavor, &amp;lt;em&amp;gt;R/V&amp;lt;/em&amp;gt; Atlantis) from 11 stations along a 150 km transect (n=77) each winter (January-February) and summer (July-August). Samples from three to four stations per cruise were used in this dataset spanning innershelf (L1), midshelf (L3, L4) and outershelf (L7, L8, L10) sections of the transect. The northernmost station, L1, is about 50 km from the mouth of NB. To collect plankton biomass for nucleic acid isolation, CTD rosette seawater from the surface and subsurface chlorophyll maximum (SCM) were passed via peristaltic pump over 25 mm 5 µm pore size filters (Sterlitech, Kent, WA, USA). Biomass filters were either flash frozen in liquid nitrogen (2018-2022) or placed in DNA/RNA shield (winter 2023; Zymo Research, Irvine, CA, USA) and stored in a -80°C freezer. The SCM depth varied as observed by &amp;lt;em&amp;gt;in situ&amp;lt;/em&amp;gt; chlorophyll fluorescence, with a median depth of 28 m for summer and 19 m for winter samples. In cases where the SCM was not well defined due to water column mixing that typically took place in winter at nearshore stations, a sampling depth between 20 and 30 m was targeted.&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;In NB, surface seawater samples were collected from various sites in the East and West Passages including the Narragansett Bay Long-Term Plankton Time Series (NBPTS) site, Whale Rock (WR), Castle Hill Beach (CHB), East Passage (EP), and University of Rhode Island Graduate School of Oceanography (GSO) dock. Seawater was transported back to the laboratory and passed over 25 mm 5 µm pore size filters (Sterlitech, Kent, WA, USA) using a peristaltic pump before flash freezing in liquid nitrogen and storage at -80°C. To fill in several missing dates from this time series, six samples collected separately in the NBPTS (https://web.uri.edu/gso/research/plankton/) sampling program were used. These samples differed in collection methodology only by the filter pore size used (0.22 µm, Express Plus, Millipore Sigma) and vacuum as opposed to peristaltic filtration.&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;DNA was extracted from most NB and NES samples (n=219) using a modified version of the DNeasy Plant Kit (Qiagen, Germantown, MD, USA) that included a 1-minute bead beating step (0.1 mm and 0.5 mm Zirconia/Silica beads, BioSpec Products, Bartlesville, OK, USA) and two part elution into a total of 45 µL Buffer AE. Similarly, the six NBPTS samples were extracted using a modified version of the DNeasy Blood &amp;amp;amp; Tissue kit (Qiagen, Germantown, MD, USA) with a 1-minute bead beating step and final elution into 50 µL Buffer AE. Some NES samples (n=18) were extracted using the Quick-DNA/RNA Miniprep Plus Kit (Zymo Research, Irvine, CA, USA) with a 1-minute bead beating step (0.4 mm Zirconium Beads, OPS Diagnostics, Lebanon, NJ, USA) and final elution into 50 µL nuclease-free water. DNA from each sample was amplified with a primer set that targets the eukaryotic internal transcribed spacer region 1 (ITS1) and effectively distinguishes &amp;lt;em&amp;gt;Pseudo-nitzschia&amp;lt;/em&amp;gt; species (White et al., 1990; Sterling et al., 2022). Briefly, DNA was diluted to 1-4 ng/µL and 2 µL of template was added to 25 µL PCR reactions with Phusion Hot Start High-Fidelity Master Mix (Thermo Fisher Scientific Inc., Waltham, MA, USA) and HPLC-purified forward and reverse primers at 0.5 µM concentration with Illumina MiSeq adapters (Integrated DNA Technologies, Coralville, IA, USA). A stepwise thermocycle was used as described in Sterling et al. (2022).&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;DNA amplicons were sequenced at the Rhode Island-INBRE Molecular Informatics Core on the Illumina MiSeq platform (Illumina, Inc., San Diego, CA, USA). There, libraries were prepared by cleaning ITS1 PCR products with KAPA pure beads (KAPA Biosystems, Woburn, MA, USA) and attaching sequencing indices and adapters using PCR. This amplification was performed with the Illumina Nextera XT Index Kit (Illumina, San Diego, CA, USA) and Phusion High Fidelity Master Mix, followed by a second round of cleaning with KAPA pure beads and visualization with gel electrophoresis. The quality of select samples was assessed on a Bioanalyzer DNA1000 chip (Agilent Technologies, Santa Clara, CA, USA) and all samples were quantified on a Qubit fluorometer (Invitrogen, Carlsbad, CA, USA). The final library was pooled, quantified with qPCR on a LightCycler480 (Roche, Pleasanton, CA, USA) using a KAPA Biosystems Illumina Kit (KAPA Biosystems, Woburn, MA, USA), and sequenced on the Illumina MiSeq using v3 chemistry and 2x250 paired-end reads. Samples were sequenced across five separate MiSeq runs using identical methods and negative controls.