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Format
Article Type
Journal
Publisher
Section
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
-
Africa
-
Southern Africa
-
Kalahari Craton (1)
-
Namibia (13)
-
South Africa (2)
-
-
-
Arctic Ocean
-
Barents Sea
-
White Sea (1)
-
-
-
Arctic region (3)
-
Asia
-
Altai Mountains
-
Mongolian Altai (1)
-
-
Arabian Peninsula
-
Arabian Shield (1)
-
Oman (1)
-
-
Far East
-
China
-
Guizhou China (1)
-
Hubei China (1)
-
Meishan China (1)
-
South China Block (1)
-
Xizang China (1)
-
Yangtze Three Gorges (2)
-
Yunnan China
-
Jinning China (1)
-
-
-
Mongolia
-
Mongolian Altai (1)
-
-
-
Gobi Desert (1)
-
Himalayas
-
Lesser Himalayas (2)
-
Zanskar Range (2)
-
-
Indian Peninsula
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Bhutan (2)
-
India
-
Himachal Pradesh India
-
Kinnaur India (1)
-
Spiti (2)
-
-
Northeastern India
-
Nagaland India (1)
-
-
Punjab India (2)
-
Rajasthan India
-
Aravalli Range (1)
-
-
-
Indo-Gangetic Plain (1)
-
Pakistan
-
Punjab Pakistan
-
Salt Range (2)
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-
-
-
Krasnoyarsk Russian Federation (1)
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Main Central Thrust (1)
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Middle East
-
Dead Sea (1)
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Iran
-
Elburz (2)
-
Sanandaj-Sirjan Zone (1)
-
-
Jordan (1)
-
-
Siberia (8)
-
Siberian Platform
-
Yenisei Ridge (1)
-
-
Yakutia Russian Federation
-
Olenek River (2)
-
-
Yudoma River (1)
-
-
Australasia
-
Australia
-
New South Wales Australia (1)
-
South Australia
-
Adelaide Australia (1)
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Fleurieu Peninsula (1)
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Flinders Ranges (1)
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-
-
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Black Mountains (1)
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Caledonides (1)
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Canada
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Eastern Canada
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Maritime Provinces
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New Brunswick (1)
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Nova Scotia (3)
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-
Meguma Terrane (3)
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Newfoundland and Labrador
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Newfoundland
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Avalon Peninsula (1)
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Burin Peninsula (5)
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-
-
-
Mackenzie Mountains (2)
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Western Canada
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British Columbia
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Cariboo Mountains (1)
-
-
Canadian Cordillera (1)
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Canadian Rocky Mountains (1)
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Northwest Territories (2)
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Yukon Territory
-
Wernecke Mountains (1)
-
-
-
-
Commonwealth of Independent States
-
Russian Federation
-
