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NARROW
Format
Article Type
Journal
Publisher
Section
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Africa
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East Africa
-
Kenya (1)
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Tanzania (1)
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East African Lakes
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Lake Kariba (1)
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Madagascar
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Mahajanga Basin (1)
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Namib Desert (1)
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North Africa
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Algeria
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Bechar Algeria
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Ougarta Algeria (1)
-
-
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Atlas Mountains
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Moroccan Atlas Mountains
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High Atlas (1)
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-
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Libya
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Murzuk Basin (2)
-
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Morocco
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Moroccan Atlas Mountains
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High Atlas (1)
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Rif (1)
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-
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Nubian Shield (1)
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Sahara (1)
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Southern Africa
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Karoo Basin (5)
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Lesotho (1)
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Namibia (3)
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South Africa
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Eastern Cape Province South Africa (3)
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Free State South Africa (1)
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Limpopo South Africa (1)
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Mpumalanga South Africa (1)
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Western Cape Province South Africa (1)
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Zimbabwe (2)
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West Africa
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Chad (1)
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Mauritania (1)
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-
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Antarctica
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Antarctic Peninsula (1)
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East Antarctica (2)
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James Ross Island (1)
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Transantarctic Mountains
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Beardmore Glacier (1)
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Victoria Land
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Allan Hills (1)
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-
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Arctic region
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Greenland
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East Greenland (3)
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Jameson Land (2)
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Northern Greenland (1)
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Scoresby Land (2)
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West Greenland (1)
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Russian Arctic (1)
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Arran (2)
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Asia
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Altai Mountains
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Arabian Peninsula
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Far East
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China
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Japan
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Korea (1)
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Indian Peninsula
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India
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Northeastern India
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Uttar Pradesh India (3)
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Kopet-Dag Range (1)
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Middle East
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Israel
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Jordan (2)
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Yakutia Russian Federation
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Atlantic Ocean
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South Atlantic
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Australasia
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Australia
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New South Wales Australia (4)
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Nullarbor Plain (1)
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South Australia
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Gawler Craton (1)
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Kangaroo Island (1)
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Western Australia (1)
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New Zealand (4)
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Bell Island (1)
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Black Mesa (1)
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Canada
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Arctic Archipelago (4)
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Eastern Canada
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Maritime Provinces
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Nova Scotia
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Meguma Terrane (1)
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Newfoundland and Labrador
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Labrador (2)
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Ontario
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Quebec
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Mackenzie Mountains (6)
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Nunavut
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Queen Elizabeth Islands
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Western Canada
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British Columbia
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Caribbean region
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West Indies
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Antilles
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Commonwealth of Independent States
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Russian Federation
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Siberian Platform (3)
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Yakutia Russian Federation
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Ukraine (1)
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Cornwallis Island (2)
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Death Valley (3)
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Europe
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Adriatic region (1)
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Alps
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Eastern Alps
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French Alps (1)
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Baltic region
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Estonia (1)
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Carpathians
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Polish Carpathians (3)
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Western Carpathians (1)
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Central Europe
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Czech Republic
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Germany
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Hesse Germany
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Poland
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Polish Carpathians (3)
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Swiety Krzyz Mountains (2)
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Jutland (1)
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Pieniny Klippen Belt (2)
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Pyrenees
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Southern Europe
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Croatia (2)
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Dobruja Basin
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Iberian Peninsula
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Portugal
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Spain
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Andalusia Spain
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Balearic Islands
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Basque Provinces Spain (3)
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Catalonia Spain
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Lleida Spain
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Guadalquivir Basin (2)
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Spanish Pyrenees (1)
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Subbetic Zone (1)
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Valencia region
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Alicante Spain
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Alcoy Spain (1)
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Istria (1)
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Italy
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Apennines
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Northern Apennines (3)
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Basilicata Italy (1)
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Emilia-Romagna Italy
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Friuli-Venezia Giulia Italy
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Trieste Italy (1)
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Lombardy Italy
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Como (1)
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Piemonte Italy
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Umbria Italy (2)
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Malta (1)
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Romania
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Ukraine (1)
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Western Europe
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Belgium (1)
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France
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Armorican Massif (1)
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French Alps (1)
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Gard France
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Herault France
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Normandy (3)
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Ireland
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Clare Ireland (1)
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Donegal Ireland (2)
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Wexford Ireland (1)
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Netherlands (1)
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Scandinavia
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Denmark (4)
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Norway
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Finnmark Norway (1)
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Sweden
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Skane Sweden
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United Kingdom
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English Channel Islands
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Jersey (1)
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Great Britain
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England
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Cheshire England (1)
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East Anglia
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East Midlands (1)
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Isle of Wight England (1)
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Oxfordshire England (2)
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Sussex England (1)
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Yorkshire England
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Scotland
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Ayrshire Scotland (1)
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Glasgow Scotland (1)
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Highland region Scotland (1)
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Midlothian Scotland (1)
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Wales
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Cardiganshire Wales
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Isle of Man (1)
