<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Hansen, Bitten Bolvig</style></author><author><style face="normal" font="default" size="100%">Milàn, Jesper</style></author><author><style face="normal" font="default" size="100%">Clemmensen, Lars B.</style></author><author><style face="normal" font="default" size="100%">Adolfssen, Jan Schulz</style></author><author><style face="normal" font="default" size="100%">Estrup, Eliza Jarl</style></author><author><style face="normal" font="default" size="100%">Nicole Klein</style></author><author><style face="normal" font="default" size="100%">Mateus,Octávio</style></author><author><style face="normal" font="default" size="100%">Oliver Wings</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Coprolites from the Late Triassic Kap Stewart Formation, Jameson Land, East Greenland: morphology, classification and prey inclusions</style></title><secondary-title><style face="normal" font="default" size="100%">Geological Society, London, Special Publications</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://sp.lyellcollection.org/content/early/2015/12/16/SP434.12.abstract</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">434</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;A large collection of vertebrate coprolites from black lacustrine shales in the Late Triassic (Rhaetian–Sinemurian) Kap Stewart Formation, East Greenland is examined with regard to internal and external morphology, prey inclusions, and possible relationships to the contemporary vertebrate fauna. A number of the coprolites were mineralogically examined by X-ray diffraction (XRD), showing the primary mineral composition to be apatite, clay minerals, carbonates and, occasionally, quartz in the form of secondary mineral grains. The coprolite assemblage shows multiple sizes and morphotypes of coprolites, and different types of prey inclusions, demonstrating that the coprolite assemblage originates from a variety of different producers.Supplementary material: A description of the size, shape, structure, texture, contents and preservation of the 328 specimens is available at &lt;a href=&quot;https://doi.org/10.6084/m9.figshare.c.2134335&quot; rel=&quot;nofollow&quot;&gt;https://doi.org/10.6084/m9.figshare.c.2134335&lt;/a&gt;&lt;/p&gt;
</style></abstract><notes><style face="normal" font="default" size="100%">&lt;p&gt;n/a&lt;/p&gt;
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