&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;Sampling Locations&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;font-family:arial,helvetica,sans-serif&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0)&amp;quot;&amp;gt;Narragansett Bay sites: &amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;font-family:arial,helvetica,sans-serif&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0)&amp;quot;&amp;gt;Narragansett Bay Long Term Plankton Time Series (41.57 N -71.39 W)&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;font-family:arial,helvetica,sans-serif&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0)&amp;quot;&amp;gt;Whale Rock (41.43 N -71.42 W)&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;font-family:arial,helvetica,sans-serif&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0)&amp;quot;&amp;gt;East Passage (41.45 N -71.38 W)&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;font-family:arial,helvetica,sans-serif&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0)&amp;quot;&amp;gt;Castle Hill Beach (41.46 N -71.36 W)&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;font-family:arial,helvetica,sans-serif&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0)&amp;quot;&amp;gt;Graduate School of Oceanography dock (41.49 N -71.42 W)&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;font-family:arial,helvetica,sans-serif&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0)&amp;quot;&amp;gt;NES stations: &amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;font-family:arial,helvetica,sans-serif&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0)&amp;quot;&amp;gt;L1 (41.20 N -70.88 W), L3 (40.86 N -70.88 W), L4 (40.70 N -70.88 W), L7 (40.23 N -70.88 W), L8 (40.14 N -70.77 W), L10 (39.93 N -70.88 W)&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;</gco:CharacterString>
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                            <gco:CharacterString>&lt;p&gt;&lt;strong&gt;Continuing Award OCE-2322676&lt;br /&gt;
&lt;em&gt;Sep 2023 to Aug 2028 (estimated)&lt;/em&gt;&lt;br /&gt;
LTER: Scales of Variability in Ecosystem Dynamics and Production on the Changing Northeast U.S. Shelf (NES II)&lt;/strong&gt;&lt;br /&gt;
&lt;strong&gt;&lt;em&gt;NSF Award Abstract:&lt;/em&gt;&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;The Northeast U.S. Shelf (NES) is the region of the Northwest Atlantic Ocean that overlies the continental shelf from North Carolina to Maine. The NES has a long history of intense human utilization and provides an array of ecosystem services including shipping, recreation, conservation, and energy development. The NES also comprises a seasonally dynamic and productive ecosystem, supporting renowned fisheries, whose integrity is critical to the health of the Northeast U.S. economy. The NES ecosystem's productivity is fueled by planktonic organisms that interact with each other in complex food webs whose structure depends on environmental conditions (e.g., temperature, light, and nutrient levels). These conditions are rapidly changing because of climate-change-related warming and human utilization. For example, the NES is seeing the largest development of coastal wind farms in the U.S. to date. Phase II of the Northeast U.S. Shelf Long-Term Ecological Research program (NES-LTER II) advances our ability to predict how anthropogenic impacts will affect the dynamics of the shelf's planktonic food webs and their ability to support the productivity of higher trophic levels, from fish to whales and humans. Because the NES is subject to long-term challenges that will impact many people, the project emphasizes an active education component for helping to train the next generation of marine scientists and outreach activities to increase public understanding of marine science and technology. The project team conducts education and outreach via three main components: (1) training and mentoring for early career researchers from undergraduates to postdoctoral researchers in LTER research; (2) an LTER Schoolyard program that engages middle and high school teachers and students; and (3) public outreach through targeted events, the project website, and social media channels.&lt;/p&gt;
