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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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North Africa
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Atlas Mountains
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Moroccan Atlas Mountains
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Anti-Atlas (1)
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Morocco
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Moroccan Atlas Mountains
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Anti-Atlas (1)
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Southern Africa
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Kaapvaal Craton (1)
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West Africa (1)
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West African Craton (1)
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Asia
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Far East
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China
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Guizhou China (2)
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Henan China (1)
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Inner Mongolia China (1)
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Ningxia China (2)
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North China Platform (4)
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Ordos Basin (1)
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Qaidam Basin (1)
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Qinghai China (3)
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Shaanxi China (2)
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Yunnan China (1)
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Siberia (3)
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Siberian Platform (2)
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Uchur River basin (1)
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Yakutia Russian Federation (1)
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Yudoma River (1)
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Commonwealth of Independent States
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Russian Federation
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Siberian Platform (2)
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Yakutia Russian Federation (1)
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Yudoma River (1)
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North America (1)
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elements, isotopes
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carbon
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C-13/C-12 (1)
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organic carbon (1)
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isotope ratios (1)
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isotopes
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stable isotopes
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C-13/C-12 (1)
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O-18/O-16 (1)
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Lu/Hf (1)
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oxygen
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O-18/O-16 (1)
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fossils
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Cloudina (1)
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ichnofossils (1)
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Invertebrata
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Protista
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Foraminifera (1)
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Metazoa (2)
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microfossils
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problematic microfossils (1)
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problematic fossils
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problematic microfossils (1)
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geochronology methods
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Lu/Hf (1)
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Pb/Pb (1)
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U/Pb (2)
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geologic age
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Paleozoic
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Cambrian
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Lower Cambrian
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Yudoma Series (1)
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Phanerozoic (1)
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Precambrian
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Archean
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upper Precambrian
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Proterozoic
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Huronian (1)
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Neoproterozoic
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Cryogenian (1)
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Dengying Formation (2)
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Ediacaran (10)
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Marinoan (1)
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Sturtian (1)
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Vendian (6)
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Paleoproterozoic
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Statherian (1)
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Sinian
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Dengying Formation (2)
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igneous rocks
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agglutinates (1)
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igneous rocks
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volcanic rocks
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basalts
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flood basalts (1)
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minerals
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carbonates
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dolomite (1)
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silicates
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orthosilicates
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nesosilicates
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zircon group
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zircon (2)
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sheet silicates
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clay minerals (1)
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sulfides
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pyrite (1)
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Primary terms
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absolute age (2)
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Africa
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North Africa
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Atlas Mountains
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Moroccan Atlas Mountains
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Anti-Atlas (1)
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Morocco
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Moroccan Atlas Mountains
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Anti-Atlas (1)
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Southern Africa
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Kaapvaal Craton (1)
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West Africa (1)
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West African Craton (1)
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Asia
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Far East
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China
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Guizhou China (2)
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Henan China (1)
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Inner Mongolia China (1)
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Ningxia China (2)
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North China Platform (4)
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Ordos Basin (1)
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Qaidam Basin (1)
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Qinghai China (3)
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Shaanxi China (2)
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Yunnan China (1)
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-
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Siberia (3)
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Siberian Platform (2)
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Uchur River basin (1)
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Yakutia Russian Federation (1)
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Yudoma River (1)
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carbon
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C-13/C-12 (1)
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organic carbon (1)
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geochronology (1)
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glacial geology (3)
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ichnofossils (1)
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igneous rocks
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volcanic rocks
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basalts
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flood basalts (1)
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Invertebrata
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Protista
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Foraminifera (1)
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-
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isotopes
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stable isotopes
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C-13/C-12 (1)
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O-18/O-16 (1)
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North America (1)
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orogeny (1)
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oxygen
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O-18/O-16 (1)
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paleoclimatology (1)
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paleoecology (1)
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paleogeography (3)
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Paleozoic
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Cambrian
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Lower Cambrian
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Yudoma Series (1)
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Phanerozoic (1)
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plate tectonics (2)
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Precambrian
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Archean
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Neoarchean (1)
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upper Precambrian
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Proterozoic
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Huronian (1)
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Neoproterozoic
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Cryogenian (1)
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Dengying Formation (2)
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Ediacaran (10)
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Marinoan (1)
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Sturtian (1)
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Vendian (6)
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Paleoproterozoic
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Statherian (1)
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Sinian
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Dengying Formation (2)
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problematic fossils
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problematic microfossils (1)
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remote sensing (1)
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sedimentary rocks
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carbonate rocks (1)
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chemically precipitated rocks
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chert (1)
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clastic rocks
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diamictite (3)
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stratigraphy (1)
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sedimentary rocks
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sedimentary rocks
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carbonate rocks (1)
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chemically precipitated rocks
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chert (1)
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clastic rocks
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diamictite (3)
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sedimentary structures
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striations (1)
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Zhengmuguan Formation
Representative photographs showing characteristics of stratigraphy and sedi...
