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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/835619.rdf" xlink:actuate="onRequest">Pigment data by phytoplankton taxa from CTD casts from NOAA Ship R/V Nancy Foster cruises NF1704 and NF1802 in the Gulf of Mexico, May 2017 and 2018</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Selph, K. E. (2021) Pigment data by phytoplankton taxa from CTD casts from NOAA Ship R/V Nancy Foster cruises NF1704 and NF1802 in the Gulf of Mexico, May 2017 and 2018. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2021-01-07 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.835619.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>CTD Fluorometer Dataset Description: &amp;lt;p&amp;gt;These data were published in&amp;amp;nbsp;Selph et al. 2021:&amp;lt;br /&amp;gt;
- Table III.&amp;amp;nbsp; Shallow pigment and taxonomic assignments.&amp;lt;br /&amp;gt;
- Table IV.&amp;amp;nbsp; Deep pigment and taxonomic assignments.&amp;lt;br /&amp;gt;
- Supp. Table I (Chemtax input/output ratios)&amp;lt;br /&amp;gt;
- Supp. Table II-IX (Depth profiles of pigments and taxa from CHEMTAX analyses)&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Flow cytometry:&amp;lt;/strong&amp;gt;&amp;amp;nbsp; Samples for picophytoplankton abundance were collected pre-dawn from Niskin bottles mounted on a 24-place rosette system equipped with a Seabird SBE911 CTD and a Seapoint fluorometer. Samples (2-mL) were preserved (0.5% paraformaldehyde) and frozen in LN2, then stored at -80°C until shore-based analyses. Flow cytometry samples were thawed and stained for 1 h with the DNA stain Hoechst 33342 (1 µg/ml, Monger and Landry, 1993), then analyzed with a Beckman Coulter EPICS Altra flow cytometer (Selph et al., 2011).&amp;amp;nbsp; Listmode data were processed using FlowJo (version 9.7.7, Treestar, Inc.) to delineate Prochlorococcus (PRO), Synechococcus (SYN), and eukaryotic phytoplankton (PEUK).&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Chlorophyll a contributions for Prochlorococcus (PRO) and Synechococcus (SYN) were assigned from normalized chlorophyll (red) fluorescence (NCF) from flow cytometry as follows:&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;(1)&amp;amp;nbsp; PRO NCF/L = PRO NCF × PRO (cells/L)&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;(2) SYN NCF/L = SYN NCF × SYN (cells/L)&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Assuming that PRO NCF/L was directly proportional to the pigment divinyl chlorophyll a (DVCHLa, ng/L) since DVCHLa is only found in PRO, we estimated the monovinyl chlorophyll a (MVCHLa) associated with SYN as:&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;amp;nbsp;&amp;amp;nbsp;&amp;amp;nbsp;&amp;amp;nbsp;&amp;amp;nbsp;&amp;amp;nbsp;(3) SYN MVChla =&amp;amp;nbsp; (SYN NCF/L)/(PRO NCF/L)× DVChla&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Microscopy for Trichodesmium:&amp;lt;/strong&amp;gt;&amp;amp;nbsp; Trichodesmium (TRICH) abundances were assessed from 6.6-L samples taken from 6 depths (2-50 m) in daily (~noon) CTD casts.&amp;amp;nbsp; Water was gravity filtered directly from the Niskin bottle onto 8-µm, 47-mm Millipore TETP filters, preserved (2% paraformaldehyde), mounted on glass slides and frozen (-80°C).&amp;amp;nbsp; Trichome chlorophyll, carbon and nitrogen (CN) contents to biovolume ratios were determined from 6.6-L samples collected as above on the same noon casts but onto 20-µm, 47-mm filters and frozen (-80°C).&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;TRICH abundance was based on microscopical analyses of preserved, frozen slides (see methods below). Thawed filters were scanned using a dissecting microscope (10X-30X) with a NightSea SFA adaptor and Royal Blue light head (EX 440-460 nm, EM &amp;amp;gt;500 nm) to find all orange-glowing trichomes and colonies.&amp;amp;nbsp; TRICH were digitally imaged (OMAX camera) using ToupLite (Touptec.com), counted, and trichome lengths measured.&amp;amp;nbsp; Trichome widths were determined with an Olympus BX-41 epifluorescence microscope (200X, EX 450-480 nm, dichroic 500 nm, EM &amp;amp;gt;515 nm). These data comprised the background contribution of trichomes to HPLC samples.&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;For chlorophyll a contents, duplicate samples of TRICH from unpreserved, frozen samples (see methods below) were suspended in salt water, filtered onto GF/F filters, extracted (90% acetone), and fluorescence determined with a 10AU fluorometer using the acidification method (Strickland and Parsons, 1972).