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cito: cites <http://dx.doi.org/10.5281/zenodo.5429208> , <http://dx.doi.org/10.5281/zenodo.5429206> ;
dc: creator " Tabuce, Rodolphe; Delmer, Cyrille; Gheerbrant, Emmanuel " ;
dc: title " Phosphatherium escuilliei Gheerbrant, Sudre & Cappetta 1996 " ;
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bibo: endPage " 628 " ;
bibo: issue " 4 " ;
bibo: journal " Zoological Journal of the Linnean Society " ;
bibo: pubDate " 2007-04-30 " ;
bibo: startPage " 611 " ;
bibo: volume " 149 " ;
dc: creator " Tabuce, Rodolphe; Delmer, Cyrille; Gheerbrant, Emmanuel " ;
dc: date " 2007 " ;
dc: title " Evolution of the tooth enamel microstructure in the earliest proboscideans (Mammalia) " ;
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dwc: authorityName " Gheerbrant, Sudre & Cappetta " ;
dwc: authorityYear " 1996 " ;
dwc: class " Mammalia " ;
dwc: family " Numidotheriidae " ;
dwc: genus " Phosphatherium " ;
dwc: kingdom " Animalia " ;
dwc: order " Proboscidea " ;
dwc: phylum " Chordata " ;
dwc: rank " species " ;
dwc: scientificNameAuthorship " Gheerbrant, Sudre & Cappetta, 1996 " ;
dwc: species " escuilliei " ;
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dwc: class " Mammalia " ;
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dwc: genus " Phosphatherium " ;
dwc: kingdom " Animalia " ;
dwc: order " Proboscidea " ;
dwc: phylum " Chordata " ;
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dc: description " Figure 2. A, Phosphatherium escuilliei, earliest Eocene, Ouled Abdoun Basin, Morocco; vertical section of an upper molar with Hunter-Schreger bands (HSB) that represent more than 85% of the enamel thickness. B, Tangential section in the same species, HSB present pronounced undulations. EDJ, enamel dentine junction; OES, outer enamel surface. " ;
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<http://dx.doi.org/10.5281/zenodo.5429206>
dc: description " Figure 1. A, Khamsaconus bulbosus, earliest Eocene, N’ Tagourt 2, Ouarzazate Basin, Morocco; natural vertical fracture of the DP4 (holotype and unique specimen) with radial enamel. B, Phosphatherium escuilliei, earliest Eocene, Ouled Abdoun Basin, Morocco; vertical section near the outer enamel surface (OES), with irregular prism cross sections that vary from open to closed. C, same sample as in (B) showing Hunter-Schreger bands (HSB) and the typical keyhole cross sections of the prisms in the ‘ ginkgo-tree-leaf ’ pattern. D, same sample as in (B) and (C) near the enamel dentine junction (EDJ), the interprismatic matrix (IPM) crystallites show the same orientation as the long axis of prisms. " ;
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