&lt;p&gt;Patterns of ecosystem change over seasons to decades have been documented in the NES, but the key mechanisms linking changes in the physical environment, planktonic food webs, and higher trophic levels remain poorly understood. As a result, predictive capability is limited and management strategies are largely reactive. To address these needs, NES II is targeting a mechanistic understanding of how food web structure and function responds to environmental conditions, natural variability and human induced changes. NES II combines observations that provide regional-scale context, process cruises along a high gradient cross-shelf transect, high-frequency time series at an inner-shelf location, coupled biological-physical food web models, and targeted population models. In addition, the research team is investigating how community structure and trophic transfer are impacted by disturbances including (i) the increasing prevalence of heat waves, (ii) intrusions of offshore water associated with increasing instability in the Gulf Stream, and (iii) offshore wind farms now under construction on the NES. The long-term research plan is guided by the overarching science question: &quot;How is climate change impacting the pelagic NES ecosystem and, in particular, affecting the relationship between compositional (e.g., species diversity and size structure) and aggregate (e.g., rates of primary production, and transfer of energy to higher trophic levels) variability?&quot; The investigators are assessing the extent to which the NES ecosystem possesses a biodiversity reservoir that is resilient to dramatic changes in the environment and that will allow the ecosystem to maintain overall productivity.&lt;br /&gt;
 &lt;/p&gt;
&lt;p&gt;&lt;strong&gt;Prior Award&lt;br /&gt;
&lt;em&gt;Sep 2017 to Feb 2024&lt;/em&gt;&lt;br /&gt;
LTER: Linking Pelagic Community Structure with Ecosystem Dynamics and Production Regimes on the Changing Northeast US Shelf&lt;/strong&gt;&lt;em&gt; &lt;/em&gt;&lt;br /&gt;
Summary information including abstract, PIs, and other award details are included in the Funding History PDF in the Files section below.&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;Additional Information:&lt;/strong&gt;&lt;br /&gt;
The NES-LTER project includes collaboration with the National Marine Fisheries Service / Northeast Fisheries Science Center [NMFS/NEFSC] in particular for sharing data related to Project EcoMon Zooplankton &lt;a class=&quot;moz-txt-link-freetext&quot; href=&quot;https://www.bco-dmo.org/project/2106&quot;&gt;https://www.bco-dmo.org/project/2106.&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;This project is supported by continuing grants with slight name variations:&lt;/strong&gt;&lt;/p&gt;
&lt;ul&gt;
&lt;li&gt;&lt;span style=&quot;color:rgb(0, 0, 0); font-family:helvetica,arial,sans-serif; font-size:14.4px&quot;&gt; LTER: Linking Pelagic Community Structure with Ecosystem Dynamics and Production Regimes on the Changing Northeast US Shelf&lt;/span&gt;&lt;/li&gt;
&lt;li&gt;&lt;span style=&quot;color:rgb(0, 0, 0); font-family:helvetica,arial,sans-serif; font-size:14.4px&quot;&gt; LTER: Scales of Variability in Ecosystem Dynamics and Production on the Changing Northeast U.S. Shelf (NES II)&lt;/span&gt;&lt;/li&gt;
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                            <gco:CharacterString>&lt;p&gt;NSF Award Abstract:&lt;/p&gt;
&lt;p&gt;Non-technical Description&lt;br /&gt;
