Large Phymatoderma in pliocene slope deposits, northwestern Ecuador: Associated ichnofauna, fabrication, and behavioral ecology

Large Phymatoderma in pliocene slope deposits, northwestern Ecuador: Associated ichnofauna, fabrication, and behavioral ecology
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厄瓜多尔西北部上新世斜坡沉积物中的大型植皮动物:相关的动物群、制造和行为生态学

DOI:
10.1080/10420949809386437
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发表时间:
1998
影响因子:
0.8
通讯作者:
E. Vokes
E. Vokes
中科院分区:
地球科学4区
文献类型:
--
作者:
W. Miller;E. Vokes

文献摘要

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植晶岩是一种复杂的、分支的生物成因结构,在遗迹学文献中很少提及,尽管它最近可能被误认为是“佐纳里特”和大颗粒填充的“球粒陨石”。遗迹属通常被解释为地下存款-进食动物的产物。厄瓜多尔上新世斜坡泥岩中保存完好的样品可归属于P. granulatum(施洛泰姆,1822年)。这些结构的总直径通常为30-40厘米;由向外分支、水平到近水平、重叠的隧道组成;隧道填充物由粒状火山灰组成。厄瓜多尔的Phymatalus出现了一个中等丰富的遗迹组合,包括Alcyonidiopsis ichnosp.,Chondrites intertricatus,几种Phycodes样结构,Phycosiphon incertum,Planarisichnosp.,变形虫罗沙奇线虫Scolicia ichnosp.,Taenidium barretti和Zoophycos ichnosp.底栖有孔虫和地质背景指向沉积上的…
Phytnatoderma is a complex, branching biogenic structure that is seldom mentioned in the ichnologic literature, although it may have been misidentified recently as “Zonarites” and large pellet‐filled “Chondrites”. The ichnogenus is usually interpreted as the product of subsurface deposit‐feeding animals. Well‐preserved examples from Pliocene slope mudstone in Ecuador are assignable to P. granulatum (Schlotheim, 1822). These structures are typically 30–40 cm in overall diameter; consist of outward‐branching, horizontal to subhorizontal, overlapping tunnels grouped in bundles; and have tunnel fills consisting of pelleted volcanic ash. The Ecuadorian Phymatoderma occur with a moderately rich ichnoassemblage that includes Alcyonidiopsis ichnosp., Chondrites intricatus, several kinds of Phycodes‐like structures, Phycosiphon incertum, Planolites ichnosp., Rorschachichnus amoeba, Scolicia ichnosp., Taenidium barretti, and Zoophycos ichnosp. Benthic foraminiferids and geologic context point to deposition on the u...
DOI: 10.2307/5527
发表时间: 1991-04
期刊: --
影响因子: --
作者:
J. Gage;P. Tyler
通讯作者: J. Gage;P. Tyler