Enzien M V
Boston University, Department of Biology, MA 02215.
Biosystems. 1990;24(3):245-51. doi: 10.1016/0303-2647(90)90039-4.
Discovery and interpretation of a filamentous microfossil from the late Proterozoic Narssârssuk Formation in northwest Greenland approximately 770 Ma is reported here. This microfossil is preserved as a single occurrence in a silicified carbonate sequence containing stromatolitic laminae. Based on the absence of other occurrences and its microstratigraphic association with planktonic microfossils, the microfossil is interpreted as allochthonous. The microfossil is similar to two extant taxa representing different kingdoms: one prokaryote, Johannesbaptistia pellucida (cyanobacteria) and one eukaryote, Bangia sp. (rhodophytes). Definitive identification, due to the lack of distinctive morphology, could not be made.
本文报道了在格陵兰岛西北部约7.7亿年前的晚元古代纳尔斯苏克组发现并解释的一种丝状微化石。这种微化石保存在一个含有叠层石薄片的硅化碳酸盐序列中,仅出现一次。基于没有其他出现情况以及它与浮游微化石的微地层关联,该微化石被解释为异地的。该微化石类似于代表不同界的两个现存分类群:一种原核生物,透明约翰浸礼菌(蓝细菌)和一种真核生物,红毛菜属(红藻)。由于缺乏独特的形态,无法进行明确鉴定。