< p >是的,这是一个相当不错的发现;亚扪人的侏罗纪在中欧。给定样本的大小,它的外观,这似乎是物种的< em >心菊石属< / em >或< em > Perisphinctes。< / em >这些菊石类属于头足纲,盘绕头足类动物。他们生活在大约1.6亿年前。亚扪人的顺序,< em >心菊石属< / em >和< em > Perisphinctes < / em >属于叫做ammonitids,开始它们的进化路径在侏罗纪时期,盛行于三叠纪和白垩纪,然后在白垩纪末灭绝。的常见物种不同的子类,鹦鹉螺目动物,有关这些侏罗纪亚扪人。这是鹦鹉螺< / em > < em >,最原始的头足类动物,今天仍然生活。< / p > < p >的中心部分化石似乎硅化和石英。微弱的外部区域也这化石的一部分的外缘有一个保存部分的外壳是可见的。的中心部分化石显示了几个不同的< em > camerae。< / em >每个镜头形成的废弃的生活室壁随着动物的成长,形成了一个新的生活。 The last living chamber of this animal is likely the faint outer region surrounding the central quartz filled area. With some estimation, one may count approximately 16 or 17 previous living chambers, with the last (or 18th) being open. The host rock shows one other fragmentary view of an ammonite, readily seen by the distinct ridges of the corrugations in the shell. There are other fossil fragments also visible. They were not readily identified, however.