{"id":5817,"date":"2024-07-09T08:15:54","date_gmt":"2024-07-09T15:15:54","guid":{"rendered":"https:\/\/blogs.oregonstate.edu\/gemmlab\/?p=5817"},"modified":"2024-07-09T08:15:54","modified_gmt":"2024-07-09T15:15:54","slug":"a-summer-of-crustacean-investigation","status":"publish","type":"post","link":"https:\/\/blogs.oregonstate.edu\/gemmlab\/2024\/07\/09\/a-summer-of-crustacean-investigation\/","title":{"rendered":"A Summer of Crustacean Investigation"},"content":{"rendered":"\n<p id=\"viewer-foo\"><em>By Matoska Silva, OSU Department of Integrative Biology, CEOAS REU Program<\/em><\/p>\n\n\n\n<p id=\"viewer-7e4r52123\">My name is Matoska Silva, and I just finished my first year at Oregon State University studying biology with a focus in ecology. This summer will be my first experience with marine ecology, and I\u2019m eager to dive right in. I\u2019m super excited for the opportunity to research krill due to the huge impacts these tiny organisms have on their surrounding ecosystems. The two weeks I\u2019ve spent in the CEOAS REU so far have been among the most fun and informative of my life, and I can\u2019t wait to see what else the summer has in store for me.<\/p>\n\n\n\n<figure class=\"wp-block-image\"><img decoding=\"async\" src=\"https:\/\/static.wixstatic.com\/media\/aff9d4_055ade153b294e818325c32d8ccf233d~mv2.jpg\/v1\/fill\/w_1480,h_1974,al_c,q_90,usm_0.66_1.00_0.01,enc_auto\/aff9d4_055ade153b294e818325c32d8ccf233d~mv2.jpg\" alt=\"\" \/><figcaption class=\"wp-element-caption\">Figure 1.&nbsp;Matoska presents his proposed research to the CEOAS REU program.<\/figcaption><\/figure>\n\n\n\n<p id=\"viewer-iosxx2133\">I\u2019ve spent most of my life in Oregon, so I was thrilled to learn that my project would focus on krill distribution along the Oregon Coast that I know and love. More specifically, my project focuses on the Northern California Current (NCC, the current found along the Oregon Coast) and the ways that geographic distribution of krill corresponds to climatic conditions in the region. Here is a synopsis of the project:<\/p>\n\n\n\n<p id=\"viewer-gx2fg2135\">The NCC system, which spans the west coast of North America from Cape Mendocino, California to southern British Columbia, is notable for seasonal upwelling, a process that brings cool, nutrient-rich water from the ocean depths to the surface. This process provides nutrients for a complex marine food web containing phytoplankton, zooplankton, fish, birds, and mammals (Checkley &amp; Barth, 2009). Euphausiids, commonly known as krill, are among the most ecologically important zooplankton groups in the NCC, playing a vital role in the flow of nutrients through the food web (Evans et al., 2022). <em>Euphausia pacifica <\/em>and <em>Thysanoessa spinifera<\/em>&nbsp;are the predominant krill species in the NCC, with <em>T. spinifera<\/em>&nbsp;mainly inhabiting coastal waters and <em>E. pacifica <\/em>inhabiting a wider range offshore (Brinton, 1962). <em>T. spinifera <\/em>individuals are typically physically larger than <em>E. pacifica<\/em>&nbsp;and are generally a higher-energy food source for predators (Fisher et al., 2020).&nbsp;<\/p>\n\n\n\n<p id=\"viewer-90roq2149\">Temperature has been previously established as a major factor impacting krill abundance and distribution in the NCC (Phillips et al., 2022). Massive, ecosystem-wide changes in the NCC have been linked to extreme warming brought on by the 2014-2016 marine heatwave (Brodeur et al., 2019). Both dominant krill species have been shown to respond negatively to warming events in the NCC, with anomalous warm temperatures in 2014-2016 being linked to severe declines in <em>E. pacifica<\/em>&nbsp;biomass and with <em>T. spinifera <\/em>nearly disappearing from the Oregon Coast (Peterson et al., 2017). Changes in normal seasonal size variation and trends toward smaller size distributions in multiple age groups have been observed in <em>E. pacifica<\/em>&nbsp;in response to warming in northern California coastal waters (Robertson &amp; Bjorkstedt, 2020).