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all geography including DSDP/ODP Sites and Legs
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Asia
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metals
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alkaline earth metals
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noble gases
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argon
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Ar-36 (1)
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helium
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krypton
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Kr-84 (1)
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neon
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Ne-20 (1)
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oxygen
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O-18/O-16 (8)
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sulfur
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organic sulfur (1)
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fossils
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Chordata
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Vertebrata
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Tetrapoda
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Mammalia
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Theria
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Eutheria
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Mammutidae (1)
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Rodentia
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fossil man (1)
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ichnofossils
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Skolithos (1)
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Invertebrata
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Arthropoda
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Chelicerata
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Mandibulata
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Crustacea
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Ostracoda (2)
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Brachiopoda
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Inarticulata (1)
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Cnidaria
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Anthozoa
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Echinodermata
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Porifera
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Stromatoporoidea
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Protista
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Foraminifera (1)
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Conodonta (6)
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palynomorphs
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Plantae
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Pteridophyta
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problematic fossils (1)
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thallophytes (2)
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geochronology methods
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paleomagnetism (2)
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thermochronology (1)
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geologic age
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Cenozoic
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Quaternary
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Holocene (2)
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Pleistocene
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upper Pleistocene
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Weichselian
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upper Weichselian
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Younger Dryas (1)
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Tertiary
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Neogene
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Miocene (2)
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Pliocene
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lower Pliocene
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Zanclean (1)
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Paleogene
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Eocene
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lower Eocene
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Ypresian (1)
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Paleocene
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lower Paleocene
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K-T boundary (1)
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upper Cenozoic (1)
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Mesozoic
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Cretaceous
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Dakota Formation (1)
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Lower Cretaceous
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Albian (1)
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Aptian (1)
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McMurray Formation (7)
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Mancos Shale (1)
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Potomac Group (1)
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Upper Cretaceous
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Cenomanian
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lower Cenomanian (1)
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Fox Hills Formation (2)
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Eagle Ford Formation (1)
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K-T boundary (1)
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Maestrichtian (2)
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Niobrara Formation (1)
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Senonian (2)
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Glen Canyon Group (1)
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Great Valley Sequence (1)
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Jurassic
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Middle Jurassic (2)
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San Rafael Group (1)
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Upper Jurassic
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Entrada Sandstone (1)
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Morrison Formation (2)
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Sundance Formation (1)
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Navajo Sandstone (1)
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Triassic
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Moenkopi Formation (1)
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Upper Triassic
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Chinle Formation (1)
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Paleozoic
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Cambrian
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Lower Cambrian
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Zabriskie Quartzite (1)
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Middle Cambrian (1)
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Upper Cambrian
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Potsdam Sandstone (4)
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Carboniferous
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Lower Carboniferous (1)
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Mississippian
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Lower Mississippian
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Osagian (1)
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Pocono Formation (1)
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Madison Group (2)
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Upper Mississippian
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Serpukhovian (1)
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Pennsylvanian
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Conemaugh Group (1)
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Lower Pennsylvanian
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Middle Pennsylvanian
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Allegheny Group (1)
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Monongahela Group (1)
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Upper Pennsylvanian
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Gzhelian (1)
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Kasimovian (1)
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Virgilian
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Wabaunsee Group (1)
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-
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-
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Chattanooga Shale (1)
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Devonian
-
Beaverhill Lake Group (6)
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Keg River Formation (2)
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Middle Devonian
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Elk Point Group (7)
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Givetian
