The earliest ossicone and post-cranial record of Giraffa
The oldest Giraffa material presently known consists of dental specimens. The oldest post-cranial Giraffa material belongs to the Plio-Pleistocene taxon Giraffa sivalensis, where the holotype is a third cervical vertebra. We describe three non-dental specimens from the Early Late Miocene of the Potw...
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description | The oldest Giraffa material presently known consists of dental specimens. The oldest post-cranial Giraffa material belongs to the Plio-Pleistocene taxon Giraffa sivalensis, where the holotype is a third cervical vertebra. We describe three non-dental specimens from the Early Late Miocene of the Potwar Plateau, including an 8.1 million year old ossicone, 9.4 million year old astragalus, and 8.9 million year old metatarsal and refer them to Giraffa. The described ossicone exhibits remarkable similarities with the ossicones of a juvenile modern giraffe, including the distribution of secondary bone growth, posterior curvature, and concave pitted undersurface where the ossicone would attach to the skull. The astragalus has a notably flat grove of the trochlea, medial twisting between the trochlea and the head, and a square-shaped sustentacular facet, all of which characterize the astragalus of Giraffa camelopardalis. The newly described astragalus is narrow and rectangular, unlike the boxy shaped bone of the modern giraffe. The metatarsal is large in size and has a shallow central trough created by thin medial and lateral ridges, a feature unique to Giraffa and Sivatherium. Our described material introduce the earliest non-dental material of Giraffa, a genus whose extinct representation is otherwise dominated by teeth, and demonstrate that the genus has been morphologically consistent over 9 million years. |
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The oldest post-cranial Giraffa material belongs to the Plio-Pleistocene taxon Giraffa sivalensis, where the holotype is a third cervical vertebra. We describe three non-dental specimens from the Early Late Miocene of the Potwar Plateau, including an 8.1 million year old ossicone, 9.4 million year old astragalus, and 8.9 million year old metatarsal and refer them to Giraffa. The described ossicone exhibits remarkable similarities with the ossicones of a juvenile modern giraffe, including the distribution of secondary bone growth, posterior curvature, and concave pitted undersurface where the ossicone would attach to the skull. The astragalus has a notably flat grove of the trochlea, medial twisting between the trochlea and the head, and a square-shaped sustentacular facet, all of which characterize the astragalus of Giraffa camelopardalis. The newly described astragalus is narrow and rectangular, unlike the boxy shaped bone of the modern giraffe. The metatarsal is large in size and has a shallow central trough created by thin medial and lateral ridges, a feature unique to Giraffa and Sivatherium. Our described material introduce the earliest non-dental material of Giraffa, a genus whose extinct representation is otherwise dominated by teeth, and demonstrate that the genus has been morphologically consistent over 9 million years.</description><identifier>ISSN: 1932-6203</identifier><identifier>EISSN: 1932-6203</identifier><identifier>DOI: 10.1371/journal.pone.0185139</identifier><identifier>PMID: 28926638</identifier><language>eng</language><publisher>United States: Public Library of Science</publisher><subject>Animals ; Biological Evolution ; Biology and Life Sciences ; Bone growth ; Curvature ; Dental materials ; Earth Sciences ; Fossils ; Fossils - history ; Giraffes - anatomy & histology ; History, Ancient ; Male ; Medicine and Health Sciences ; Metatarsal ; Metatarsus ; Miocene ; Museums ; Osteopathic medicine ; People and Places ; Pleistocene ; Skull ; Skull - anatomy & histology ; Spine ; Studies ; Talus - anatomy & histology ; Teeth ; Twisting ; Vertebrae ; Young adults</subject><ispartof>PloS one, 2017-09, Vol.12 (9), p.e0185139-e0185139</ispartof><rights>2017 Danowitz et al. This is an open access article distributed under the terms of the Creative Commons Attribution License: http://creativecommons.org/licenses/by/4.0/ (the “License”), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><rights>2017 Danowitz et al 2017 Danowitz et al</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a549t-fa0900bbfc5f10a39a76d2039c1970d98be9cfdfc2d96d8bccef11757aa769503</citedby><cites>FETCH-LOGICAL-a549t-fa0900bbfc5f10a39a76d2039c1970d98be9cfdfc2d96d8bccef11757aa769503</cites><orcidid>0000-0001-7970-8244</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC5605118/pdf/$$EPDF$$P50$$Gpubmedcentral$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC5605118/$$EHTML$$P50$$Gpubmedcentral$$Hfree_for_read</linktohtml><link.rule.ids>230,314,723,776,780,860,881,2096,2915,23845,27901,27902,53766,53768,79343,79344</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/28926638$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><contributor>Cray, James J.