The University of Rhode Island (URI) will establish the Consortium for Coastal Ecology Assessment, Innovation, and Modeling (C-AIM) to coordinate research, education, and workforce development across Rhode Island (RI) in coastal marine science and ecology. C-AIM addresses fundamental research questions using observations, computational methods, and technology development applied to Narraganset Bay (NB), the largest estuary in New England and home to important ecosystem services including fisheries, recreation, and tourism. The research will improve understanding of the microorganisms in NB, develop new models to predict pollution and harmful algal bloom events in NB, build new sensors for nutrients and pollutants, and provide data and tools for stakeholders in the state. Observational capabilities will be coordinated in an open platform for researchers across RI; it will provide real-time physical, chemical, and biological observations ? including live streaming to mobile devices. C-AIM will also establish the RI STEAM (STEM + Art) Imaging Consortium to foster collaboration between artists, designers, engineers, and scientists. Research internships will be offered to undergraduate students throughout the state and seed funding for research projects will be competitively awarded to Primarily Undergraduate Institution partners.&lt;/p&gt;
&lt;p&gt;Technical Description&lt;br /&gt;
C-AIM will employ observations and modeling to assess interactions between organisms and ecosystem function in NB and investigate ecological responses to environmental events, such as hypoxia and algal blooms. Observations of the circulation, biogeochemistry, and ecosystem will be made using existing and new instrument platforms. The Bay Observatory ? a network of observational platforms around NB - will be networked to trigger enhanced water sampling and sensing during specific environmental events, such as hypoxic conditions or phytoplankton blooms. Biogeochemical, ecological, and coastal circulation models will be integrated and coupled to focus on eutrophication and pollutant loading. Data and models will be integrated on multiple scales, from individual organisms and trophic interactions to food-web responses, and from turbulence to the regional ocean circulation. New sensing technologies for nutrients and pollutants will be developed, including affordable, micro-fluidic (Lab-on-a-Chip) devices with antifouling capabilities. The results will be synthesized and communicated to stakeholders.&lt;/p&gt;</gco:CharacterString>
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                            <gco:CharacterString>&lt;p&gt;The Narragansett Bay Long-Term Plankton Time Series is one of the world’s longest-running plankton surveys. Beginning in 1957, weekly samples have been collected to assess the phytoplankton community and characterize the physical parameters of Narragansett Bay.&lt;/p&gt;
&lt;p&gt;Samples are collected once per week -regardless of tidal stage- for temperature, salinity, turbidity, size-fractionated chlorophyll a and nutrients. Microplankton community composition (size range &amp;gt;10μm, both species identification and abundance) is determined using a light microscope to quantify live samples. The species list for the &amp;gt;10μm size fraction includes 246 different species or species complexes of protists. Samples are also collected for the determination of copepod and ctenophore concentrations.&lt;/p&gt;
&lt;p&gt;Funding for the time series has come from the University of Rhode Island since 1999. Ship time is frequently provided by the U.S. Department of Fish and Wildlife.&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;This Time Series is related to the following projects at BCO-DMO:&lt;/strong&gt;&lt;/p&gt;
&lt;ul&gt;
&lt;li&gt;Connecting local, regional and global scales of gene flow in planktonic marine diatoms (&lt;a href=&quot;https://www.bco-dmo.org/project/511708&quot;&gt;https://www.bco-dmo.org/project/511708&lt;/a&gt;)&lt;/li&gt;
&lt;li&gt;Dimensions: Collaborative Research: Genetic, functional and phylogenetic diversity determines marine phytoplankton community responses to changing temperature and nutrients (&lt;a href=&quot;https://www.bco-dmo.org/project/712787&quot;&gt;https://www.bco-dmo.org/project/712787&lt;/a&gt;)&lt;/li&gt;
&lt;li&gt;LTER: Linking Pelagic Community Structure with Ecosystem Dynamics and Production Regimes on the Changing Northeast US Shelf (&lt;a href=&quot;https://www.bco-dmo.org/project/747769&quot;&gt;https://www.bco-dmo.org/project/747769&lt;/a&gt;)&lt;/li&gt;
&lt;li&gt;Quantifying Temperature Dependence In Growth &amp;amp; Grazing Rates of Planktonic Herbivores (&lt;a href=&quot;https://www.bco-dmo.org/project/739232&quot;&gt;https://www.bco-dmo.org/project/739232&lt;/a&gt;)&lt;/li&gt;
&lt;li&gt;RII Track-1: Rhode Island Consortium for Coastal Ecology Assessment, Innovation, and Modeling (&lt;a href=&quot;https://www.bco-dmo.org/project/836631&quot;&gt;https://www.bco-dmo.org/project/836631&lt;/a&gt;)&lt;/li&gt;