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Horn Plateau Formation (1)
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Marcellus Shale (1)
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Prairie Evaporite (11)
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Winnipegosis Formation (10)
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Slave Point Formation (2)
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Swan Hills Formation (4)
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Upper Devonian
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Birdbear Formation (1)
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Famennian
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Wabamun Group (1)
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Frasnian (3)
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Grosmont Formation (1)
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Nisku Formation (1)
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Ohio Shale (1)
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Waterways Formation (2)
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Dunkard Group (1)
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Exshaw Formation (1)
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lower Paleozoic (1)
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Maroon Formation (1)
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New Albany Shale (1)
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Ordovician
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Lower Ordovician
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Saint George Group (2)
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Tremadocian (2)
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Martinsburg Formation (1)
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Middle Ordovician (2)
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Utica Shale (1)
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Permian
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Council Grove Group (1)
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Guadalupian
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Tansill Formation (1)
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Lower Permian
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Cisuralian
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Artinskian (1)
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Asselian (1)
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Kungurian (1)
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Sakmarian (1)
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-
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Upper Permian
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Zechstein (1)
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Yates Formation (1)
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Road River Formation (1)
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Silurian
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Middle Silurian
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Guelph Formation (1)
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Upper Silurian
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Salina Group (1)
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Supai Formation (1)
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upper Paleozoic
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Admire Group (1)
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Bakken Formation (2)
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Phanerozoic (1)
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Precambrian
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upper Precambrian
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Proterozoic
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Neoproterozoic
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Ediacaran (3)
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Vendian (1)
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metamorphic rocks
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metamorphic rocks
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impactites (1)
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metasedimentary rocks (1)
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minerals
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carbonates
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calcite (3)
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dolomite (4)
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chlorides
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carnallite (1)
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halite (7)
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oxides
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hematite (1)
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iron oxides (1)
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phosphates
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silicates
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framework silicates
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feldspar group
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alkali feldspar
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silica minerals
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quartz (2)
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orthosilicates
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nesosilicates
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-
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sulfates
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anhydrite (12)
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gypsum (2)
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Primary terms
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absolute age (2)
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Arctic region (1)
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Asia
-
Far East
-
China
-
Guizhou China (1)
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-
Indonesia (1)
-
-
Indian Peninsula
-
India
-
Rajasthan India (1)
-
-
Indus Basin (1)
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Pakistan (1)
-
-
Southeast Asia (1)
-
-
Atlantic Ocean
-
North Atlantic
-
Caribbean Sea (1)
-
North Sea (2)
-
-
-
Australasia
-
Australia
-
South Australia
-
Flinders Ranges (1)
-
-
Western Australia
-
Carnarvon Basin (1)
-
-
-
-
bibliography (1)
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biography (1)
-
brines (3)
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Canada
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Arctic Archipelago (2)
-
Cold Lake (1)
-
Eastern Canada
-
Newfoundland and Labrador
-
Newfoundland
-
Great Northern Peninsula (1)
-
Port au Port Peninsula (2)
-
-
-
Ontario (2)
-
Quebec
-
Anticosti Island (1)
-
-
-
Elk Point Basin (6)
-
Mackenzie Mountains (1)
-
Nunavut
-
Ellesmere Island (2)
-
Sverdrup Basin (1)
-
-
Queen Elizabeth Islands
-
Ellesmere Island (2)
-
Sverdrup Basin (1)
-
-
Richardson Mountains (2)
-
Selwyn Mountains (1)
-
Western Canada
-
Alberta
-
Alberta Basin (2)
-
Athabasca Oil Sands (9)
-
Peace River Arch (1)
-
-
British Columbia (5)
-
Manitoba (4)
-
Northwest Territories
-
Great Slave Lake (1)
-
-
Saskatchewan
-
Esterhazy Saskatchewan (1)
-
-
Yukon Territory
-
Wernecke Mountains (1)
-
-
-
-
carbon
-
C-13/C-12 (11)
-
C-14 (1)
-
-
Cenozoic
-
Quaternary
-
Holocene (2)
-
Pleistocene
-
upper Pleistocene
-
Weichselian
-
upper Weichselian
-
Younger Dryas (1)
-
-
-
-
-
-
Tertiary
-
Neogene
-
Miocene (2)
-
Pliocene
-
lower Pliocene
-
Zanclean (1)
-
-
-
-
Paleogene
-
Eocene
-
lower Eocene
-
Ypresian (1)
-
-
-
Paleocene
-
lower Paleocene
-
K-T boundary (1)
-
-
-
-
-
upper Cenozoic (1)
-
-
Central America
-
Belize (1)
-
-
Chordata
-
Vertebrata
-
Tetrapoda
-
Mammalia
-
Theria
-
Eutheria
-
Proboscidea
-
Mastodontoidea
-
Mammutidae (1)
-
-
-
Rodentia
-
Castoridae (1)
-
-
-
-
-
-
-
-
climate change (2)
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continental shelf (1)
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crust (1)
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dams (2)
-
data processing (4)
-
deformation (2)
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diagenesis (22)
-
earthquakes (1)
-
East Pacific Ocean Islands
-
Hawaii
-
Hawaii County Hawaii
-
Hawaii Island
-
Hualalai (1)
-
Kilauea (1)
-
Kohala (1)
-
Mauna Kea (1)
-
-
-
Mauna Loa (1)
-
-
-
economic geology (10)
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energy sources (2)
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epeirogeny (1)
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Europe
-
Arkhangelsk Russian Federation
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Nenets Russian Federation (1)
-
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Western Europe
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United Kingdom
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Great Britain
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England (1)
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-
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evaporite deposits (1)
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faults (10)
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Elk Mound Group
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Image
Protichnites eremita Form 2, Trackways A and B, Elk Mound Group, Blackberry...
