With stromatolite but no desiccation crack, the depositional environment of Middle-Late Cambrian in the area was intertidal zone to subtidal zone with the shallow-water features.
据其中
叠层石和无明显泥裂构造，
潮间带-局限潮
带沉积环境。
;
;
降,降低;With stromatolite but no desiccation crack, the depositional environment of Middle-Late Cambrian in the area was intertidal zone to subtidal zone with the shallow-water features.
据其中叠层石和无明显泥裂构造，潮间带-局限潮带沉积环境。
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