&nbsp;<\/p>\n\n\n\n<p id=\"viewer-v4rm22157\">The El Ni\u00f1o-Southern Oscillation (ENSO) is a worldwide climatic pattern that has been linked to warming events and ecosystem disturbances in the California Current System (McGowan et al., 1998). El Ni\u00f1o events of both strong and weak intensity can result in changes in the NCC ecosystem (Fisher et al., 2015). Alterations in the typical zooplankton community accompanying warm water conditions and a decline in phytoplankton have been recorded in the NCC during weak and strong El Ni\u00f1o occurrences (Fisher et al., 2015). A strong El Ni\u00f1o event occurred in 2023 and 2024, with three-month Oceanic Ni\u00f1o Index means reaching above 1.90 from October 2023 to January 2024 (NOAA Climate Prediction Center, <a target=\"_blank\" href=\"https:\/\/www.cpc.ncep.noaa.gov\/data\/indices\/oni.ascii.txt\" rel=\"noreferrer noopener\"><u>https:\/\/www.cpc.ncep.noaa.gov\/data\/indices\/oni.ascii.txt<\/u><\/a>).&nbsp;&nbsp;&nbsp;<\/p>\n\n\n\n<figure class=\"wp-block-image\"><img decoding=\"async\" src=\"https:\/\/static.wixstatic.com\/media\/aff9d4_9c24605e64044acab317824acf8d71b3~mv2.png\/v1\/fill\/w_1264,h_693,al_c,q_90,enc_auto\/aff9d4_9c24605e64044acab317824acf8d71b3~mv2.png\" alt=\"\" \/><figcaption class=\"wp-element-caption\">Figure 2. A graph of the ONI showing variability across two decades. Retrieved from NOAA at https:\/\/www.climate.gov\/news-features\/understanding-climate\/climate-variability-oceanic-nino-index&nbsp;<\/figcaption><\/figure>\n\n\n\n<p id=\"viewer-pskap2170\">While patterns in krill responses to warming have been described from previous years,&nbsp; the effects of the 2023-2024 El Ni\u00f1o on the spatial distribution of krill off the Oregon coast have not yet been established. As climate models have predicted that strong El Ni\u00f1o events may become more common due to greenhouse warming effects (Cai et al., 2014), continuing efforts to document zooplankton responses to El Ni\u00f1o conditions are vital for understanding how the NCC ecosystem responds to a changing climate. By investigating krill spatial distributions in April 2023, during a period of neutral ENSO conditions following a year of La Ni\u00f1a conditions, and April 2024, during the 2023-2024 El Ni\u00f1o event, we can assess how recent ENSO activity has impacted krill distributions in the NCC. In addition to broader measures of ENSO, we will examine records of localized sea surface temperatures (SST) and measurements of upwelling activity during April 2023 and 2024.<\/p>\n\n\n\n<p id=\"viewer-lnzad2173\">Understanding spatial distribution of krill aggregations is both ecologically and economically relevant, with implications for both marine conservation and management of commercial fisheries. Modeling patterns in the distribution of krill species and their predators has potential to inform marine management decisions to mitigate human impacts on marine mammals like whales (Rockwood et al., 2020). The data used to identify krill distribution were originally collected as part of the <a target=\"_blank\" href=\"https:\/\/mmi.oregonstate.edu\/marine-mammals-offshore-wind#bootstrap-fieldgroup-nav-item--summary\" rel=\"noreferrer noopener\"><u>Marine Offshore Species Assessments to Inform Clean Energy (MOSAIC) project<\/u><\/a>. The larger MOSAIC initiative centers around monitoring <a target=\"_blank\" href=\"https:\/\/blogs.oregonstate.edu\/gemmlab\/2024\/04\/08\/a-mosaic-of-species-datasets-tools-and-collaborators\/\" rel=\"noreferrer noopener\"><u>marine mammals and birds<\/u><\/a>&nbsp;in areas identified for possible future development of offshore wind energy infrastructure. The findings of this study could aid in the conservation of krill consumers during the implementation of wind energy expansion projects. Changes in krill spatial distribution are also important for monitoring species that support commercial fisheries. Temperature has been shown to play a role in the overlap in distribution of NCC krill and Pacific hake (<em>Merluccius productus<\/em>), a commercially valuable fish species in Oregon waters (Phillips et al., 2023). The findings of my project could supplement existing commercial fish abundance surveys by providing ecological insights into factors driving changes in economically important fisheries.