{"id":1985,"date":"2022-10-04T13:42:51","date_gmt":"2022-10-04T13:42:51","guid":{"rendered":"https:\/\/www.marine.usf.edu\/comit\/?page_id=1985"},"modified":"2022-10-11T15:52:07","modified_gmt":"2022-10-11T15:52:07","slug":"crubiano-research","status":"publish","type":"page","link":"https:\/\/www.marine.usf.edu\/comit\/crubiano-research\/","title":{"rendered":"Catalina Rubiano"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; fullwidth=&#8221;on&#8221; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][\/et_pb_section][et_pb_section fb_built=&#8221;1&#8243; _builder_version=&#8221;4.17.4&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_row _builder_version=&#8221;4.17.4&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221; custom_padding=&#8221;||58px|||&#8221; custom_margin=&#8221;|auto|-8px|auto||&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.17.4&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.17.4&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<h1>Catalina Rubiano<\/h1>\n<p>Master&#8217;s Thesis Research<\/p>\n<p>[\/et_pb_text][et_pb_text _builder_version=&#8221;4.17.4&#8243; _module_preset=&#8221;default&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<\/p>\n<h3>Paleoshorelines of the West Florida Shelf<\/h3>\n<p>[\/et_pb_text][et_pb_code _builder_version=&#8221;4.17.4&#8243; _module_preset=&#8221;default&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<iframe loading=\"lazy\" width=\"560\" height=\"315\" src=\"https:\/\/www.youtube.com\/embed\/uy_UdgtKTX4\" title=\"YouTube video player\" frameborder=\"0\" allow=\"accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture\" allowfullscreen><\/iframe>[\/et_pb_code][et_pb_text _builder_version=&#8221;4.17.4&#8243; _module_preset=&#8221;default&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<\/p>\n<p>The West Florida Shelf is a wide low-relief platform that was formed millions of years ago. Since the deglaciation following the Last Glacial Maximum about 20,000 years ago, sea level has risen about 120 meters leaving traces of where it stood still in the form of drowned and cemented paleoshorelines that are scattered across the shelf. Today these paleoshorelines not only serve as important fish habitat, but also hold the key to understanding Quaternary sea level history in the eastern Gulf of Mexico. Evidence from high-resolution bathymetric data along with collective knowledge shared among commercial and recreational fisheries suggests these ridges could be even more common and widely dispersed that currently documented.<\/p>\n<p>This flythrough contains a map of datasets, identified and labelled herein as shorelines A-V in which paleoshorelines have been already identified, and for which the high-resolution multibeam data have already extracted to a WFS bathymetry database. These data have been compiled from various sources: USGS, USF College of Marine Science, and NOAA NMFS. Some of these paleoshorelines have been discussed extensively in previous studies (Locker et al., 1996; Jarrett et al., 2005; Gardner et al., 2005, 2007; Allee et al., 2012; Brizzolara et al., 2020; Ilich et al., 2021), while others \u2013 The Edges, Radius-Ulna, and shorelines P, QR, and S \u2013 have not yet been described. Shorelines have been identified by the depth range in which they lie, their length, and their approximate age based on correlation to the most accurate local sea level curve (Joy, 2019).