Bashkortostan Russian Federation (1)
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Chelyabinsk Russian Federation (1)
-
Krasnoyarsk Russian Federation (1)
-
Siberian Platform
-
Yenisei Ridge (1)
-
-
Yakutia Russian Federation
-
Olenek River (2)
-
-
Yudoma River (1)
-
-
Ukraine
-
Podolia (1)
-
-
Urals
-
Southern Urals (1)
-
-
-
Death Valley (10)
-
Europe
-
Bashkortostan Russian Federation (1)
-
Central Europe
-
Poland
-
Swiety Krzyz Mountains (1)
-
-
-
Lapland (2)
-
Southern Europe
-
Iberian Peninsula
-
Central Iberian Zone (2)
-
Ossa-Morena Zone (1)
-
Spain
-
Iberian Mountains (1)
-
-
-
-
Ukraine
-
Podolia (1)
-
-
Western Europe
-
Scandinavia
-
Norway
-
Finnmark Norway
-
Tana Fjord (1)
-
-
Northern Norway (1)
-
-
Sweden
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Norrbotten Sweden
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Kiruna Sweden (1)
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Laisvall Sweden (1)
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-
-
-
United Kingdom
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Great Britain
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England
-
Leicestershire England (1)
-
-
Wales
-
Gwynedd Wales
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Harlech Dome (1)
-
-
-
-
-
-
-
Hartford Basin (1)
-
Mexico
-
Sonora Mexico (3)
-
-
North America
-
Appalachians
-
Northern Appalachians (1)
-
Southern Appalachians (1)
-
Valley and Ridge Province (1)
-
-
Basin and Range Province
-
Great Basin (3)
-
-
North American Cordillera
-
Canadian Cordillera (1)
-
-
Rocky Mountains
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Canadian Rocky Mountains (1)
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Central Rocky Mountains (1)
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-
-
Russian Platform (1)
-
South America
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Brazil
-
Minas Gerais Brazil (3)
-
Sao Francisco Basin (1)
-
Sao Francisco Craton (2)
-
-
Paraguay (1)
-
-
Spring Mountains (2)
-
United States
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California
-
Inyo County California
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Funeral Mountains (2)
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Inyo Mountains (1)
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Panamint Range (1)
-
-
Kingston Range (1)
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Nopah Range (3)
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San Bernardino County California (2)
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Southern California (1)
-
-
Great Basin (3)
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Massachusetts
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Hampden County Massachusetts (1)
-
-
Mojave Desert (1)
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Nevada
-
Esmeralda County Nevada (5)
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Nye County Nevada (2)
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Tennessee (1)
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White Mountains (2)
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commodities
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industrial minerals (1)
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metal ores
