{"id":2564,"date":"2019-02-04T19:25:14","date_gmt":"2019-02-04T19:25:14","guid":{"rendered":"http:\/\/blogs.oregonstate.edu\/gemmlab\/?p=2564"},"modified":"2019-02-04T19:25:14","modified_gmt":"2019-02-04T19:25:14","slug":"more-than-just-whales-the-importance-of-studying-an-ecosystem","status":"publish","type":"post","link":"https:\/\/blogs.oregonstate.edu\/gemmlab\/2019\/02\/04\/more-than-just-whales-the-importance-of-studying-an-ecosystem\/","title":{"rendered":"More than just whales: The importance of studying an ecosystem"},"content":{"rendered":"<p>&nbsp;<\/p>\n<p><strong>By <a href=\"https:\/\/mmi.oregonstate.edu\/people\/dawn-barlow\">Dawn Barlow<\/a>, PhD student,\u00a0OSU Department of Fisheries and Wildlife, <a href=\"https:\/\/mmi.oregonstate.edu\/gemm-lab\">Geospatial Ecology of Marine Megafauna Lab<\/a><\/strong><\/p>\n<p>I have the privilege of studying the largest animals on the planet: blue whales (<em>Balaenoptera musculus<\/em>). However, in order to understand the ecology, distribution, and habitat use patterns of these ocean giants, I have dedicated the past several months to studying something much smaller: krill (<em>Nyctiphanes australis<\/em>). New Zealand\u2019s South Taranaki Bight region (\u201cSTB\u201d, Figure 1) is an important foraging ground for a unique population of blue whales [1,2]. A wind-driven upwelling system off of Kahurangi Point (the &#8220;X&#8221; in Figure 1) generates productivity in the region [3], leading to an abundance of krill [4], the desired blue whale prey [5].<\/p>\n<div id='gallery-1' class='gallery galleryid-2564 gallery-columns-3 gallery-size-large'><figure class='gallery-item'>\n\t\t\t<div class='gallery-icon portrait'>\n\t\t\t\t<a href='https:\/\/blogs.oregonstate.edu\/gemmlab\/2017\/06\/19\/finding-edge-preliminary-insights-blue-whale-habitat-selection-new-zealand\/fig-1\/'><img loading=\"lazy\" decoding=\"async\" width=\"660\" height=\"733\" src=\"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2017\/06\/fig-1.png\" class=\"attachment-large size-large\" alt=\"\" aria-describedby=\"gallery-1-1310\" srcset=\"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2017\/06\/fig-1.png 680w, https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2017\/06\/fig-1-270x300.png 270w\" sizes=\"auto, (max-width: 660px) 100vw, 660px\" \/><\/a>\n\t\t\t<\/div>\n\t\t\t\t<figcaption class='wp-caption-text gallery-caption' id='gallery-1-1310'>\n\t\t\t\tFigure 1.  A map of New Zealand, with the South Taranaki Bight (STB) region delineated by the black box. Cape Farewell is denoted by a star, and Kahurangi point is denoted by an X. \n\t\t\t\t<\/figcaption><\/figure><figure class='gallery-item'>\n\t\t\t<div class='gallery-icon landscape'>\n\t\t\t\t<a href='https:\/\/blogs.oregonstate.edu\/gemmlab\/2018\/02\/06\/new-approaches-come-new-insights-dont-know-blue-whales\/lunge2\/'><img loading=\"lazy\" decoding=\"async\" width=\"660\" height=\"411\" src=\"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2018\/02\/lunge2-1024x637.jpg\" class=\"attachment-large size-large\" alt=\"\" aria-describedby=\"gallery-1-1865\" srcset=\"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2018\/02\/lunge2-1024x637.jpg 1024w, https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2018\/02\/lunge2-300x187.jpg 300w, https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2018\/02\/lunge2-768x478.jpg 768w, https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2018\/02\/lunge2-e1517899825463.jpg 1000w\" sizes=\"auto, (max-width: 660px) 100vw, 660px\" \/><\/a>\n\t\t\t<\/div>\n\t\t\t\t<figcaption class='wp-caption-text gallery-caption' id='gallery-1-1865'>\n\t\t\t\tFigure 4. A blue whale lunges on an aggregation of krill. UAS piloted by Todd Chandler. \n\t\t\t\t<\/figcaption><\/figure><figure class='gallery-item'>\n\t\t\t<div class='gallery-icon landscape'>\n\t\t\t\t<a href='https:\/\/blogs.oregonstate.edu\/gemmlab\/2019\/02\/04\/more-than-just-whales-the-importance-of-studying-an-ecosystem\/n-australis\/'><img loading=\"lazy\" decoding=\"async\" width=\"558\" height=\"383\" src=\"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/02\/N.-australis.jpg\" class=\"attachment-large size-large\" alt=\"\" aria-describedby=\"gallery-1-2568\" srcset=\"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/02\/N.-australis.jpg 558w, https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/02\/N.-australis-300x206.jpg 300w\" sizes=\"auto, (max-width: 558px) 100vw, 558px\" \/><\/a>\n\t\t\t<\/div>\n\t\t\t\t<figcaption class='wp-caption-text gallery-caption' id='gallery-1-2568'>\n\t\t\t\tKrill (Nyctiphanes australis), blue whale prey in New Zealand\u2019s South Taranaki Bight region. Image: Te Papa.