<\/p>\n\n\n\n<figure class=\"wp-block-image\"><img decoding=\"async\" src=\"https:\/\/static.wixstatic.com\/media\/aff9d4_4e54a3e173a34597aa900fdd5fe649c8~mv2.png\/v1\/fill\/w_768,h_1536,al_c,q_90,enc_auto\/aff9d4_4e54a3e173a34597aa900fdd5fe649c8~mv2.png\" alt=\"\" \/><figcaption class=\"wp-element-caption\">Figure 3. The study area and transect design of the MOSAIC project, during which active acoustic data was collected (MOSAIC Project, https:\/\/mmi.oregonstate.edu\/marine-mammals-offshore-wind).&nbsp;<\/figcaption><\/figure>\n\n\n\n<p id=\"viewer-9qpze2188\">I\u2019m very grateful for the chance to work on a project with such important implications for the future of our Oregon coast ecosystems. My project has a lot of room for additional investigation of climate variables, with limited time being the main constraint on which processes I can explore. There are also unique methodological challenges to address during the project, and I\u2019m ready to do some experimentation to work out solutions. Wherever my project takes me, I know that I will have developed a diverse range of skills and knowledge of krill by the end of the summer.<\/p>\n\n\n<div class=\"emaillist\" id=\"es_form_f1-n1\"><form action=\"\/gemmlab\/wp-json\/wp\/v2\/posts\/5817#es_form_f1-n1\" method=\"post\" class=\"es_subscription_form es_shortcode_form  es_ajax_subscription_form\" id=\"es_subscription_form_69e1a8d019081\" data-source=\"ig-es\" data-form-id=\"1\"><div class=\"es-field-wrap\"><label>Name*<br \/><input type=\"text\" name=\"esfpx_name\" class=\"ig_es_form_field_name\" placeholder=\"\" value=\"\" required=\"required\" \/><\/label><\/div><div class=\"es-field-wrap ig-es-form-field\"><label class=\"es-field-label\">Email*<br \/><input class=\"es_required_field es_txt_email ig_es_form_field_email ig-es-form-input\" type=\"email\" name=\"esfpx_email\" value=\"\" placeholder=\"\" required=\"required\" \/><\/label><\/div><input type=\"hidden\" name=\"esfpx_lists[]\" value=\"e75fbcad40a2\" \/><input type=\"hidden\" name=\"esfpx_form_id\" value=\"1\" \/><input type=\"hidden\" name=\"es\" value=\"subscribe\" \/>\n\t\t\t<input type=\"hidden\" name=\"esfpx_es_form_identifier\" value=\"f1-n1\" \/>\n\t\t\t<input type=\"hidden\" name=\"esfpx_es_email_page\" value=\"5817\" \/>\n\t\t\t<input type=\"hidden\" name=\"esfpx_es_email_page_url\" value=\"https:\/\/blogs.oregonstate.edu\/gemmlab\/2024\/07\/09\/a-summer-of-crustacean-investigation\/\" \/>\n\t\t\t<input type=\"hidden\" name=\"esfpx_status\" value=\"Unconfirmed\" \/>\n\t\t\t<input type=\"hidden\" name=\"esfpx_es-subscribe\" id=\"es-subscribe-69e1a8d019081\" value=\"47c4709961\" \/>\n\t\t\t<label style=\"position:absolute;top:-99999px;left:-99999px;z-index:-99;\" aria-hidden=\"true\"><span hidden>Please leave this field empty.