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copper ores (1)
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gold ores (1)
-
-
mineral deposits, genesis (1)
-
-
elements, isotopes
-
carbon
-
C-13 (1)
-
C-13/C-12 (21)
-
-
isotope ratios (21)
-
isotopes
-
stable isotopes
-
C-13 (1)
-
C-13/C-12 (21)
-
O-18/O-16 (4)
-
S-34/S-32 (2)
-
Sr-87/Sr-86 (3)
-
-
-
Lu/Hf (1)
-
metals
-
actinides
-
uranium (2)
-
-
alkaline earth metals
-
strontium
-
Sr-87/Sr-86 (3)
-
-
-
lead (1)
-
rare earths
-
neodymium (1)
-
samarium (1)
-
-
vanadium (1)
-
-
oxygen
-
O-18/O-16 (4)
-
-
sulfur
-
S-34/S-32 (2)
-
-
-
fossils
-
burrows (20)
-
Chordata
-
Vertebrata (1)
-
-
Cloudina (6)
-
cyanobacteria (1)
-
Graptolithina
-
Graptoloidea (1)
-
-
ichnofossils
-
Arenicolites (1)
-
Chondrites ichnofossils (1)
-
Cruziana (3)
-
Nereites (1)
-
Ophiomorpha (1)
-
Palaeophycus (1)
-
Planolites (4)
-
Rusophycus (1)
-
Skolithos (4)
-
Thalassinoides (1)
-
Zoophycos (1)
-
-
Invertebrata
-
Archaeocyatha (4)
-
Arthropoda
-
Mandibulata
-
Crustacea (1)
-
Insecta
-
Pterygota
-
Neoptera
-
Endopterygota
-
Diptera (1)
-
-
-
-
-
-
Trilobitomorpha
-
Trilobita
-
Agnostida (1)
-
-
-
-
Brachiopoda (1)
-
Cnidaria (1)
-
Echinodermata (1)
-
Mollusca (6)
-
Porifera (2)
-
Vermes
-
Annelida (1)
-
Chaetognatha (1)
-
Nematoida (1)
-
Priapulida (3)
-
-
-
lichens (1)
-
Metazoa (7)
-
microfossils
-
problematic microfossils (2)
-
-
palynomorphs
-
acritarchs (10)
-
-
Plantae
-
algae (3)
-
-
problematic fossils
-
problematic microfossils (2)
-
-
thallophytes (1)
-
tracks (1)
-
trails (5)
-
-
geochronology methods
-
Ar/Ar (1)
-
fission-track dating (1)
-
Lu/Hf (1)
-
paleomagnetism (1)
-
thermochronology (2)
-
U/Pb (19)
-
uranium disequilibrium (1)
-
-
geologic age
-
Cenozoic
-
Quaternary
-
Pleistocene (1)
-
-
Tertiary
-
Paleogene
-
Eocene
-
upper Eocene (1)
-
-
Oligocene
-
lower Oligocene (1)
-
-
-
-
-
Mesozoic
-
Jurassic
-
Lower Jurassic
-
East Berlin Formation (1)
-
-
Upper Jurassic (1)
-
-
Newark Supergroup (1)
-
Triassic (1)
-
-
Paleozoic
-
Cambrian
-
Lower Cambrian
-
Poleta Formation (2)
-
Rome Formation (1)
-
Terreneuvian
-
Fortunian (5)
-
-
Tommotian (3)
-
Yudoma Series (1)
-
-
Middle Cambrian (1)
-
Upper Cambrian
-
Goldenville Formation (2)
-
-
-
lower Paleozoic (6)
-
Ordovician
-
Lower Ordovician
-
Tremadocian
-
Halifax Formation (1)
-
-
-
-
Permian (1)
-
Sauk Sequence (1)
-
Silurian (1)
-
-
Phanerozoic (2)
-
Precambrian
-
Johnnie Formation (3)
-
Kingston Peak Formation (1)
-
Noonday Dolomite (3)
-
Pahrump Series (1)
-
Stirling Quartzite (4)
-
upper Precambrian
-
Proterozoic
-
Bambui Group (3)
-
Espinhaco Supergroup (1)
-
Mesoproterozoic (2)
-
Miette Group (1)
-
Neoproterozoic
-
Blaini Formation (1)
-
Cryogenian (3)
-
Dengying Formation (1)
-
Doushantuo Formation (2)
-
Ediacaran (68)
-
Macaubas Group (1)
-
Riphean
-
upper Riphean (1)
-
-
Tonian (2)
-
Vendian (22)
-
Wilpena Group (1)
-
-
Paleoproterozoic (1)
-
Sinian
-
Dengying Formation (1)
-
Doushantuo Formation (2)
-
-
Windermere System (2)
-
-
-
-
Vindhyan (1)
-
-
igneous rocks
-
igneous rocks
-
volcanic rocks
-
pyroclastics
-
tuff (2)
-
-
-
-
-
metamorphic rocks
-
metamorphic rocks
-
schists (1)
-
-
turbidite (3)
-
-
minerals
-
carbonates
-
dolomite (1)
-
-
oxides
-
chrome spinel (1)
-
-
phosphates (1)
-
silicates
-
orthosilicates
-
nesosilicates
-
garnet group (1)
-
zircon group
-
zircon (16)
-
-
-
-