in Protichnites eremita Unshelled? Experimental Model-Based Neoichnology and New Evidence for A Euthycarcinoid Affinity for This Ichnospecies
> Journal of Paleontology
Published: 01 May 2012
F igure 1 Protichnites eremita Form 2, Trackways A and B, Elk Mound Group, Blackberry Hill, Wisconsin, PRI Station 3421. 1 , PRI 10143, both trackways shown, Trackway B exhibits a sharp right turn whereas Trackway A exhibits a gentle turn; segmentation present in the intermittent medial
Image
Elk Mound Group fossils, Blackberry Hill, Wisconsin, PRI Station 3421. 1 ,...
in Protichnites eremita Unshelled? Experimental Model-Based Neoichnology and New Evidence for A Euthycarcinoid Affinity for This Ichnospecies
> Journal of Paleontology
Published: 01 May 2012
F igure 2 Elk Mound Group fossils, Blackberry Hill, Wisconsin, PRI Station 3421. 1 , PRI 11041, Protichnites eremita Form 2, Trackway E, (p = postabdominal imprint, s = segment, t = track); arrow indicates likely direction of travel; 2 , Arenosicaris inflata (phyllocarid crustacean), showing
Image
Figure 4. 1 , Arenosicaris inflata from the Furongian Elk Mound Group of...
in Early Evolution of Phyllocarid Arthropods: Phylogeny and Systematics of Cambrian-Devonian Archaeostracans
> Journal of Paleontology
Published: 01 September 2010
Figure 4. 1 , Arenosicaris inflata from the Furongian Elk Mound Group of Wisconsin – PRI–1013: 1a–c ( a at top, c at bottom), three phyllocarids; two partial, and one complete; 2 , Ceratiocaris acuminata , PE-664, inset image (YPM 212400) shows a telson with a row of small pits where
Image
Figure 1. Elk Mound Group channel deposits where traces and body fossils of...
in DEAD IN THEIR TRACKS—CAMBRIAN ARTHROPODS AND THEIR TRACES FROM INTERTIDAL SANDSTONES OF QUEBEC AND WISCONSIN
> PALAIOS
Published: 01 August 2010
Figure 1. Elk Mound Group channel deposits where traces and body fossils of their producers co-occur. A) Large channel cutting through an Elk Mound Group tidal flat. Rock hammer (arrowed) is 28 cm long. B) Part of a large phyllocarid-bearing slab from the horizon that infills the surface visible
Image
Figure 5. Ropelike Elk Mound Group traces. A) Circular, looping ropelike fo...
in DEAD IN THEIR TRACKS—CAMBRIAN ARTHROPODS AND THEIR TRACES FROM INTERTIDAL SANDSTONES OF QUEBEC AND WISCONSIN
> PALAIOS
Published: 01 August 2010
Figure 5. Ropelike Elk Mound Group traces. A) Circular, looping ropelike form A shallow surface trace on bed sole. Note Y-shaped impressions (arrowed), lateral furrows ( = lf), and characteristic ropy outline (outlined). B) Close-up photograph of the left side of Fig. 5A , note well-defined Y
Image
Figure 6. Ropelike form B traces from the Elk Mound Group. A) Map of a larg...