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;HPLC pigments:&amp;lt;/strong&amp;gt;&amp;amp;nbsp; Samples (2.2-L) for pigment analyses by high-pressure liquid chromatography (HPLC) were collected pre-dawn from Niskin bottles mounted on a 24-place rosette system equipped with a Seabird SBE911 CTD and a Seapoint fluorometer.&amp;amp;nbsp; They were filtered onto GF/F filters, frozen in LN2 and stored at -85°C.&amp;amp;nbsp; On shore, samples were sent to Horn Point Analytical Services Laboratory (University of Maryland Center for Environmental Science).&amp;amp;nbsp; There they were extracted, and analyzed using an automated 1100 HPLC system with Agilent temperature-controlled autosampler, Peltier temperature-controlled column oven compartment, PDA detector and ChemStation software.&amp;amp;nbsp; The HPLC method uses a C8 column and a reversed phase, methanol-based solvent system (Van Heukelem and Thomas, 2001; Hooker et al., 2012).&amp;amp;nbsp; MVCHLa and DVCHLa are detected at 665 nm.&amp;amp;nbsp; Carotenoid and xanthophyll accessory pigments are detected at 450 nm.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The pigments used for phytoplankton taxonomic identification were monovinyl chlorophyll a (MVCHLa), divinyl chlorophyll a (DVCHLa), monovinyl chlorophyll b (MVCHLb), divinyl chlorophyll b (DVCHLb), chlorophyll c3 (CHLc3), zeaxanthin (ZEAX), fucoxanthin (FUCO), 19’-hex-fucoxanthin (HEX), 19’-but-fucoxanthin (BUT), allophycocyanin (ALLO), peridinin (PER), neoxanthin (NEO), and prasinoxanthin (PRAS).&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;SYN and TRICH MVCHLa was subtracted from the total MVCHLa, and the remaining MVCHLa was used for all eukaryotic taxa in CHEMTAX analyses (v. 1.95, Wright, 2008).&amp;amp;nbsp; For CHEMTAX, initial pigment ratios (accessory pigment:MVCHLa) were those of oceanic species (Higgens et al., 2011) and indicative of the following groups: chlorophytes (CHLOR), diatoms (DIAT), prymnesiophytes - type 6 (PRYM), pelagophytes (PELAG), cryptophytes (CRYPT), prasinophytes - type 3 (PRAS3), and dinoflagellates (A-DINO).&amp;amp;nbsp; Data were divided into 2 groups: shallower and deeper than 60 m, since some of the accessory pigments were only present in deep samples (NEO and ALLO) and the general pattern of pigments showed a different community at depth.&amp;amp;nbsp; The initial ratio matrix was randomized into 60 matrices (0.7 x random number between -0.5 and +0.5), which were then applied to the data sets (Selph et al., 2021, Supp. Table 1).&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/819487.rdf" xlink:title="OCE-1851558" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1851558 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1851558</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/834952.rdf" xlink:title="NA16NMF4320058" xlink:actuate="onRequest">Funding provided by National Oceanic and Atmospheric Administration (NOAA) Award Number: NA16NMF4320058 Award URL: https://grantsonline.rdc.noaa.gov/flows/publicSearch/showAwardDetails.do?awdNum=NA16NMF4320058</gmx:Anchor>
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                            <gco:CharacterString>&lt;p&gt;&lt;em&gt;NSF Award Abstract:&lt;/em&gt;&lt;br /&gt;
The small area between NW Australia and Indonesia in the eastern Indian Ocean (IO) is the only known spawning ground of Southern Bluefin Tuna (SBT), a critically endangered top marine predator. Adult SBT migrate thousands of miles each year from high latitude feeding areas to lay their eggs in these tropical waters, where food concentrations on average are below levels that can support optimal feeding and growth of their larvae. Many critical aspects of this habitat are poorly known, such as the main source of nitrogen nutrient that sustains system productivity, how the planktonic food web operates to produce the unusual types of zooplankton prey that tuna larvae prefer, and how environmental differences in habitat quality associated with ocean fronts and eddies might be utilized by adult spawning tuna to give their larvae a greater chance for rapid growth and survival success. This project investigates these questions on a 38-day expedition in early 2021, during the peak time of SBT spawning. This project is a US contribution to the 2nd International Indian Ocean Expedition (IIOE-2) that advances understanding of biogeochemical and ecological dynamics in the poorly studied eastern IO. This is the first detailed study of nitrogen and carbon cycling in the region linking Pacific and IO waters. The