<\/span><input type=\"email\" name=\"esfpx_es_hp_email\" class=\"es_required_field\" tabindex=\"-1\" autocomplete=\"-1\" value=\"\" \/><\/label><input type=\"submit\" name=\"submit\" class=\"es_subscription_form_submit es_submit_button es_textbox_button\" id=\"es_subscription_form_submit_69e1a8d019081\" value=\"Subscribe\" \/><span class=\"es_spinner_image\" id=\"spinner-image\"><img decoding=\"async\" src=\"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-content\/plugins\/email-subscribers\/lite\/public\/images\/spinner.gif\" alt=\"Loading\" \/><\/span><\/form><span class=\"es_subscription_message \" id=\"es_subscription_message_69e1a8d019081\" role=\"alert\" aria-live=\"assertive\"><\/span><\/div>\n\n\n\n<p id=\"viewer-dlcpf2191\"><strong>References<\/strong><\/p>\n\n\n\n<p id=\"viewer-2b08e2194\">Brinton, E. (1962). The distribution of Pacific euphausiids. <em>Bulletin of the Scripps Institution of Oceanography<\/em>, <em>8<\/em>(2), 51-270. <a target=\"_blank\" href=\"https:\/\/escholarship.org\/uc\/item\/6db5n157\" rel=\"noreferrer noopener\">https:\/\/escholarship.org\/uc\/item\/6db5n157<\/a>&nbsp;<\/p>\n\n\n\n<p id=\"viewer-xlxge2202\">Brodeur, R. D., Auth, T. D., &amp; Phillips, A. J. (2019). Major shifts in pelagic micronekton and macrozooplankton community structure in an upwelling ecosystem related to an unprecedented marine heatwave. <em>Frontiers in Marine Science<\/em>, <em>6<\/em>. <a target=\"_blank\" href=\"https:\/\/doi.org\/10.3389\/fmars.2019.00212\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.3389\/fmars.2019.00212<\/a>&nbsp;<\/p>\n\n\n\n<p id=\"viewer-rdqlm2210\">Cai, W., Borlace, S., Lengaigne, M., van Rensch, P., Collins, M., Vecchi, G., Timmermann, A., Santoso, A., McPhaden, M. J., Wu, L., England, M. H., Wang, G., Guilyardi, E., &amp; Jin, F. F. (2014). Increasing frequency of extreme El Ni\u00f1o events due to greenhouse warming. <em>Nature Climate Change<\/em>, <em>4<\/em>, 111\u2013116. <a target=\"_blank\" href=\"https:\/\/doi.org\/10.1038\/nclimate2100\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.1038\/nclimate2100<\/a>&nbsp;<\/p>\n\n\n\n<p id=\"viewer-wuxd12218\">Checkley, D. M., &amp; Barth, J. A. (2009). Patterns and processes in the California Current System. <em>Progress in Oceanography<\/em>, <em>83<\/em>, 49\u201364. <a target=\"_blank\" href=\"https:\/\/doi.org\/10.1016\/j.pocean.2009.07.028\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.1016\/j.pocean.2009.07.028<\/a>&nbsp;<\/p>\n\n\n\n<p id=\"viewer-q4odx2226\">Evans, R., Gauthier, S., &amp; Robinson, C. L. K. (2022). Ecological considerations for species distribution modelling of euphausiids in the Northeast Pacific Ocean. <em>Canadian Journal of Fisheries and Aquatic Sciences<\/em>, <em>79<\/em>, 518\u2013532. <a target=\"_blank\" href=\"https:\/\/doi.org\/10.1139\/cjfas-2020-0481\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.1139\/cjfas-2020-0481<\/a>&nbsp;<\/p>\n\n\n\n<p id=\"viewer-kodk32234\">Fisher, J. L., Peterson, W. T., &amp; Rykaczewski, R. R. (2015). The impact of El Ni\u00f1o events on the pelagic food chain in the northern California Current. <em>Global Change Biology, 21,<\/em> 4401\u20134414. <a target=\"_blank\" href=\"https:\/\/doi.org\/10.1111\/gcb.13054\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.1111\/gcb.13054<\/a>&nbsp;<\/p>\n\n\n\n<p id=\"viewer-0xlrs2240\">Fisher, J. L., Menkel, J., Copeman, L., Shaw, C. T., Feinberg, L. R., &amp; Peterson, W. T. (2020). Comparison of condition metrics and lipid content between <em>Euphausia pacifica<\/em>&nbsp;and <em>Thysanoessa spinifera<\/em>&nbsp;in the Northern California Current, USA. <em>Progress in Oceanography<\/em>, <em>188<\/em>, 102417. <a target=\"_blank\" href=\"https:\/\/doi.org\/10.1016\/j.pocean.2020.102417\" rel=\"noreferrer noopener\"><u>https:\/\/doi.org\/10.1016\/j.pocean.2020.102417<\/u><\/a><\/p>\n\n\n\n<p id=\"viewer-4topn2251\">McGowan, J. A., Cayan, D. R., &amp; Dorman, L. M. (1998). Climate-ocean variability and ecosystem response in the Northeast Pacific. <em>Science<\/em>, <em>281<\/em>, 210\u2013217. <a target=\"_blank\" href=\"https:\/\/doi.org\/10.1126\/science.281.5374.210\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.1126\/science.281.5374.210<\/a>&nbsp;<\/p>\n\n\n\n<p id=\"viewer-s1lev2259\">Phillips, E. M., Chu, D., Gauthier, S., Parker-Stetter, S. L., Shelton, A. O., &amp; Thomas, R. E. (2022). Spatiotemporal variability of Euphausiids in the California Current Ecosystem: Insights from