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	Name: Species
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	Description: &lt;p&gt;Taxonomic assignment of Pseudo-nitzschia species&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/940250.rdf
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http://lod.bco-dmo.org/id/dataset-parameter/940251.rdf
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http://lod.bco-dmo.org/id/dataset-parameter/940252.rdf
	Name: Genbank_ASV_number
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http://lod.bco-dmo.org/id/dataset-parameter/940253.rdf
	Name: ASV_seq
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	Description: &lt;p&gt;DNA sequence of Amplicon Sequence Variant (ASV)&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/940254.rdf
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                <gco:CharacterString>&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;Samples were selected from the NES-LTER transect and various time series sites in &amp;lt;/span&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0); font-family:helvetica,arial,sans-serif; font-size:14.4px&amp;quot;&amp;gt;Narragansett Bay, Rhode Island (&amp;lt;/span&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;NB) during winter and summer periods from January 2018 through February 2023 to compare seasonal and regional patterns of &amp;lt;em&amp;gt;Pseudo-nitzschia&amp;lt;/em&amp;gt; species composition and DA, as well as environmental drivers. NB and NES will henceforth be referred to as subregions of the larger Northeast U.S. Continental Shelf region, with NES specifically referring to the area spanned by the NES-LTER transect. Samples were collected on NES-LTER cruises (&amp;lt;em&amp;gt;R/V&amp;lt;/em&amp;gt; Endeavor, &amp;lt;em&amp;gt;R/V&amp;lt;/em&amp;gt; Atlantis) from 11 stations along a 150 km transect (n=77) each winter (January-February) and summer (July-August). Samples from three to four stations per cruise were used in this dataset spanning innershelf (L1), midshelf (L3, L4) and outershelf (L7, L8, L10) sections of the transect. The northernmost station, L1, is about 50 km from the mouth of NB. To collect plankton biomass for nucleic acid isolation, CTD rosette seawater from the surface and subsurface chlorophyll maximum (SCM) were passed via peristaltic pump over 25 mm 5 µm pore size filters (Sterlitech, Kent, WA, USA). Biomass filters were either flash frozen in liquid nitrogen (2018-2022) or placed in DNA/RNA shield (winter 2023; Zymo Research, Irvine, CA, USA) and stored in a -80°C freezer. The SCM depth varied as observed by &amp;lt;em&amp;gt;in situ&amp;lt;/em&amp;gt; chlorophyll fluorescence, with a median depth of 28 m for summer and 19 m for winter samples. In cases where the SCM was not well defined due to water column mixing that typically took place in winter at nearshore stations, a sampling depth between 20 and 30 m was targeted.&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;In NB, surface seawater samples were collected from various sites in the East and West Passages including the Narragansett Bay Long-Term Plankton Time Series (NBPTS) site, Whale Rock (WR), Castle Hill Beach (CHB), East Passage (EP), and University of Rhode Island Graduate School of Oceanography (GSO) dock. Seawater was transported back to the laboratory and passed over 25 mm 5 µm pore size filters (Sterlitech, Kent, WA, USA) using a peristaltic pump before flash freezing in liquid nitrogen and storage at -80°C. To fill in several missing dates from this time series, six samples collected separately in the NBPTS (https://web.uri.edu/gso/research/plankton/) sampling program were used. These samples differed in collection methodology only by the filter pore size used (0.22 µm, Express Plus, Millipore Sigma) and vacuum as opposed to peristaltic filtration.