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Anomuran Microcoprolites from the Lowermost Navesink Formation (Maastrichtian), Monmouth County, New Jersey

机译:新泽西州蒙茅斯县最底层纳韦辛克岩层(马斯特里赫蒂安)的无色族微细铜辉石

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摘要

Anomuran microcoprolites are preserved in the Late Cretaceous lowermost Navesink Formation in Monmouth County, New Jersey. These microcoprolites occur within lens-to cigar-shaped phosphatic clay masses that occasionally include fragments of anomuran appendages. Individual microcoprolites are pellet-or rod-shaped and morphologically similar in longitudinal and cross-section to fecal material excreted from the ventro-dorsal hindgut of modern anomurans. The association of these anomuran microcoprolites in situ with Ophiomorpha burrows and the decapod crustacean Protocallianassa provides a compelling association for the identity of their producer.
机译:在新泽西州蒙茅斯县晚白垩世最底层的纳维辛克组中保留了无壬村微细粉岩。这些微土质出现在镜头到雪茄状的磷粘土团块中,该团块偶尔包括无尾附肢的碎片。各个微细铜硅石呈丸状或棒状,其纵向和横截面在形态上与从现代无足动物的腹背后肠排出的排泄物相似。这些无规村庄微胭脂土与麦兜铃洞穴和十足类甲壳动物原Callatasassa的联系提供了令人信服的协会,以了解其生产者的身份。

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