藏北日土地区南羌塘乌拉尔统曲地组孢粉化石的发现及意义OA
Discovery and significance of sporopollen fossils from the Cisuralian Qudi Formation in the South Qiangtang Block,Rutog area,northern Xizang
首次在藏北日土地区的南羌塘地层区乌拉尔统曲地组中获得孢粉化石.其中,裸子植物花粉含量(80.0%~88.6%)远高于蕨类植物孢子(11.4%~20.0%),又以双囊具肋花粉 Protohaploxypinus和单囊花粉 Potonieisporites最为突出,可称为Protohaploxypinus—Potonieisporites组合.该组合具有明显的亚安加拉植物群特征,同时包含冈瓦纳特征分子Plicatipollenites,这与保山、拉萨等地块上观察到的现象一致,表明早二叠世冈瓦纳区和亚安加拉区存在某些共有植物类群.造成这种植物群混生现象的原因可能是南羌塘、拉萨、保山等冈瓦纳北缘的裂离地块,在早二叠世大冰期后为双囊具肋花粉等微植物群通过"逐岛跳跃(island hopping)"方式进行洲际散布迁移提供了关键的媒介作用.
Dispersed palynomorphs from the Cisuralian Qudi Formation within the South Qiangtang stratigraphic region of Rutog area,northern Xizang,are reported here for the first time.Gymnosperm pollen(80.0%-88.6%)is significantly dominant over pteridophyte spores(11.4%-20.0%),with the bisaccate striate pollen Protohaploxypinus and monosaccate pollen Potonieisporites being the most prominent.This assemblage is designated as the Protohaploxypinus—Potonieisporites Assemblage.It exhibits distinct Sub-Angara floristic characteristics,while also containing the Gondwanan diagnostic taxon Plicatipollenites.This pattern aligns with observations from the Baoshan and Lhasa blocks,indicating shared plant taxa between the Gondwanan and Sub-Angaran realms during the Early Permian.The observed floral mixing likely resulted from Gondwana-affiliated rifted terranes(e.g.,South Qiangtang,Lhasa,and Baoshan blocks),serving as stepping stones for the"island hopping"dispersal of microfloras,such as bisaccate ribbed pollen,following the Early Permian deglaciation.
张予杰
中国地质调查局成都地质调查中心(西南地质科技创新中心),四川 成都 610218||中国地质调查局青藏高原地质研究中心,四川 成都 610218
天文与地球科学
孢粉化石乌拉尔统日土地区南羌塘地块
sporopollen fossilsCisuralianRutog areaSouth Qiangtang Block
《沉积与特提斯地质》 2026 (2)
288-298,11
中国地质调查局项目(D20250102609)国家自然科学基金项目(42241205,42473021)第二次青藏高原综合科学考察项目(2019QZKK0706)
评论