&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;DNA was extracted from most NB and NES samples (n=219) using a modified version of the DNeasy Plant Kit (Qiagen, Germantown, MD, USA) that included a 1-minute bead beating step (0.1 mm and 0.5 mm Zirconia/Silica beads, BioSpec Products, Bartlesville, OK, USA) and two part elution into a total of 45 µL Buffer AE. Similarly, the six NBPTS samples were extracted using a modified version of the DNeasy Blood &amp;amp;amp; Tissue kit (Qiagen, Germantown, MD, USA) with a 1-minute bead beating step and final elution into 50 µL Buffer AE. Some NES samples (n=18) were extracted using the Quick-DNA/RNA Miniprep Plus Kit (Zymo Research, Irvine, CA, USA) with a 1-minute bead beating step (0.4 mm Zirconium Beads, OPS Diagnostics, Lebanon, NJ, USA) and final elution into 50 µL nuclease-free water. DNA from each sample was amplified with a primer set that targets the eukaryotic internal transcribed spacer region 1 (ITS1) and effectively distinguishes &amp;lt;em&amp;gt;Pseudo-nitzschia&amp;lt;/em&amp;gt; species (White et al., 1990; Sterling et al., 2022). Briefly, DNA was diluted to 1-4 ng/µL and 2 µL of template was added to 25 µL PCR reactions with Phusion Hot Start High-Fidelity Master Mix (Thermo Fisher Scientific Inc., Waltham, MA, USA) and HPLC-purified forward and reverse primers at 0.5 µM concentration with Illumina MiSeq adapters (Integrated DNA Technologies, Coralville, IA, USA). A stepwise thermocycle was used as described in Sterling et al. (2022).&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;DNA amplicons were sequenced at the Rhode Island-INBRE Molecular Informatics Core on the Illumina MiSeq platform (Illumina, Inc., San Diego, CA, USA). There, libraries were prepared by cleaning ITS1 PCR products with KAPA pure beads (KAPA Biosystems, Woburn, MA, USA) and attaching sequencing indices and adapters using PCR. This amplification was performed with the Illumina Nextera XT Index Kit (Illumina, San Diego, CA, USA) and Phusion High Fidelity Master Mix, followed by a second round of cleaning with KAPA pure beads and visualization with gel electrophoresis. The quality of select samples was assessed on a Bioanalyzer DNA1000 chip (Agilent Technologies, Santa Clara, CA, USA) and all samples were quantified on a Qubit fluorometer (Invitrogen, Carlsbad, CA, USA). The final library was pooled, quantified with qPCR on a LightCycler480 (Roche, Pleasanton, CA, USA) using a KAPA Biosystems Illumina Kit (KAPA Biosystems, Woburn, MA, USA), and sequenced on the Illumina MiSeq using v3 chemistry and 2x250 paired-end reads. Samples were sequenced across five separate MiSeq runs using identical methods and negative controls.&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;Sampling Locations&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;font-family:arial,helvetica,sans-serif&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0)&amp;quot;&amp;gt;Narragansett Bay sites: &amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;font-family:arial,helvetica,sans-serif&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0)&amp;quot;&amp;gt;Narragansett Bay Long Term Plankton Time Series (41.57 N -71.39 W)&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;font-family:arial,helvetica,sans-serif&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0)&amp;quot;&amp;gt;Whale Rock (41.43 N -71.42 W)&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;font-family:arial,helvetica,sans-serif&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0)&amp;quot;&amp;gt;East Passage (41.45 N -71.38 W)&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;font-family:arial,helvetica,sans-serif&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0)&amp;quot;&amp;gt;Castle Hill Beach (41.46 N -71.36 W)&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;font-family:arial,helvetica,sans-serif&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0)&amp;quot;&amp;gt;Graduate School of Oceanography dock (41.49 N -71.42 W)&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;font-family:arial,helvetica,sans-serif&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0)&amp;quot;&amp;gt;NES stations: &amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;font-size:14px&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;font-family:arial,helvetica,sans-serif&amp;quot;&amp;gt;&amp;lt;span style=&amp;quot;color:rgb(0, 0, 0)&amp;quot;&amp;gt;L1 (41.20 N -70.88 W), L3 (40.86 N -70.88 W), L4 (40.70 N -70.88 W), L7 (40.23 N -70.88 W), L8 (40.14 N -70.77 W), L10 (39.93 N -70.88 W)&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/span&amp;gt;&amp;lt;/p&amp;gt;</gco:CharacterString>
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