sheet silicates
-
clay minerals (1)
-
mica group (1)
-
-
-
sulfates (1)
-
sulfides
-
pyrite (1)
-
-
-
Primary terms
-
absolute age (21)
-
Africa
-
Southern Africa
-
Kalahari Craton (1)
-
Namibia (13)
-
South Africa (2)
-
-
-
Arctic Ocean
-
Barents Sea
-
White Sea (1)
-
-
-
Arctic region (3)
-
Asia
-
Altai Mountains
-
Mongolian Altai (1)
-
-
Arabian Peninsula
-
Arabian Shield (1)
-
Oman (1)
-
-
Far East
-
China
-
Guizhou China (1)
-
Hubei China (1)
-
Meishan China (1)
-
South China Block (1)
-
Xizang China (1)
-
Yangtze Three Gorges (2)
-
Yunnan China
-
Jinning China (1)
-
-
-
Mongolia
-
Mongolian Altai (1)
-
-
-
Gobi Desert (1)
-
Himalayas
-
Lesser Himalayas (2)
-
Zanskar Range (2)
-
-
Indian Peninsula
-
Bhutan (2)
-
India
-
Himachal Pradesh India
-
Kinnaur India (1)
-
Spiti (2)
-
-
Northeastern India
-
Nagaland India (1)
-
-
Punjab India (2)
-
Rajasthan India
-
Aravalli Range (1)
-
-
-
Indo-Gangetic Plain (1)
-
Pakistan
-
Punjab Pakistan
-
Salt Range (2)
-
-
-
-
Krasnoyarsk Russian Federation (1)
-
Main Central Thrust (1)
-
Middle East
-
Dead Sea (1)
-
Iran
-
Elburz (2)
-
Sanandaj-Sirjan Zone (1)
-
-
Jordan (1)
-
-
Siberia (8)
-
Siberian Platform
-
Yenisei Ridge (1)
-
-
Yakutia Russian Federation
-
Olenek River (2)
-
-
Yudoma River (1)
-
-
Australasia
-
Australia
-
New South Wales Australia (1)
-
South Australia
-
Adelaide Australia (1)
-
Fleurieu Peninsula (1)
-
Flinders Ranges (1)
-
-
-
-
bibliography (1)
-
biogeography (5)
-
Canada
-
Eastern Canada
-
Maritime Provinces
-
New Brunswick (1)
-
Nova Scotia (3)
-
-
Meguma Terrane (3)
-
Newfoundland and Labrador
-
Newfoundland
-
Avalon Peninsula (1)
-
Burin Peninsula (5)
-
-
-
-
Mackenzie Mountains (2)
-
Western Canada
-
British Columbia
-
Cariboo Mountains (1)
-
-
Canadian Cordillera (1)
-
Canadian Rocky Mountains (1)
-
Northwest Territories (2)
-
Yukon Territory
-
Wernecke Mountains (1)
-
-
-
-
carbon
-
C-13 (1)
-
C-13/C-12 (21)
-
-
Cenozoic
-
Quaternary
-
Pleistocene (1)
-
-
Tertiary
-
Paleogene
-
Eocene
-
upper Eocene (1)
-
-
Oligocene
-
lower Oligocene (1)
-
-
-
-
-
Chordata
-
Vertebrata (1)
-
-
continental drift (1)
-
diagenesis (1)
-
Europe
-
Bashkortostan Russian Federation (1)
-
Central Europe
-
Poland
-
Swiety Krzyz Mountains (1)
-
-
-
Lapland (2)
-
Southern Europe
-
Iberian Peninsula
-
Central Iberian Zone (2)
-
Ossa-Morena Zone (1)
-
Spain
-
Iberian Mountains (1)
-
-
-
-
Ukraine
-
Podolia (1)
-
-
Western Europe
-
Scandinavia
-
Norway
-
Finnmark Norway
-
Tana Fjord (1)
-
-
Northern Norway (1)
-
-
Sweden
-
Norrbotten Sweden
-
Kiruna Sweden (1)
-
Laisvall Sweden (1)
-
-
-
-
United Kingdom
-
Great Britain
-
England
-
Leicestershire England (1)
-
-
Wales
-
Gwynedd Wales
-
Harlech Dome (1)
-
-
-
-
-
-
-
faults (3)
-
folds (1)
-
geochemistry (4)
-
geochronology (3)
-
glacial geology (4)
-
Graptolithina
-
Graptoloidea (1)
-
-
ichnofossils
-
Arenicolites (1)
-
Chondrites ichnofossils (1)
-
Cruziana (3)
-
Nereites (1)
-
Ophiomorpha (1)
-
Palaeophycus (1)
-
Planolites (4)
-
Rusophycus (1)
-
Skolithos (4)
-
Thalassinoides (1)
-
Zoophycos (1)
-
-
igneous rocks
-
volcanic rocks
-
pyroclastics
-
tuff (2)
-
-
-
-
industrial minerals (1)
-
Invertebrata
-
Archaeocyatha (4)
-
Arthropoda
-
Mandibulata
-
Crustacea (1)
-
Insecta
-
Pterygota
-
Neoptera
-
Endopterygota
-
Diptera (1)
-
-
-
-
-
-
Trilobitomorpha
-
Trilobita
-
Agnostida (1)