</contributor><creatorcontrib>Danowitz, Melinda</creatorcontrib><creatorcontrib>Barry, John C</creatorcontrib><creatorcontrib>Solounias, Nikos</creatorcontrib><title>The earliest ossicone and post-cranial record of Giraffa</title><title>PloS one</title><addtitle>PLoS One</addtitle><description>The oldest Giraffa material presently known consists of dental specimens. The oldest post-cranial Giraffa material belongs to the Plio-Pleistocene taxon Giraffa sivalensis, where the holotype is a third cervical vertebra. We describe three non-dental specimens from the Early Late Miocene of the Potwar Plateau, including an 8.1 million year old ossicone, 9.4 million year old astragalus, and 8.9 million year old metatarsal and refer them to Giraffa. The described ossicone exhibits remarkable similarities with the ossicones of a juvenile modern giraffe, including the distribution of secondary bone growth, posterior curvature, and concave pitted undersurface where the ossicone would attach to the skull. The astragalus has a notably flat grove of the trochlea, medial twisting between the trochlea and the head, and a square-shaped sustentacular facet, all of which characterize the astragalus of Giraffa camelopardalis. The newly described astragalus is narrow and rectangular, unlike the boxy shaped bone of the modern giraffe. The metatarsal is large in size and has a shallow central trough created by thin medial and lateral ridges, a feature unique to Giraffa and Sivatherium. Our described material introduce the earliest non-dental material of Giraffa, a genus whose extinct representation is otherwise dominated by teeth, and demonstrate that the genus has been morphologically consistent over 9 million years.</description><subject>Animals</subject><subject>Biological Evolution</subject><subject>Biology and Life Sciences</subject><subject>Bone growth</subject><subject>Curvature</subject><subject>Dental materials</subject><subject>Earth Sciences</subject><subject>Fossils</subject><subject>Fossils - history</subject><subject>Giraffes - anatomy & histology</subject><subject>History, Ancient</subject><subject>Male</subject><subject>Medicine and Health Sciences</subject><subject>Metatarsal</subject><subject>Metatarsus</subject><subject>Miocene</subject><subject>Museums</subject><subject>Osteopathic medicine</subject><subject>People and Places</subject><subject>Pleistocene</subject><subject>Skull</subject><subject>Skull - anatomy & histology</subject><subject>Spine</subject><subject>Studies</subject><subject>Talus - 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Academic</collection><collection>PubMed Central (Full Participant titles)</collection><collection>DOAJ Directory of Open Access Journals</collection><jtitle>PloS one</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Danowitz, Melinda</au><au>Barry, John C</au><au>Solounias, Nikos</au><au>Cray, James J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The earliest ossicone and post-cranial record of Giraffa</atitle><jtitle>PloS one</jtitle><addtitle>PLoS One</addtitle><date>2017-09-19</date><risdate>2017</risdate><volume>12</volume><issue>9</issue><spage>e0185139</spage><epage>e0185139</epage><pages>e0185139-e0185139</pages><issn>1932-6203</issn><eissn>1932-6203</eissn><abstract>The oldest Giraffa material presently known consists of dental specimens. The oldest post-cranial Giraffa material belongs to the Plio-Pleistocene taxon Giraffa sivalensis, where the holotype is a third cervical vertebra. We describe three non-dental specimens from the Early Late Miocene of the Potwar Plateau, including an 8.1 million year old ossicone, 9.4 million year old astragalus, and 8.9 million year old metatarsal and refer them to Giraffa. The described ossicone exhibits remarkable similarities with the ossicones of a juvenile modern giraffe, including the distribution of secondary bone growth, posterior curvature, and concave pitted undersurface where the ossicone would attach to the skull. The astragalus has a notably flat grove of the trochlea, medial twisting between the trochlea and the head, and a square-shaped sustentacular facet, all of which characterize the astragalus of Giraffa camelopardalis. The newly described astragalus is narrow and rectangular, unlike the boxy shaped bone of the modern giraffe. The metatarsal is large in size and has a shallow central trough created by thin medial and lateral ridges, a feature unique to Giraffa and Sivatherium. Our described material introduce the earliest non-dental material of Giraffa, a genus whose extinct representation is otherwise dominated by teeth, and demonstrate that the genus has been morphologically consistent over 9 million years.</abstract><cop>United States</cop><pub>Public Library of Science</pub><pmid>28926638</pmid><doi>10.1371/journal.pone.0185139</doi><orcidid>https://orcid.org/0000-0001-7970-8244</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Animals Biological Evolution Biology and Life Sciences Bone growth Curvature Dental materials Earth Sciences Fossils Fossils - history Giraffes - anatomy & histology History, Ancient Male Medicine and Health Sciences Metatarsal Metatarsus Miocene Museums Osteopathic medicine People and Places Pleistocene Skull Skull - anatomy & histology Spine Studies Talus - anatomy & histology Teeth Twisting Vertebrae Young adults |
title | The earliest ossicone and post-cranial record of Giraffa |
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