a recently developed time series. <em>ICES Journal of Marine Science<\/em>, <em>79<\/em>, &nbsp; 1312\u20131326. <a target=\"_blank\" href=\"https:\/\/doi.org\/10.1093\/icesjms\/fsac055\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.1093\/icesjms\/fsac055<\/a>&nbsp;<\/p>\n\n\n\n<p id=\"viewer-h8l2v2267\">Phillips, E. M., Malick, M. J., Gauthier, S., Haltuch, M. A., Hunsicker, M. E., Parker\u2010Stetter, S. L., &amp; Thomas, R. E. (2023). The influence of temperature on Pacific hake co\u2010occurrence with euphausiids in the California Current Ecosystem. <em>Fisheries Oceanography<\/em>, <em>32<\/em>, 267\u2013279. <a target=\"_blank\" href=\"https:\/\/doi.org\/10.1111\/fog.12628\" rel=\"noreferrer noopener\"><u>https:\/\/doi.org\/10.1111\/fog.12628<\/u><\/a><\/p>\n\n\n\n<p id=\"viewer-yw7qd2274\">Peterson, W. T., Fisher, J. L., Strub, P. T., Du, X., Risien, C., Peterson, J., &amp; Shaw, C. T. (2017). The pelagic ecosystem in the Northern California Current off Oregon during the 2014\u20132016 warm anomalies within the context of the past 20 years. <em>Journal of Geophysical Research: Oceans<\/em>, <em>122<\/em>(9), 7267\u20137290. <a target=\"_blank\" href=\"https:\/\/doi.org\/10.1002\/2017jc012952\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.1002\/2017jc012952<\/a>&nbsp;<\/p>\n\n\n\n<p id=\"viewer-ags272282\">Robertson, R. R., &amp; Bjorkstedt, E. P. (2020). Climate-driven variability in <em>Euphausia pacifica<\/em>size distributions off Northern California. <em>Progress in Oceanography<\/em>, <em>188<\/em>, 102412.<a target=\"_blank\" href=\"https:\/\/doi.org\/10.1016\/j.pocean.2020.102412\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.1016\/j.pocean.2020.102412<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>By Matoska Silva, OSU Department of Integrative Biology, CEOAS REU Program My name is Matoska Silva, and I just finished my first year at Oregon State University studying biology with a focus in ecology. This summer will be my first experience with marine ecology, and I\u2019m eager to dive right in. I\u2019m super excited for &hellip; <a href=\"https:\/\/blogs.oregonstate.edu\/gemmlab\/2024\/07\/09\/a-summer-of-crustacean-investigation\/\" class=\"more-link\">Continue reading <span class=\"screen-reader-text\">A Summer of Crustacean Investigation<\/span><\/a><\/p>\n","protected":false},"author":10751,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_jetpack_memberships_contains_paid_content":false,"footnotes":"","jetpack_publicize_message":"","jetpack_publicize_feature_enabled":true,"jetpack_social_post_already_shared":true,"jetpack_social_options":{"image_generator_settings":{"template":"highway","default_image_id":0,"font":"","enabled":false},"version":2}},"categories":[188686,1310535],"tags":[1310796,712836,148762,106204,5],"class_list":["post-5817","post","type-post","status-publish","format-standard","hentry","category-current-projects","category-oregon-whale-distribution","tag-intern","tag-krill","tag-oregon-coast","tag-reu","tag-science"],"jetpack_publicize_connections":[],"jetpack_featured_media_url":"","jetpack_sharing_enabled":true,"post_mailing_queue_ids":[],"_links":{"self":[{"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/posts\/5817","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/users\/10751"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/comments?post=5817"}],"version-history":[{"count":1,"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/posts\/5817\/revisions"}],"predecessor-version":[{"id":5818,"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/posts\/5817\/revisions\/5818"}],"wp:attachment":[{"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/media?parent=5817"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/categories?post=5817"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/tags?post=5817"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}