-
-
-
-
Brachiopoda (1)
-
Cnidaria (1)
-
Echinodermata (1)
-
Mollusca (6)
-
Porifera (2)
-
Vermes
-
Annelida (1)
-
Chaetognatha (1)
-
Nematoida (1)
-
Priapulida (3)
-
-
-
isotopes
-
stable isotopes
-
C-13 (1)
-
C-13/C-12 (21)
-
O-18/O-16 (4)
-
S-34/S-32 (2)
-
Sr-87/Sr-86 (3)
-
-
-
lichens (1)
-
Mesozoic
-
Jurassic
-
Lower Jurassic
-
East Berlin Formation (1)
-
-
Upper Jurassic (1)
-
-
Newark Supergroup (1)
-
Triassic (1)
-
-
metal ores
-
copper ores (1)
-
gold ores (1)
-
-
metals
-
actinides
-
uranium (2)
-
-
alkaline earth metals
-
strontium
-
Sr-87/Sr-86 (3)
-
-
-
lead (1)
-
rare earths
-
neodymium (1)
-
samarium (1)
-
-
vanadium (1)
-
-
metamorphic rocks
-
schists (1)
-
-
metamorphism (1)
-
metasomatism (1)
-
Mexico
-
Sonora Mexico (3)
-
-
mineral deposits, genesis (1)
-
North America
-
Appalachians
-
Northern Appalachians (1)
-
Southern Appalachians (1)
-
Valley and Ridge Province (1)
-
-
Basin and Range Province
-
Great Basin (3)
-
-
North American Cordillera
-
Canadian Cordillera (1)
-
-
Rocky Mountains
-
Canadian Rocky Mountains (1)
-
Central Rocky Mountains (1)
-
-
-
orogeny (4)
-
oxygen
-
O-18/O-16 (4)
-
-
paleoclimatology (3)
-
paleoecology (30)
-
paleogeography (20)
-
paleomagnetism (1)
-
paleontology (2)
-
Paleozoic
-
Cambrian
-
Lower Cambrian
-
Poleta Formation (2)
-
Rome Formation (1)
-
Terreneuvian
-
Fortunian (5)
-
-
Tommotian (3)
-
Yudoma Series (1)
-
-
Middle Cambrian (1)
-
Upper Cambrian
-
Goldenville Formation (2)
-
-
-
lower Paleozoic (6)
-
Ordovician
-
Lower Ordovician
-
Tremadocian
-
Halifax Formation (1)
-
-
-
-
Permian (1)
-
Sauk Sequence (1)
-
Silurian (1)
-
-
palynomorphs
-
acritarchs (10)
-
-
petrology (1)
-
Phanerozoic (2)
-
Plantae
-
algae (3)
-
-
plate tectonics (4)
-
Precambrian
-
Johnnie Formation (3)
-
Kingston Peak Formation (1)
-
Noonday Dolomite (3)
-
Pahrump Series (1)
-
Stirling Quartzite (4)
-
upper Precambrian
-
Proterozoic
-
Bambui Group (3)
-
Espinhaco Supergroup (1)
-
Mesoproterozoic (2)
-
Miette Group (1)
-
Neoproterozoic
-
Blaini Formation (1)
-
Cryogenian (3)
-
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1-20 OF 205 RESULTS FOR
Treptichnus pedum
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Journal Article
Treptichnus pedum and the Ediacaran–Cambrian boundary: significance and caveats Available to Purchase
Journal: Geological Magazine
Publisher: Cambridge University Press
Published: 22 August 2017
Geological Magazine (2018) 155 (1): 174–180.
...LUIS A. BUATOIS Abstract The Ediacaran–Cambrian (E-C) boundary is based on the first appearance of the ichnofossil Treptichnus pedum . Investing an ichnotaxon with such biostratigraphic pre-eminence has been the focus of criticism. Points of contention have revolved around four main issues: (1...
Journal Article
Environmental tolerance and range offset of Treptichnus pedum : Implications for the recognition of the Ediacaran-Cambrian boundary Available to Purchase
Journal: Geology
Publisher: Geological Society of America
Published: 01 April 2013
Geology (2013) 41 (4): 519–522.
...Luis A. Buatois; John Almond; Gerard J.B. Germs Abstract The Ediacaran-Cambrian boundary, arguably the most important in the stratigraphic column, is based on the first appearance of the ichnospecies Treptichnus pedum . However, most trace fossils have long temporal ranges and occur in a narrow...