shared dietary preferences of SBT larvae with those of other large tuna and billfish species may also make the insights gained broadly applicable to understanding larval recruitment issues for top consumers in other marine ecosystems. New information from the study will enhance international management efforts for SBT. The shared larval dietary preferences of large tuna and billfish species may also extend the insights gained broadly to many other marine top consumers, including Atlantic bluefin tuna that spawn in US waters of the Gulf of Mexico. The end-to-end study approach, highlights connections among physical environmental variability, biogeochemistry, and plankton food webs leading to charismatic and economically valuable fish production, is the theme for developing educational tools and modules through the &quot;scientists-in-the-schools&quot; program of the Center for Ocean-Atmospheric Prediction Studies at Florida State University, through a program for enhancing STEM learning pathways for underrepresented students in Hawaii, and through public outreach products for display at the Birch Aquarium in San Diego. The study also aims to support an immersive field experience to introduce talented high school students to marine research, with the goal of developing a sustainable marine-related educational program for underrepresented students in rural northwestern Florida.&lt;/p&gt;
&lt;p&gt;Southern Bluefin Tuna (SBT) migrate long distances from high-latitude feeding grounds to spawn exclusively in a small oligotrophic area of the tropical eastern Indian Ocean (IO) that is rich in mesoscale structures, driven by complex currents and seasonally reversing monsoonal winds. To survive, SBT larvae must feed and grow rapidly under environmental conditions that challenge conventional understanding of food-web structure and functional relationships in poor open-ocean systems. The preferred prey of SBT larvae, cladocerans and Corycaeidae copepods, are poorly studied and have widely different implications for trophic transfer efficiencies to larvae. Differences in nitrogen sources - N fixation vs deep nitrate of Pacific origin - to sustain new production in the region also has implications for conditions that may select for prey types (notably cladocerans) that enhance transfer efficiency and growth rates of SBT larvae. The relative importance of these N sources for the IO ecosystem may affect SBT resiliency to projected increased ocean stratification. This research expedition investigates how mesoscale variability in new production, food-web structure and trophic fluxes affects feeding and growth conditions for SBT larvae. Sampling across mesoscale features tests hypothesized relationships linking variability in SBT larval feeding and prey preferences (gut contents), growth rates (otolith analyses) and trophic positions (TP) to the environmental conditions of waters selected by adult spawners. Trophic Positions of larvae and their prey are determined using Compound-Specific Isotope Analyses of Amino Acids (CSIA-AA). Lagrangian experiments investigate underlying process rates and relationships through measurements of water-column 14C productivity, N2 fixation, 15NO3- uptake and nitrification; community biomass and composition (flow cytometry, pigments, microscopy, in situ imaging, genetic analyses); and trophic fluxes through micro- and mesozooplankton grazing, remineralization and export. Biogeochemical and food web elements of the study are linked by CSIA-AA (N source, TP), 15N-constrained budgets and modeling. The project elements comprise an end-to-end coupled biogeochemistry-trophic study as has not been done previously for any pelagic ecosystem.&lt;/p&gt;
&lt;p&gt;This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.&lt;/p&gt;</gco:CharacterString>
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            http://lod.bco-dmo.org/id/dataset-parameter/835715.rdf
	Name: Cruise
	Units: unitless
	Description: &lt;p&gt;cruise identifier&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/835716.rdf
	Name: Station
	Units: unitless
	Description: &lt;p&gt;station identifier&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/835717.rdf
	Name: Date
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	Name: Lat
	Units: decimal degrees
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http://lod.bco-dmo.org/id/dataset-parameter/835719.rdf
	Name: Lon
	Units: decimal degrees
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http://lod.bco-dmo.org/id/dataset-parameter/835720.rdf
	Name: Cycle
