<?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%">Milàn, J.</style></author><author><style face="normal" font="default" size="100%">L. B. Clemmensen</style></author><author><style face="normal" font="default" size="100%">J.S. Adolfssen</style></author><author><style face="normal" font="default" size="100%">E.J. Estrup</style></author><author><style face="normal" font="default" size="100%">N. Frobøse</style></author><author><style face="normal" font="default" size="100%">N. Klein</style></author><author><style face="normal" font="default" size="100%">O. Mateus</style></author><author><style face="normal" font="default" size="100%">O. Wings</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">A preliminary report on coprolites from the Late Triassic part of the Kap Stewart Formation, Jameson Land, East Greenland</style></title><secondary-title><style face="normal" font="default" size="100%">New Mexico Museum of Natural History and Science, Bulletin</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><urls><related-urls><url><style face="normal" font="default" size="100%">https://docentes.fct.unl.pt/sites/default/files/omateus/files/milan_et_al_2012_greenland_coprolites_triassic.pdf</style></url></related-urls></urls><volume><style face="normal" font="default" size="100%">57</style></volume><pages><style face="normal" font="default" size="100%">203-205</style></pages><abstract><style face="normal" font="default" size="100%">&lt;p&gt;The basal part of the Triassic-Jurassic (Rhaetian-Sinemurian) Kap Stewart Formation, exposed at Jameson Land, East Greenland, yields an extensive coprolite collection from black, parallel-laminated mudstone (“paper shale”), representing an open lacustrine system. Preliminary investigations show three different types of coprolites: elongated cylindrical masses, composed of irregularly wrapped layers; elongated cylindrical masses with constriction marks; and spirally-coiled specimens.&lt;/p&gt;
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