Journal Article
DEEP-WATER INCISED VALLEY DEPOSITS AT THE EDIACARAN-CAMBRIAN BOUNDARY IN SOUTHERN NAMIBIA CONTAIN ABUNDANT TREPTICHNUS PEDUM Available to Purchase
JONATHAN P. WILSON, JOHN P. GROTZINGER, WOODWARD W. FISCHER, KEVIN P. HAND, SÖREN JENSEN, ANDREW H. KNOLL, JOHN ABELSON, JOANNAH M. METZ, NICOLA MCLOUGHLIN, PHOEBE A. COHEN, MICHAEL M. TICE
Journal: PALAIOS
Publisher: SEPM Society for Sedimentary Geology
Published: 01 April 2012
PALAIOS (2012) 27 (4): 252–273.
... Treptichnus pedum. Facies analysis shows that T. pedum is closely linked to a nearshore sandstone deposit, indicating a close environmental or taphonomic connection to very shallow, mud-draped sandy seafloor swept by tidal currents. Facies restriction may limit the biostratigraphic potential of T. pedum...
Image
Complex burrowing traces from Chicago Pass. A ) Treptichnus pedum (Spec.... Available to Purchase
in THE ROLE OF SURFICIAL BIOTURBATION IN THE LATEST EDIACARAN: A QUANTITATIVE ANALYSIS OF TRACE FOSSIL INTENSITY IN THE TERMINAL EDIACARAN–LOWER CAMBRIAN OF CALIFORNIA
> PALAIOS
Published: 29 December 2022
Fig. 6 Complex burrowing traces from Chicago Pass. A ) Treptichnus pedum (Spec. ID: CP.511-LT3). B ) Unidentified treptichnid (Spec. ID: CP.481.6-LT1). C ) Treptichnus bifurcus (Spec ID: CP.481.2-LT1). D ) Cross-section view of C showing burrow troughs and infilled burrows. E ) Cross
Image
Variations in Treptichnus pedum preservation in relation to different typ... Available to Purchase
in The Ediacaran–Cambrian Chapel Island Formation of Newfoundland, Canada: evaluating the impact of outcrop quality on trace-fossil data sets at the Cambrian GSSP and less-explored sections
> Canadian Journal of Earth Sciences
Published: 23 December 2022
Fig. 5. Variations in Treptichnus pedum preservation in relation to different types of outcrop exposure. Scale bars are 1 cm. ( a ) Bed base with segments extending laterally on a flat, well exposed surface. Positive hyporelief, Grand Bank Head, M2A. ( b ) Oblique weathering of a bed top
Image
Morphology of Treptichnus pedum . (a) Specimen from the type locality. Nob... Available to Purchase
in Treptichnus pedum and the Ediacaran–Cambrian boundary: significance and caveats
> Geological Magazine
Published: 22 August 2017
Figure 1. Morphology of Treptichnus pedum . (a) Specimen from the type locality. Nobulus Shale, lower Cambrian, Salt Range, Pakistan. Specimen housed at the Palaeontological Collection, Geologisches Institut, University of Tübingen, Germany. (b) Klipbak Formations, Brandkop Subgroup, lower
Image
Size distributions of Planolites from the Treptichnus pedum and Rusoph... Available to Purchase
in Diachronous Increase in Early Cambrian Ichnofossil Size and Benthic Faunal Activity in Different Climatic Regions
> Journal of Paleontology
Published: 01 March 2014
Figure 2 Size distributions of Planolites from the Treptichnus pedum and Rusophycus avalonensis zones of the three study areas.
