摘要
本文对最近从东太平洋深海锰结核中发现的“纳米级超微生物化石”提出了不同看法，并对今后研究工作提出了建议。由于太平洋螺旋孢菌和中华微放线菌在形态构造上存在多解性。
In this paper, some comments on the newly discovered “nanometer scale ultra microfossils ” (Spirisosphaerospora pacifica and Miniactinomyces chinensis) in pelagic manganese nodules from the East Pacific Ocean are made.Because the morphology of these “fossils” is uncertain,at present the evidence for a microbial origin and their biological affinities can not be regarded as conclusive.Much further work,therefore,is needed to clarify the true nature of these problematic microorganisms.
出处
《高校地质学报》
CAS
CSCD
1997年第1期115-117,共3页
Geological Journal of China Universities
关键词
深海
锰结核
纳米级
超微生物化石
pelagic manganese nodule,“nanometer scale ultra microfossil”, Spirisosphaerospora pacifica,Miniactinomyces chinensis.