\n\t\t\t\t<\/figcaption><\/figure>\n\t\t<\/div>\n\n<p>Our blue whale research team collected <a href=\"http:\/\/blogs.oregonstate.edu\/gemmlab\/2017\/02\/22\/best-field-season-ever\/\">a multitude of datastreams<\/a> in three different years, including hydroacoustic data to map krill distribution throughout our study region. The summers of 2014 and 2017 were characterized by what could be considered \u201ctypical\u201d conditions: A plume of cold, upwelled water curving its way around Cape Farewell (marked with the star in Figure 1) and entering the South Taranaki Bight, spurring a cascade of productivity in the region. The 2016 season, however, was different. <a href=\"http:\/\/blogs.oregonstate.edu\/gemmlab\/2016\/02\/26\/scratching-the-surface\/\">The surface water temperatures were hot, and the whales were not where we expected to find them<\/a>.<\/p>\n<figure id=\"attachment_2569\" aria-describedby=\"caption-attachment-2569\" style=\"width: 912px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/blogs.oregonstate.edu\/gemmlab\/files\/2019\/02\/SST-comparison.png\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-2569 size-full\" src=\"http:\/\/blogs.oregonstate.edu\/gemmlab\/files\/2019\/02\/SST-comparison.png\" alt=\"\" width=\"912\" height=\"323\" srcset=\"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/02\/SST-comparison.png 912w, https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/02\/SST-comparison-300x106.png 300w, https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/02\/SST-comparison-768x272.png 768w\" sizes=\"auto, (max-width: 912px) 100vw, 912px\" \/><\/a><figcaption id=\"caption-attachment-2569\" class=\"wp-caption-text\">Figure 2. Sea surface temperature maps of the South Taranaki Bight region in each of our three study years. The white circles indicate where most blue whale sightings were made in each year. Note the very warm temperatures in 2016, and more westerly location of blue whale sightings.<\/figcaption><\/figure>\n<p>What happened to the blue whales\u2019 food source under these different conditions in 2016? Before I share some preliminary findings from my recent analyses, it is important to note that there are many possible ways to measure krill availability. For example, the number of krill aggregations, as well as how deep, thick, and dense those aggregations are in an area will all factor into how \u201cdesirable\u201d krill patches are to a blue whale. While there may not be \u201cmore\u201d or \u201cless\u201d krill from one year to the next, it may be more or less accessible to a blue whale due to energetic costs of capturing it. Here is a taste of what I\u2019ve found so far:<\/p>\n<p>In 2016, when surface waters were warm, the krill aggregations were significantly deeper than in the \u201ctypical\u201d years (ANOVA, F=7.94, p &lt;0.001):<\/p>\n<figure id=\"attachment_2565\" aria-describedby=\"caption-attachment-2565\" style=\"width: 700px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/blogs.oregonstate.edu\/gemmlab\/files\/2019\/02\/krill-depth-boxplot.png\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-2565 size-full\" src=\"http:\/\/blogs.oregonstate.edu\/gemmlab\/files\/2019\/02\/krill-depth-boxplot.png\" alt=\"\" width=\"700\" height=\"432\" srcset=\"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/02\/krill-depth-boxplot.png 700w, https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/02\/krill-depth-boxplot-300x185.png 300w\" sizes=\"auto, (max-width: 700px) 100vw, 700px\" \/><\/a><figcaption id=\"caption-attachment-2565\" class=\"wp-caption-text\">Figute 3. Boxplots comparing the median krill aggregation depth in each of our three survey years.<\/figcaption><\/figure>\n<p>The number of aggregations was not significantly different between years, but as you can see in the plot below (Figure 4) the krill were distributed differently in space:<\/p>\n<figure id=\"attachment_2566\" aria-describedby=\"caption-attachment-2566\" style=\"width: 569px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/blogs.oregonstate.edu\/gemmlab\/files\/2019\/02\/krill-num-aggs-comparison-e1549306868375.png\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-2566 size-full\" src=\"http:\/\/blogs.oregonstate.edu\/gemmlab\/files\/2019\/02\/krill-num-aggs-comparison-e1549306868375.png\" alt=\"\" width=\"569\" height=\"900\" \/><\/a><figcaption id=\"caption-attachment-2566\" class=\"wp-caption-text\">Figure 4. Map of the South Taranaki Bight region with the number of aggregations per 4 km^2, standardized by vessel survey effort. The darker colors represent areas with a higher density of krill aggregations.