{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,3,18]],"date-time":"2026-03-18T13:02:34Z","timestamp":1773838954932,"version":"3.50.1"},"reference-count":47,"publisher":"The Royal Society","issue":"1","license":[{"start":{"date-parts":[[2015,1,1]],"date-time":"2015-01-01T00:00:00Z","timestamp":1420070400000},"content-version":"tdm","delay-in-days":0,"URL":"https:\/\/royalsociety.org\/journals\/ethics-policies\/data-sharing-mining\/"}],"content-domain":{"domain":["royalsocietypublishing.org"],"crossmark-restriction":true},"short-container-title":["R. Soc. open sci."],"published-print":{"date-parts":[[2015,1]]},"abstract":"<jats:p>Living in water imposes severe constraints on the evolution of the vertebrate body. As a result of these constraints, numerous extant and extinct aquatic vertebrate groups evolved convergent osteological and soft-tissue adaptations. However, one important suite of adaptations is still poorly understood: dermal cover morphologies and how they influence surface fluid dynamics. This is especially true for fossil aquatic vertebrates where the soft tissue of the dermis is rarely preserved. Recent studies have suggested that the keeled scales of mosasaurids (pelagic lizards that lived during the Late Cretaceous) aided in surface frictional drag reduction in a manner analogous to the riblets on shark placoid scales. However, here we demonstrate that mosasaurid scales were over an order of magnitude too large to have this effect. More likely they increased the frictional drag of the body and may have played a role in controlling flow separation by acting as surface roughness that turbulated the boundary layer. Such a role could have reduced pressure drag and enhanced manoeuvrability. We caution those studying fossil aquatic vertebrates from positing the presence of surface drag reducing morphologies, because as we show herein, to be effective such features need to have a spacing of approximately 0.1\u2009mm or less.<\/jats:p>","DOI":"10.1098\/rsos.140163","type":"journal-article","created":{"date-parts":[[2015,1,15]],"date-time":"2015-01-15T04:31:02Z","timestamp":1421296262000},"page":"140163","update-policy":"https:\/\/doi.org\/10.1098\/crossmark-policy","source":"Crossref","is-referenced-by-count":7,"title":["Surface drag reduction and flow separation control in pelagic vertebrates, with implications for interpreting scale morphologies in fossil taxa"],"prefix":"10.1098","volume":"2","author":[{"given":"Colin","family":"Palmer","sequence":"first","affiliation":[{"name":"Ocean and Earth Science, National Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK"},{"name":"School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Mark T.","family":"Young","sequence":"additional","affiliation":[{"name":"Ocean and Earth Science, National Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK"},{"name":"Grant Institute, School of GeoSciences, University of Edinburgh, The King's Buildings, Edinburgh EH9 3FE, UK"}],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"175","published-online":{"date-parts":[[2015,1]]},"reference":[{"key":"e_1_3_5_2_2","first-page":"381","article-title":"On the discovery of an almost perfect skeleton of the?","volume":"1","author":"Conybeare WD","year":"1824","journal-title":"Plesiosaurus."},{"key":"e_1_3_5_3_2","first-page":"1","article-title":"Die Meer-Krocodilier (Thalattosuchia) des oberen Jura unter specieller ber\u00fccksichtigung von Dacosaurus und Geosaurus","volume":"49","author":"Fraas E","year":"1902","journal-title":"Paleontographica"},{"key":"e_1_3_5_4_2","volume-title":"A descriptive catalogue of the marine reptiles of the Oxford Clay, part one.","author":"Andrews CW","year":"1910"},{"key":"e_1_3_5_5_2","volume-title":"A descriptive catalogue of the marine reptiles of the Oxford Clay, part two.","author":"Andrews CW","year":"1913"},{"key":"e_1_3_5_6_2","first-page":"829","volume-title":"Proc. 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