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http://lod.bco-dmo.org/id/dataset-parameter/835721.rdf
	Name: CTD_cast
	Units: unitless
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http://lod.bco-dmo.org/id/dataset-parameter/835723.rdf
	Name: Depth
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http://lod.bco-dmo.org/id/dataset-parameter/835724.rdf
	Name: TChl_a
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http://lod.bco-dmo.org/id/dataset-parameter/835725.rdf
	Name: MVChl_a
	Units: ng/L
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http://lod.bco-dmo.org/id/dataset-parameter/835726.rdf
	Name: DVChl_a
	Units: ng/L
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http://lod.bco-dmo.org/id/dataset-parameter/835727.rdf
	Name: PRO
	Units: ng divinyl chlorophyll a/L
	Description: &lt;p&gt;Prochlorococcus divinyl chlorophyll a concentration&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/835728.rdf
	Name: SYN
	Units: ng monovinyl chlorophyll a/L
	Description: &lt;p&gt;Synechococcus monovinyl chlorophyll a concentration&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/835729.rdf
	Name: Diatoms
	Units: ng monovinyl chlorophyll a/L
	Description: &lt;p&gt;Diatoms monovinyl chlorophyll a concentration&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/835730.rdf
	Name: Dinofl
	Units: ng monovinyl chlorophyll a/L
	Description: &lt;p&gt;Dinoflagellates monovinyl chlorophyll a concentration&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/835731.rdf
	Name: Pelago
	Units: ng monovinyl chlorophyll a/L
	Description: &lt;p&gt;Pelagophytes monovinyl chlorophyll a concentration&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/835732.rdf
	Name: Pras3
	Units: ng monovinyl chlorophyll a/L
	Description: &lt;p&gt;Prasinophytes-Type 3 monovinyl chlorophyll a concentration&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/835733.rdf
	Name: Prymnes6
	Units: ng monovinyl chlorophyll a/L
	Description: &lt;p&gt;Prymnesiophytes-Type 6 monovinyl chlorophyll a concentration&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/835734.rdf
	Name: Chloroph
	Units: ng monovinyl chlorophyll a/L
	Description: &lt;p&gt;Chlorophytes monovinyl chlorophyll a concentration&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/835735.rdf
	Name: Crypto
	Units: ng monovinyl chlorophyll a/L
	Description: &lt;p&gt;Cryptophytes monovinyl chlorophyll a concentration&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/835736.rdf
	Name: TRICHO
	Units: ng monovinyl chlorophyll a/L
	Description: &lt;p&gt;Trichodesmium monovinyl chlorophyll a concentration&lt;/p&gt; 
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                <gco:CharacterString>&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Flow cytometry:&amp;lt;/strong&amp;gt;&amp;amp;nbsp; Samples for picophytoplankton abundance were collected pre-dawn from Niskin bottles mounted on a 24-place rosette system equipped with a Seabird SBE911 CTD and a Seapoint fluorometer. Samples (2-mL) were preserved (0.5% paraformaldehyde) and frozen in LN2, then stored at -80°C until shore-based analyses. Flow cytometry samples were thawed and stained for 1 h with the DNA stain Hoechst 33342 (1 µg/ml, Monger and Landry, 1993), then analyzed with a Beckman Coulter EPICS Altra flow cytometer (Selph et al., 2011).&amp;amp;nbsp; Listmode data were processed using FlowJo (version 9.7.7, Treestar, Inc.) to delineate Prochlorococcus (PRO), Synechococcus (SYN), and eukaryotic phytoplankton (PEUK).&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Chlorophyll a contributions for Prochlorococcus (PRO) and Synechococcus (SYN) were assigned from normalized chlorophyll (red) fluorescence (NCF) from flow cytometry as follows:&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;(1)&amp;amp;nbsp; PRO NCF/L = PRO NCF × PRO (cells/L)&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;(2) SYN NCF/L = SYN NCF × SYN (cells/L)&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Assuming that PRO NCF/L was directly proportional to the pigment divinyl chlorophyll a (DVCHLa, ng/L) since DVCHLa is only found in PRO, we estimated the monovinyl chlorophyll a (MVCHLa) associated with SYN as:&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;amp;nbsp;&amp;amp;nbsp;&amp;amp;nbsp;&amp;amp;nbsp;&amp;amp;nbsp;&amp;amp;nbsp;(3) SYN MVChla =&amp;amp;nbsp; (SYN NCF/L)/(PRO NCF/L)× DVChla&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Microscopy for Trichodesmium:&amp;lt;/strong&amp;gt;&amp;amp;nbsp; Trichodesmium (TRICH) abundances were assessed from 6.6-L samples taken from 6 depths (2-50 m) in daily (~noon) CTD casts.