THE KRZYZANOWSKI BONEBED: AN UPPER TRIASSIC (ADAMANIAN: LATEST CARNIAN) VERTEBRATE FAUNA, AND ITS IMPLICATIONS FOR MICROVERTEBRATE STUDIES

A. Heckert, S. Krzyzanowski, S. Lucas, S. K. Harris
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引用次数: 2

Abstract

The Krzyzanowski bonebed (NMMNH locality 3764) is an extremely rich vertebrate locality in Upper Triassic Chinle Group strata in the Blue Hills near St. Johns in east-central Arizona. The fauna of the Blue Hills includes the aetosaur Stagonolepis and the phytosaur Rutiodon , both index fossils of the Adamanian (latest Carnian) land-vertebrate faunachron. The bonebearing horizon is low in the Blue Mesa Member of the Petrified Forest Formation and consists of an intraformational conglomerate that rapidly (<10 cm) fines upward into a bentonitic mudstone. The entire bonebed appears to be pedogenically modified, as the strata are color-mottled, and the bones are frequently encrusted with an iron-rich concretionary coating. Fossils from the Krzyzanowski bonebed consist of disarticulated, but associated (often jumbled) bones of small tetrapods and fish, and the largest elements recovered thus far are less than 20 cm maximum dimension. To date, the macrovertebrate fauna consists of actinopterygian and coelacanth fish, extremely fragmentary metoposaurid amphibians (confined to the base of the bonebed), phytosaurs, at least one sphenosuchian, several fish, probable theropods, and a possible ornithischian. Among the most important of these are a fish with an elongate, edentulous rostrum, and a tiny dentary bearing teeth that closely resemble those of Triassic ornithischians. Microvertebrates previously reported from the quarry include actinopterygian fish, at least two archosauriforms, probable theropods, an ornithischian dinosaur, and another probable herbivorous
krzyzanowski骨床:上三叠统(adamanian:最新卡尼系)脊椎动物区系及其对微脊椎动物研究的意义
Krzyzanowski骨床(NMMNH位置3764)是美国亚利桑那州中东部圣约翰附近蓝山上三叠统Chinle群地层中一个脊椎动物极其丰富的地区。蓝山的动物群包括Stagonolepis主龙和Rutiodon植龙,它们都是Adamanian(最新的卡尼期)陆生脊椎动物faunachron的指示化石。在石化森林组的蓝台地段,含骨层位较低,由地层内砾岩组成,向上迅速(<10厘米)细磨成膨润土泥岩。整个骨床似乎经过了土成作用的修饰,因为地层颜色斑驳,而且骨骼经常被一层富含铁的结缔组织所覆盖。来自Krzyzanowski骨床的化石由小型四足动物和鱼类的骨头组成,这些骨头是分离的,但却相互关联(通常是混乱的),迄今为止发现的最大骨头的最大尺寸小于20厘米。到目前为止,大型脊椎动物动物群包括放光鳍鱼和腔棘鱼,极零碎的后甲纲两栖动物(局限于骨床底部),植物龙,至少一种蝶类动物,几种鱼类,可能的兽脚亚目动物和一种可能的鸟臀目动物。其中最重要的是一种鱼,它有一个细长的、无牙的喙,和一个小的、有牙齿的、与三叠纪鸟臀目非常相似的牙齿。先前在采石场发现的微脊椎动物包括放光翼鱼、至少两种始龙目、可能的兽脚亚目、一种鸟臀目恐龙和另一种可能的草食性动物
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