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Early Triassic Archosaur-Dominated Footprint Assemblage from the Argana Basin (Western High Atlas, Morocco)

机译:Argana盆地(摩洛哥西部高图集)的早期三叠纪始祖龙占主导地位的足迹集合

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An assemblage of abundant and well-preserved tetrapod footprints has been discovered in the Tanamert Member (T3) of the Triassic Timezgadiouine Formation (Argana basin, western High Atlas, Morocco). It is the first fossil record from T3. Surfaces from different localities show a uniform tetrapod ichnofauna that consists of chirotherian and small lacertoid forms. The chirotherians are assigned to the plexus Protochirotherium—Synaptichnium, their trackmakers interpreted as basal archosaurs. The lacertoid imprints show close affinities with Rhynchosauroides and may reflect archosauromorphs or lepidosauromorphs. Protochirotherium—Synaptichnium assemblages are characteristic of the Early Triassic and were known previously only from units of this age in central Europe. Biostratigraphically, the European record implies a wide-spread pre-Anisian Protochirotherium—Synaptichnium dominated assemblage preceding the first appearance of Chirotherium barthii near the Olenekian-Anisian boundary. The stratigraphic position of T3 between Late Permian (uppermost T2) and Middle Triassic (T4) and the European correlatives suggest an Early Triassic age of this unit. It is the first record of Early Triassic continental deposits in Morocco. The surfaces from T3 open up perspectives for further contributions to ecology, biogeography and locomotion of early archosaurs. Furthermore, excellent outcrops and quality of footprint preservation in the Argana basin offer a potential for clarification of ichnotaxonomic and biostratigraphic issues.View full textDownload full textKeywords Protochirotherium , Synaptichnium , tetrapod footprints, red-beds, Northern AfricaRelated var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/10420940.2010.510030
机译:在三叠纪的Timezgadiouine组(摩洛哥阿格纳盆地,高阿特拉斯,摩洛哥)的Tanamert成员(T3)中发现了一系列丰富且保存完好的四足动物脚印。这是T3的第一个化石记录。来自不同地方的表面显示出均匀的四足鱼栖动物,由手足动物和小类类骆驼科动物组成。这些手足动物被分配到神经丛原手足动物– Synaptichnium,他们的追踪者被解释为基础恐龙。乳头状动物印记显示与Rhynchosaurouroides有密切的亲缘关系,并且可能反映archosauromorphes或lepidosauromorphes。 Protochirotherium–Synaptichnium组合是三叠纪早期的特征,以前仅在中欧这个年龄的单位中才知道。从生物地层学上看,欧洲记录暗示了在奥列尼克-阿尼西亚边界附近首次出现巴蒂奇氏酵母菌之前,广泛存在的前阿尼西亚原生质瘤-以突触小柱藻为主的组合。 T3在晚二叠世(最高T2)和中三叠纪(T4)之间的地层位置以及欧洲相关资料表明该单元的早三叠世年龄。这是摩洛哥早期三叠纪大陆沉积的第一记录。 T3的表面为早期考古学家的生态学,生物地理学和运动进一步发展开辟了前景。此外,Argana盆地出色的露头和脚印保存的质量为澄清鱼类分类学和生物地层学问题提供了潜力。查看全文下载全文关键字Protochirotherium,Synaptichnium,四足动物脚印,红床,北非相关var addthis_config = {ui_cobrand:“ Taylor &Francis Online”,services_compact:“ citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,更多”,发布号:“ ra-4dff56cd6bb1830b”};添加到候选列表链接永久链接http://dx.doi.org/10.1080/10420940.2010.510030

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