Image
Bedding plane bioturbation indices (BPBI) from the Treptichnus pedum and ... Available to Purchase
in Diachronous Increase in Early Cambrian Ichnofossil Size and Benthic Faunal Activity in Different Climatic Regions
> Journal of Paleontology
Published: 01 March 2014
Figure 3 Bedding plane bioturbation indices (BPBI) from the Treptichnus pedum and Rusophycus avalonensis zones of the three study areas. Numbers in the pie charts show the percentages of bedding planes that are classified under each bioturbation index. Upper left, Torrowangea isp. from
Image
Examples of Treptichnus pedum in Fortunian units of Vanrhynsdorp Group (S... Available to Purchase
in Environmental tolerance and range offset of Treptichnus pedum : Implications for the recognition of the Ediacaran-Cambrian boundary
> Geology
Published: 01 April 2013
Figure 1. Examples of Treptichnus pedum in Fortunian units of Vanrhynsdorp Group (South Africa). All scale bars are 1 cm long. A: Specimen showing classic branching pattern, from upper offshore deposits, Klipbak Formation. B: Specimen showing looping, from upper offshore deposits, Klipbak
Image
Treptichnus pedum response curve based on occurrences in Vanrhynsdorp Grou... Available to Purchase
in Environmental tolerance and range offset of Treptichnus pedum : Implications for the recognition of the Ediacaran-Cambrian boundary
> Geology
Published: 01 April 2013
Figure 3. Treptichnus pedum response curve based on occurrences in Vanrhynsdorp Group (South Africa). A: Wave-dominated shallow-marine clastic gradient. Ab—absent; A—abundant (more than 30 specimens); C—common (30–5); R—rare (fewer than 5). B: Tide-dominated shallow-marine clastic gradient.
Image
Treptichnus pedum preserved on sandstone bed soles. A–B) Specimen with curv... Available to Purchase
in DEEP-WATER INCISED VALLEY DEPOSITS AT THE EDIACARAN-CAMBRIAN BOUNDARY IN SOUTHERN NAMIBIA CONTAIN ABUNDANT TREPTICHNUS PEDUM
> PALAIOS
Published: 01 April 2012
F igure 12— Treptichnus pedum preserved on sandstone bed soles. A–B) Specimen with curved portions in which the segments project outwards, resulting in an appearance that has been compared to a crosier. C, D, F) Specimens in which vertically oriented portions are preferentially preserved. E
Image
Treptichnus pedum preserved on sandstone bed soles. A–D) Curved specimens s... Available to Purchase
in DEEP-WATER INCISED VALLEY DEPOSITS AT THE EDIACARAN-CAMBRIAN BOUNDARY IN SOUTHERN NAMIBIA CONTAIN ABUNDANT TREPTICHNUS PEDUM
> PALAIOS
Published: 01 April 2012
F igure 13— Treptichnus pedum preserved on sandstone bed soles. A–D) Curved specimens showing differences in the spacing of vertical probes. Note zigzag development of burrow in upper part of C. E–F) Specimens largely preserved as disjunct probes, in places showing a three-lobed basal surface.
Image
Treptichnus pedum preserved on sandstone bed soles, with examples of specim... Available to Purchase
in DEEP-WATER INCISED VALLEY DEPOSITS AT THE EDIACARAN-CAMBRIAN BOUNDARY IN SOUTHERN NAMIBIA CONTAIN ABUNDANT TREPTICHNUS PEDUM
> PALAIOS
Published: 01 April 2012
F igure 14— Treptichnus pedum preserved on sandstone bed soles, with examples of specimens with a three-lobed basal surface and narrow lateral lobes with a fine transverse ornamentation. E is a close-up of central area in D. G shows burrow segments in upper part of F with a different orientation
Image
A–C) Top surface of sandstone bed covered with Treptichnus pedum preserved ... Available to Purchase
in DEEP-WATER INCISED VALLEY DEPOSITS AT THE EDIACARAN-CAMBRIAN BOUNDARY IN SOUTHERN NAMIBIA CONTAIN ABUNDANT TREPTICHNUS PEDUM
> PALAIOS
Published: 01 April 2012
F igure 15— A–C) Top surface of sandstone bed covered with Treptichnus pedum preserved as grooves. B is a close-up of top area in A. Hammerhead in A is 24 mm wide. Furrows in C are about 5 mm wide.