\u00a0<\/figcaption><\/figure>\n<p>While the bulk of the krill aggregations were located north of Cape Farewell under typical conditions (2014 and 2017), in the warm year (2016) the krill were not in this area. Rather, the area with the most aggregations was offshore, in the western portion of our study region. Now, take a look at the same figure, overlaid with our blue whale sighting locations:<\/p>\n<figure id=\"attachment_2567\" aria-describedby=\"caption-attachment-2567\" style=\"width: 569px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/blogs.oregonstate.edu\/gemmlab\/files\/2019\/02\/krill-num-aggs-comparison_sightings-e1549307337324.png\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-2567 size-full\" src=\"http:\/\/blogs.oregonstate.edu\/gemmlab\/files\/2019\/02\/krill-num-aggs-comparison_sightings-e1549307337324.png\" alt=\"\" width=\"569\" height=\"900\" \/><\/a><figcaption id=\"caption-attachment-2567\" class=\"wp-caption-text\">Figure 5. Map of standardized number of krill aggregations, overlaid with blue whale sighting locations in red stars.<\/figcaption><\/figure>\n<p>Where did we find the whales? In each year, most whale encounters were in the locations where the most krill aggregations were found! Not only that, but in 2016 the whales responded to the difference in krill distribution by shifting their distribution patterns so that they were virtually absent north of Cape Farewell, where most sightings were made in the typical years.<\/p>\n<p>The above figures demonstrate the importance of studying an ecosystem. We could puzzle and speculate over why the blue whales were further west in the warm year, but the story that is emerging in the krill data may be a key link in our understanding of how the ecosystem responds to warm conditions. While the focus of my dissertation research is blue whales, they do not live in isolation. It is through understanding the ecosystem-scale story that we can better understand blue whale ecology in the STB. As I continue <a href=\"http:\/\/blogs.oregonstate.edu\/gemmlab\/2018\/07\/23\/cloudy-with-a-chance-of-blue-whales\/\">modeling the relationships between oceanography, krill, and blue whales<\/a> in warm and typical years, we are beginning to scratch the surface of how blue whales may be responding to their environment.<\/p>\n<ol>\n<li>Torres LG. 2013 Evidence for an unrecognised blue whale foraging ground in New Zealand. <em>New Zeal. J. Mar. Freshw. Res.<\/em> <strong>47<\/strong>, 235\u2013248. (doi:10.1080\/00288330.2013.773919)<\/li>\n<li>Barlow DR <em>et al.<\/em> 2018 Documentation of a New Zealand blue whale population based on multiple lines of evidence. <em>Endanger. Species Res.<\/em> <strong>36<\/strong>, 27\u201340. (doi:https:\/\/doi.org\/10.3354\/esr00891)<\/li>\n<li>Shirtcliffe TGL, Moore MI, Cole AG, Viner AB, Baldwin R, Chapman B. 1990 Dynamics of the Cape Farewell upwelling plume, New Zealand. <em>New Zeal. J. Mar. Freshw. Res.<\/em> <strong>24<\/strong>, 555\u2013568. (doi:10.1080\/00288330.1990.9516446)<\/li>\n<li>Bradford-Grieve JM, Murdoch RC, Chapman BE. 1993 Composition of macrozooplankton assemblages associated with the formation and decay of pulses within an upwelling plume in greater cook strait, New Zealand. <em>New Zeal. J. Mar. Freshw. Res.<\/em> <strong>27<\/strong>, 1\u201322. (doi:10.1080\/00288330.1993.9516541)<\/li>\n<li>Gill P. 2002 A blue whale (Balaenoptera musculus) feeding ground in a southern Australian coastal upwelling zone. <em>J. Cetacean Res. Manag.<\/em> <strong>4<\/strong>, 179\u2013184.<\/li>\n<\/ol>\n","protected":false},"excerpt":{"rendered":"<p>&nbsp; By Dawn Barlow, PhD student,\u00a0OSU Department of Fisheries and Wildlife, Geospatial Ecology of Marine Megafauna Lab I have the privilege of studying the largest animals on the planet: blue whales (Balaenoptera musculus). However, in order to understand the ecology, distribution, and habitat use patterns of these ocean giants, I have dedicated the past several &hellip; <a href=\"https:\/\/blogs.oregonstate.edu\/gemmlab\/2019\/02\/04\/more-than-just-whales-the-importance-of-studying-an-ecosystem\/\" class=\"more-link\">Continue reading <span class=\"screen-reader-text\">More than just whales: The importance of studying an ecosystem<\/span><\/a><\/p>\n","protected":false},"author":8072,"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":[712807],"tags":[712808,1667,712899,712774,677522,635445,96374,712836,200562,799],"class_list":["post-2564","post","type-post","status-publish","format-standard","hentry","category-new-zealand-blue-whales","tag-blue-whale","tag-data-analysis","tag-dawn-barlow","tag-distribution","tag-foraging-ecology","tag-gemm-lab","tag-habitat","tag-krill","tag-new-zealand","tag-oceanography"],"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\/2564","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\/8072"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/comments?post=2564"}],"version-history":[{"count":14,"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/posts\/2564\/revisions"}],"predecessor-version":[{"id":2583,"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/posts\/2564\/revisions\/2583"}],"wp:attachment":[{"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/media?parent=2564"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/categories?post=2564"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/tags?post=2564"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}