&amp;amp;nbsp; Water was gravity filtered directly from the Niskin bottle onto 8-µm, 47-mm Millipore TETP filters, preserved (2% paraformaldehyde), mounted on glass slides and frozen (-80°C).&amp;amp;nbsp; Trichome chlorophyll, carbon and nitrogen (CN) contents to biovolume ratios were determined from 6.6-L samples collected as above on the same noon casts but onto 20-µm, 47-mm filters and frozen (-80°C).&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;TRICH abundance was based on microscopical analyses of preserved, frozen slides (see methods below). Thawed filters were scanned using a dissecting microscope (10X-30X) with a NightSea SFA adaptor and Royal Blue light head (EX 440-460 nm, EM &amp;amp;gt;500 nm) to find all orange-glowing trichomes and colonies.&amp;amp;nbsp; TRICH were digitally imaged (OMAX camera) using ToupLite (Touptec.com), counted, and trichome lengths measured.&amp;amp;nbsp; Trichome widths were determined with an Olympus BX-41 epifluorescence microscope (200X, EX 450-480 nm, dichroic 500 nm, EM &amp;amp;gt;515 nm). These data comprised the background contribution of trichomes to HPLC samples.&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;For chlorophyll a contents, duplicate samples of TRICH from unpreserved, frozen samples (see methods below) were suspended in salt water, filtered onto GF/F filters, extracted (90% acetone), and fluorescence determined with a 10AU fluorometer using the acidification method (Strickland and Parsons, 1972).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;HPLC pigments:&amp;lt;/strong&amp;gt;&amp;amp;nbsp; Samples (2.2-L) for pigment analyses by high-pressure liquid chromatography (HPLC) were collected pre-dawn from Niskin bottles mounted on a 24-place rosette system equipped with a Seabird SBE911 CTD and a Seapoint fluorometer.&amp;amp;nbsp; They were filtered onto GF/F filters, frozen in LN2 and stored at -85°C.&amp;amp;nbsp; On shore, samples were sent to Horn Point Analytical Services Laboratory (University of Maryland Center for Environmental Science).&amp;amp;nbsp; There they were extracted, and analyzed using an automated 1100 HPLC system with Agilent temperature-controlled autosampler, Peltier temperature-controlled column oven compartment, PDA detector and ChemStation software.&amp;amp;nbsp; The HPLC method uses a C8 column and a reversed phase, methanol-based solvent system (Van Heukelem and Thomas, 2001; Hooker et al., 2012).&amp;amp;nbsp; MVCHLa and DVCHLa are detected at 665 nm.&amp;amp;nbsp; Carotenoid and xanthophyll accessory pigments are detected at 450 nm.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The pigments used for phytoplankton taxonomic identification were monovinyl chlorophyll a (MVCHLa), divinyl chlorophyll a (DVCHLa), monovinyl chlorophyll b (MVCHLb), divinyl chlorophyll b (DVCHLb), chlorophyll c3 (CHLc3), zeaxanthin (ZEAX), fucoxanthin (FUCO), 19’-hex-fucoxanthin (HEX), 19’-but-fucoxanthin (BUT), allophycocyanin (ALLO), peridinin (PER), neoxanthin (NEO), and prasinoxanthin (PRAS).&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;SYN and TRICH MVCHLa was subtracted from the total MVCHLa, and the remaining MVCHLa was used for all eukaryotic taxa in CHEMTAX analyses (v. 1.95, Wright, 2008).&amp;amp;nbsp; For CHEMTAX, initial pigment ratios (accessory pigment:MVCHLa) were those of oceanic species (Higgens et al., 2011) and indicative of the following groups: chlorophytes (CHLOR), diatoms (DIAT), prymnesiophytes - type 6 (PRYM), pelagophytes (PELAG), cryptophytes (CRYPT), prasinophytes - type 3 (PRAS3), and dinoflagellates (A-DINO).&amp;amp;nbsp; Data were divided into 2 groups: shallower and deeper than 60 m, since some of the accessory pigments were only present in deep samples (NEO and ALLO) and the general pattern of pigments showed a different community at depth.&amp;amp;nbsp; The initial ratio matrix was randomized into 60 matrices (0.7 x random number between -0.5 and +0.5), which were then applied to the data sets (Selph et al., 2021, Supp. Table 1).&amp;lt;/p&amp;gt;</gco:CharacterString>
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&amp;lt;p&amp;gt;Trichodesmium image analysis:&amp;amp;nbsp; ToupLite (Touptec.com)&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;HPLC:&amp;amp;nbsp; ChemStation software for generated raw data, whereas the program CHEMTAX was used for partitioning MVCHLa into taxonomic groups (CHEMTAX, v. 1.95,Wright, 2008).&amp;lt;/p&amp;gt;

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