in DEAD IN THEIR TRACKS—CAMBRIAN ARTHROPODS AND THEIR TRACES FROM INTERTIDAL SANDSTONES OF QUEBEC AND WISCONSIN
> PALAIOS
Published: 01 August 2010
Figure 6. Ropelike form B traces from the Elk Mound Group. A) Map of a large outcrop surface (5 × 3 m) showing exposure of three horizons and their surface features. B) Photograph showing three thin beds that make up this surface. Note pustular microbial structures ( = arrowed ms). U = upper bed
Image
Figure 1 —Geological context of the Elk Mound Group and St. Lawrence Forma...
in THREE-DIMENSIONALLY PRESERVED ARTHROPODS FROM CAMBRIAN LAGERSTÄTTEN OF QUEBEC AND WISCONSIN
> Journal of Paleontology
Published: 01 July 2010
Figure 1 —Geological context of the Elk Mound Group and St. Lawrence Formation of Wisconsin and the Potsdam Group of New York, Quebec, and Ontario. 1 , Laurentia in the late Cambrian (Furongian) with the locations of field sites starred along the shoreline; 2 , outcrop map of the Potsdam Group
Image
Figure 4 — Arenosicaris inflata n. gen. n. sp. from the Elk Mound Group (...
in THREE-DIMENSIONALLY PRESERVED ARTHROPODS FROM CAMBRIAN LAGERSTÄTTEN OF QUEBEC AND WISCONSIN
> Journal of Paleontology
Published: 01 July 2010
Figure 4 — Arenosicaris inflata n. gen. n. sp. from the Elk Mound Group (4.1–4.5, 4.7) and St. Lawrence Formation (4.6). 1 , PRI 10130 (holotype), a nearly complete phyllocarid, note prominent limb bases (arrowheads); 2 , PRI 10131a–c, three phyllocarids (a at top, c at bottom); two partial
Image
Figure 7 — Mosinieia macnaughtoni n. gen. n. sp. from the Elk Mound Group...
in THREE-DIMENSIONALLY PRESERVED ARTHROPODS FROM CAMBRIAN LAGERSTÄTTEN OF QUEBEC AND WISCONSIN
> Journal of Paleontology
Published: 01 July 2010
Figure 7 — Mosinieia macnaughtoni n. gen. n. sp. from the Elk Mound Group, and Mictomerus melochevillensis n. fam. n. gen. n. sp. from the Potsdam Group. 1 , PRI 10144 (holotype) Mosinieia macnaughtoni n. sp. and 2 , camera lucida drawing. Note that the preservation of the abdominal region
Journal Article
THREE-DIMENSIONALLY PRESERVED ARTHROPODS FROM CAMBRIAN LAGERSTÄTTEN OF QUEBEC AND WISCONSIN
Journal: Journal of Paleontology
Publisher: Paleontological Society
Published: 01 July 2010
Journal of Paleontology (2010) 84 (4): 646–667.
...Figure 1 —Geological context of the Elk Mound Group and St. Lawrence Formation of Wisconsin and the Potsdam Group of New York, Quebec, and Ontario. 1 , Laurentia in the late Cambrian (Furongian) with the locations of field sites starred along the shoreline; 2 , outcrop map of the Potsdam Group...
Journal Article
DEAD IN THEIR TRACKS—CAMBRIAN ARTHROPODS AND THEIR TRACES FROM INTERTIDAL SANDSTONES OF QUEBEC AND WISCONSIN
Journal: PALAIOS
Publisher: SEPM Society for Sedimentary Geology
Published: 01 August 2010
PALAIOS (2010) 25 (8): 475–486.
...Figure 1. Elk Mound Group channel deposits where traces and body fossils of their producers co-occur. A) Large channel cutting through an Elk Mound Group tidal flat. Rock hammer (arrowed) is 28 cm long. B) Part of a large phyllocarid-bearing slab from the horizon that infills the surface visible...
Journal Article
Protichnites eremita Unshelled? Experimental Model-Based Neoichnology and New Evidence for A Euthycarcinoid Affinity for This Ichnospecies
Journal: Journal of Paleontology
Publisher: Paleontological Society
Published: 01 May 2012
Journal of Paleontology (2012) 86 (3): 442–454.
...F igure 1 Protichnites eremita Form 2, Trackways A and B, Elk Mound Group, Blackberry Hill, Wisconsin, PRI Station 3421. 1 , PRI 10143, both trackways shown, Trackway B exhibits a sharp right turn whereas Trackway A exhibits a gentle turn; segmentation present in the intermittent medial...