PROBLEMATIC MACROFOSSILS FROM EDIACARAN SUCCESSIONS IN THE NORTH CHINA AND CHAIDAM BLOCKS: IMPLICATIONS FOR THEIR EVOLUTIONARY ROOTS AND BIOSTRATIGRAPHIC SIGNIFICANCE
Discussion of ‘First finds of problematic Ediacaran fossil Gaojiashania in Siberia and its origin’
Figure 6 —Measurements of 5 Horodyskia moniliformis ? specimens from the ...
Figure 5 —Measurements of 25 Helanoichnus helanensis specimens from the ...
Figure 4 — Helanoichnus helanensis Yang in Yang and Zheng, 1985 , from ...
Figure 10 —Thin sections of Helanoichnus helanensis from the Zhoujieshan...
Revisiting Ediacaran to early Cambrian depositional history of western North China: did it remain passive until the mid-Paleozoic?
Figure 8 — Palaeopascichnus minimus n. sp. ( 1–5 ); Palaeopascichnus men...
First finds of problematic Ediacaran fossil Gaojiashania in Siberia and its origin
Silicified Horodyskia and Palaeopascichnus from upper Ediacaran cherts in South China: tentative phylogenetic interpretation and implications for evolutionary stasis
Comparison of Horodyskia species. Bead size and spacing were measured on ...
New Ediacara-type fossils and late Ediacaran stratigraphy from the northern Qaidam Basin (China): Paleogeographic implications
Bird’s-eye view of an Ediacaran subglacial landscape
Duration of the first biozone in the Siberian hypostratotype of the Vendian
TAPHONOMY OF THE UPPER EDIACARAN ENIGMATIC RIBBONLIKE FOSSIL SHAANXILITHES
The role of glaciations in the biosphere
Newly discovered diamictite and cap carbonate couplet in the southern Alxa Block, northwestern China: Implications for stratigraphic correlation and Marinoan glaciation
Patterns of Evolution of the Ediacaran Soft-Bodied Biota
The Central Iapetus magmatic province: An updated review and link with the ca. 580 Ma Gaskiers glaciation
ABSTRACT Large igneous provinces and associated silicic magmatism can have a significant global climatic effect, so we explored the relationship between the large igneous province record and the ca. 580 Ma Gaskiers glaciation. The late Ediacaran glaciation exists on at least 14 different paleocontinental blocks, and assuming synchroneity, this Gaskiers glaciation was likely of short duration, with estimates ranging from 1.6 m.y. to 340 k.y. The Central Iapetus magmatic province event found in Laurentia, Baltica, and West Africa consists of multiple pulses in the range 620–520 Ma, with the ca. 580 Ma pulse particularly well developed in North Africa. Based on the age matches of 580–570 Ma Central Iapetus magmatic province pulses and the Gaskiers glaciation, and taking into consideration that there is no robust evidence for a major meteorite impact at the time of the Gaskiers onset, we propose that: (1) the initial silicic ca. 580 Ma pulse of the Ouarzazate event (Anti-Atlas of Morocco) helped to trigger the Gaskiers glaciation, and (2) global warming associated with the subsequent ca. 579–570 Ma continental flood basalts, marking the second stage of the Ouarzazate event, helped to end the ice age.