Image
Figure 3. A: Treptichnus pedum on base of sandstone bed, Early Cambrian M... Available to Purchase
Published: 01 February 2000
Figure 3. A: Treptichnus pedum on base of sandstone bed, Early Cambrian Mickwitzia sandstone member, File Haidar Formation, Lugnås, Västergötland, Sweden (Sedgwick Museum, Cambridge, x29339). Scale bar = 10 mm. B, C: Change in morphology of trepthichnid as result of lowering plane
Journal Article
Ichnostratigraphy of the Ediacaran-Cambrian boundary: new insights on lower Cambrian biozonations from the Soltanieh Formation of northern Iran Available to Purchase
Journal: Journal of Paleontology
Publisher: Paleontological Society
Published: 12 September 2017
Journal of Paleontology (2017) 91 (6): 1178–1198.
..., containing Helminthoidichnites tenuis , Helminthopsis tenuis , and Cochlichnus anguineus , is early Fortunian based on small shelly fossils, and is interpreted as a distal expression of the Treptichnus pedum zone. Ichnozone 2, comprising the first occurrence of T . pedum , is middle Fortunian, and is best...
Journal Article
Burrowing below the basal Cambrian GSSP, Fortune Head, Newfoundland Available to Purchase
Journal: Geological Magazine
Publisher: Cambridge University Press
Published: 01 March 2001
Geological Magazine (2001) 138 (2): 213–218.
...JAMES G. GEHLING; SÖREN JENSEN; MARY L. DROSER; PAUL M. MYROW; GUY M. NARBONNE Abstract The range of Treptichnus pedum , the index trace fossil for the Treptichnus pedum Zone, extends some 4 m below the Global Standard Stratotype-section and Point for the base of the Cambrian Period at Fortune...
Journal Article
The Ediacaran–Cambrian Chapel Island Formation of Newfoundland, Canada: evaluating the impact of outcrop quality on trace-fossil data sets at the Cambrian GSSP and less-explored sections Available to Purchase
Romain Gougeon, M. Gabriela Mángano, Luis A. Buatois, Guy M. Narbonne, Brittany A. Laing, Maximiliano Paz
Journal: Canadian Journal of Earth Sciences
Publisher: Canadian Science Publishing
Published: 23 December 2022
Canadian Journal of Earth Sciences (2023) 60 (7): 897–911.
...Fig. 5. Variations in Treptichnus pedum preservation in relation to different types of outcrop exposure. Scale bars are 1 cm. ( a ) Bed base with segments extending laterally on a flat, well exposed surface. Positive hyporelief, Grand Bank Head, M2A. ( b ) Oblique weathering of a bed top...
Journal Article
Tulaneia amabilia n. gen. n. sp.: a new erniettomorph from the Wood Canyon Formation, Nevada and the age of the Ediacaran–Cambrian transition in the Great Basin Open Access
Bruce Runnegar, Robert J. Horodyski, James G. Gehling, Sören Jensen, Stefan Bengtson, Kevin J. Peterson, Matthew R. Saltzman, Michael J. Vendrasco
Journal: Journal of Paleontology
Publisher: Paleontological Society
Published: 01 November 2024
Journal of Paleontology (2024) 98 (6): 929–951.
...) was confirmed by subsequent discoveries. Because the upper part of the LMWCF contains Treptichnus pedum (Seilacher), the Ediacaran–Cambrian boundary has long been drawn at its first appearance. However, in the Esmeralda Member of the Deep Spring Formation in the White-Inyo Mountains, California, and at Mount...
Journal Article
Distribution and correlation of Sabellidites cambriensis (Annelida?) in the basal Cambrian on Baltica Open Access
Jan Ove R. Ebbestad, Frida Hybertsen, Anette E. S. Högström, Sören Jensen, Teodoro Palacios, Wendy L. Taylor, Heda Agić, Magne Høyberget, Guido Meinhold
Journal: Geological Magazine
Publisher: Cambridge University Press
Published: 09 December 2021
Geological Magazine (2022) 159 (7): 1262–1283.
.... Here, the Ediacaran–Cambrian boundary is located in the lower part of the upper parasequence (third cycle) of the Manndrapselva Member. Specimens of Sabellidites are rare but consistently present close to the lowest level of Treptichnus pedum and upsection, whereas the taxon is common and abundant...
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