Journal Article
Hermit arthropods 500 million years ago?
Journal: Geology
Publisher: Geological Society of America
Published: 01 April 2009
Geology (2009) 37 (4): 295–298.
..., trace fossils from the Late Cambrian Elk Mound Group of Wisconsin illustrate how some arthropods might have managed to withstand the vicissitudes of subaerial exposure—by using foreign shells like hermit crabs. This behavior is suggested by trackways (Protichnites eremita isp. nov.), which have “tail...
Journal Article
STRANDED IN UPSTATE NEW YORK: CAMBRIAN SCYPHOMEDUSAE FROM THE POTSDAM SANDSTONE
Journal: PALAIOS
Publisher: SEPM Society for Sedimentary Geology
Published: 01 July 2008
PALAIOS (2008) 23 (7): 424–441.
... and morphologically to coeval scyphomedusae from the Elk Mound Group of Wisconsin and were likely stranded on a sand flat. Soft-tissue preservation in such sandstones is rare, except in Ediacaran Konservat-Lagerstätten. Although subtidal facies are abundant and continental facies are present in the Potsdam, soft...
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Figure 11 —Composite reconstructions of the arthropods presented in this s...
in THREE-DIMENSIONALLY PRESERVED ARTHROPODS FROM CAMBRIAN LAGERSTÄTTEN OF QUEBEC AND WISCONSIN
> Journal of Paleontology
Published: 01 July 2010
Figure 11 —Composite reconstructions of the arthropods presented in this study. 1 , Arenosicaris inflata n. sp. from the Elk Mound Group and Lodi Member, St. Lawrence Formation of Wisconsin. Reconstruction based on 47 specimens; 2 , Mosinieia macnaughtoni n. sp. from the Elk Mound Group
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FIGURE 8 —Histogram of size distribution (A) and preservational quality (B)...
Published: 01 July 2008
FIGURE 8 —Histogram of size distribution (A) and preservational quality (B) of a subset of medusae from the Potsdam and Elk Mound Groups. The Elk Mound data subset was randomly selected among the thousands of medusae measured as part of another study ( Hagadorn et al., 2003 ), and the Potsdam
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Figure 4. Top surface expression of the intrastratal burrow, Climactichnit...
Published: 01 September 2010
Figure 4. Top surface expression of the intrastratal burrow, Climactichnites youngi . A) Rippled sandstone of the Elk Mound Group (PRI 8980), with a scyphomedusae impression (arrowhead) resting on top of the ripples. B) Closeup of this surface dotted with sand stromatolites (one of them
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Figure 6 — Arenosicaris inflata n. gen. n. sp. carapaces from the Elk Mou...
in THREE-DIMENSIONALLY PRESERVED ARTHROPODS FROM CAMBRIAN LAGERSTÄTTEN OF QUEBEC AND WISCONSIN
> Journal of Paleontology
Published: 01 July 2010
Figure 6 — Arenosicaris inflata n. gen. n. sp. carapaces from the Elk Mound Group. 1 , carapace internal mold, field specimen and 2 , (lucida). These specimens show the internal surface morphology of the carapace valves. Note the anterodorsal depression present in both examples, which may
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Figure 3. Infaunal molluscan burrows. A) Sole of sandy flagstone from the e...
Published: 01 September 2010
as the producer of a meandering Psammichnites saltensis wedged its way at a lower level, backfilling the burrow with sand from the surface. From Seilacher et al. (2005 , fig. 22); coin in lower left is 1.7 cm wide. B) Sole face of a split part-counterpart sandstone slab from the middle-late Cambrian Elk Mound
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Protichnites : ( 1–6 ) Owen's ( 1852 ) drawings of the holotypes of the ori...
Published: 01 January 2023
(from Owen, 1852 , pl. 14); ( 7–10 ) a variety of forms commonly assigned to Protichnites , Cambrian, Elk Mound Group, Blackberry Hill, central Wisconsin, 44.7075°N, 89.5071°W: ( 7 ) Protichnites eremita Hagadorn and Seilacher, 2009 , YPM IP 204961, photographed by S. Butts; ( 8 ) WM/P 982
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