\u00a0<\/p>\n<p><span style=\"text-decoration: underline;\">Works Cited<\/span><\/p>\n<p><span style=\"font-size: small;\">Locker, S. D., Hine, A. C., Tedesco, L. P., &amp; Shinn, E. A. (1996). Magnitude and timing of episodic sea-level rise during the last deglaciation. Geology, 24(9), 827-830. <\/span><\/p>\n<p><span style=\"font-size: small;\">Gardner, J. V., Dartnell, P., Mayer, L. A., Clarke, J. E. H., Calder, B. R., &amp; Duffy, G. (2005). Shelf-edge deltas and drowned barrier-island complexes on the northwest Florida outer continental shelf. Geomorphology, 64, 133-166. <\/span><\/p>\n<p><span style=\"font-size: small;\">Jarrett, B. D., Hine, A. C., Halley, R. B., Naar, D. F., Locker, S. D., Neumann, A. C., Twichell, D., Hu, C., Donahue, B. T., Jaap, W. C., Palandro, D., &amp; Ciembronowicz, K. (2005). Strange bedfellows &#8211; a deep-water hermatypic coral reef superimposed on a drowned barrier island; southern Pulley Ridge, SW Florida platform margin. Marine Geology, 214(4), 295-307. <\/span><\/p>\n<p><span style=\"font-size: small;\">Gardner, J. V., Calder, B. R., Clarke, J. E. H., Mayer, L. A., Elston, G., &amp; Rzhanov, Y. (2007). Drowned shelf-edge deltas, barrier islands and related features along the outer continental shelf north of the head of De Soto Canyon, NE Gulf of Mexico. Geomorphology, 89, 370-390. <\/span><\/p>\n<p><span style=\"font-size: small;\">Allee, R. J., David, A. W., &amp; Naar, D. F. (2012). Two Shelf-Edge Marine Protected Areas in the Eastern Gulf of Mexico. In. <\/span><br \/><span style=\"font-size: small;\">Joy, S. (2019) The trouble with the curve: Reevaluating the Gulf of Mexico sea-level curve. Quaternary International, 525. 103-113.<\/span><\/p>\n<p><span style=\"font-size: small;\">Brizzolara, J. L., Grasty, S. E., Ilich, A. R., Gray, J. W., Naar, D. F., &amp; Murawski, S. A. (2020). Characterizing benthic habitats in two Marine Protected Areas on the West Florida Shelf. In Seafloor Geomorphology as Benthic\u00a0Habitat. http:\/\/scholarcommons.usf.edu\/etd\/6806 <\/span><\/p>\n<p><span style=\"font-size: small;\">Ilich, A. R., Brizzolara, J. L., Grasty, S. E., Gray, J. W., Hommeyer, M., Lembke, C., Locker, S. D., Silverman, A., Switzer, T. S., Vivlamore, A., &amp; Murawski, S. A. (2021). Integrating Towed Underwater Video and Multibeam Acoustics for Marine Benthic Habitat Mapping and Fish Population Estimation. Geosciences, 11(176).<\/span><\/p>\n<p>[\/et_pb_text][et_pb_code _builder_version=&#8221;4.17.4&#8243; _module_preset=&#8221;default&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<iframe loading=\"lazy\" src=\"https:\/\/drive.google.com\/file\/d\/1GsGA6TuM4uxnCj0BD1HmTHMjdtoctLR1\/preview\" style=\"border: 0\" width=\"1000\" height=\"800\" frameborder=\"0\" scrolling=\"no\"><\/iframe><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] -->[\/et_pb_code][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Catalina Rubiano Master&#8217;s Thesis ResearchPaleoshorelines of the West Florida ShelfThe West Florida Shelf is a wide low-relief platform that was formed millions of years ago. Since the deglaciation following the Last Glacial Maximum about 20,000 years ago, sea level has risen about 120 meters leaving traces of where it stood still in the form of [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"","om_disable_all_campaigns":false,"_exactmetrics_skip_tracking":false,"_exactmetrics_sitenote_active":false,"_exactmetrics_sitenote_note":"","_exactmetrics_sitenote_category":0,"_monsterinsights_skip_tracking":false,"_monsterinsights_sitenote_active":false,"_monsterinsights_sitenote_note":"","_monsterinsights_sitenote_category":0,"footnotes":""},"class_list":["post-1985","page","type-page","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.marine.usf.edu\/comit\/wp-json\/wp\/v2\/pages\/1985","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.marine.usf.edu\/comit\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.marine.usf.edu\/comit\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.marine.usf.edu\/comit\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.marine.usf.edu\/comit\/wp-json\/wp\/v2\/comments?post=1985"}],"version-history":[{"count":6,"href":"https:\/\/www.marine.usf.edu\/comit\/wp-json\/wp\/v2\/pages\/1985\/revisions"}],"predecessor-version":[{"id":2006,"href":"https:\/\/www.marine.usf.edu\/comit\/wp-json\/wp\/v2\/pages\/1985\/revisions\/2006"}],"wp:attachment":[{"href":"https:\/\/www.marine.usf.edu\/comit\/wp-json\/wp\/v2\/media?parent=1985"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}