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Fraser River (1)
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Grand Banks (1)
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Green River basin (1)
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Guadalupe Mountains (1)
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Hartford Basin (1)
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Indian Ocean
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Arabian Sea
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Indian Ocean Islands
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Madagascar
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Mediterranean region
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Mediterranean Sea
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Mexico
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Pacific Ocean
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Pacific region
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Florida
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Tompkins County New York
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Yates County New York (1)
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Newark Basin (1)
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Eocene
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middle Eocene
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upper Eocene
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Oligocene
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Brule Formation (3)
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Paleocene
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Clayton Formation (2)
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Danian (3)
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Porters Creek Formation (1)
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upper Tertiary (1)
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Mesozoic
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Lower Cretaceous
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Albian
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Middle Cretaceous (2)
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Natih Formation (1)
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Upper Cretaceous
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Almond Formation (1)
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Belle Fourche Shale (1)
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Campanian
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Cardium Formation (1)
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Two Medicine Formation (1)
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Franciscan Complex (2)
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Jurassic
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Maiolica Limestone (1)
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Triassic
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Upper Triassic
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Baldonnel Formation (1)
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Sag River Sandstone (1)
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upper Mesozoic (1)
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Paleozoic
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Cambrian
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Lower Cambrian
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Antietam Formation (1)
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Terreneuvian
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-
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Middle Cambrian
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Burgess Shale (2)
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Upper Cambrian
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Eau Claire Formation (1)
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Carboniferous
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Price Formation (2)
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Upper Mississippian
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Meramecian
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Saint Louis Limestone (1)
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Serpukhovian (1)
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Pennsylvanian
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Conemaugh Group (2)
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Lower Pennsylvanian
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Crab Orchard Mountains Group (1)
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Mansfield Formation (1)
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Middle Pennsylvanian
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Carbondale Formation (1)
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Kanawha Formation (2)
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Monongahela Group (3)
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Upper Pennsylvanian
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Glenshaw Formation (1)
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Missourian (1)
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Virgilian
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Shawnee Group (2)
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-
-
-
Upper Carboniferous (3)
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Catskill Formation (1)
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Devonian
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Genesee Group (2)
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Hunsruck Shale (1)
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Lower Devonian
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Middle Devonian
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Marcellus Shale (1)
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Moscow Formation (2)
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Onondaga Limestone (1)
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Winnipegosis Formation (1)
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-
Muth Quartzite (2)
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Old Red Sandstone (2)
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Upper Devonian
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Birdbear Formation (1)
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Chemung Formation (1)
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Duperow Formation (1)
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Famennian
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lower Famennian (1)
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upper Famennian (1)
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Wabamun Group (2)
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Frasnian
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upper Frasnian (1)
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Kellwasser event (1)
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Palliser Formation (2)
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West Falls Formation (1)
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-
Upper Old Red Sandstone (1)
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-
Dunkard Group (3)
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Hanson Creek Formation (1)
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lower Paleozoic
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Cape Phillips Formation (1)
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-
Ordovician
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Ely Springs Dolomite (1)
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Eureka Quartzite (1)
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Lower Ordovician
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Manitou Formation (1)
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Oneota Dolomite (1)
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Tremadocian (2)
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Meguma Group (2)
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Middle Ordovician
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Black River Group (2)
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Champlainian (1)
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Galena Dolomite (1)
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Platteville Formation (1)
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Winnipeg Formation (1)
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-
Trenton Group (2)
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Upper Ordovician
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Bighorn Dolomite (1)
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Cincinnatian
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Maysvillian (1)
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-
Fairview Formation (1)
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Fish Haven Dolomite (1)
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Hirnantian (1)
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Juniata Formation (3)
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Katian (1)
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Red River Formation (1)
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Trentonian (4)
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Yeoman Formation (2)
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-
-
Permian
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Coconino Sandstone (1)
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Guadalupian
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Roadian (1)
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Seven Rivers Formation (1)
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Tansill Formation (1)
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-
Lower Permian
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Abo Formation (2)
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Barakar Stage (1)
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Qixia Formation (1)
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Wolfcampian
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Albian
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Campanian
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Cardium Formation (1)
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Gulfian
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Turonian
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Two Medicine Formation (1)
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Viking Formation (1)
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Franciscan Complex (2)
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Jurassic
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Upper Jurassic
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Arab Formation (2)
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Smackover Formation (1)
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Maiolica Limestone (1)
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Triassic
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Lower Triassic
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Permian-Triassic boundary (4)
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Middle Triassic
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Doig Formation (4)
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Upper Triassic
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Paleozoic
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Upper Carboniferous (3)
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Catskill Formation (1)
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Upper Old Red Sandstone (1)
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lower Paleozoic
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Ordovician
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Upper Ordovician
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Fairview Formation (1)
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Permian
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Lower Permian
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Abo Formation (2)
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Maokou Formation (1)
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Upper Permian
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Permian-Triassic boundary (4)
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Rio do Rasto Formation (1)
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Vryheid Formation (1)
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Silurian
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Lower Silurian
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Grimsby Sandstone (1)
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Llandovery
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Bloomsburg Formation (1)
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upper Paleozoic
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Woodford Shale (1)
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Plantae
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Spermatophyta
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Gymnospermae
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Coniferales (1)
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plate tectonics (3)
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Precambrian
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Wyman Formation (2)
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
burrows
Paleoenvironmental conditions and evolution of a muddy turbidite system: an integrated sedimentological and ichnological analysis Available to Purchase
CRAB TRACES ON MUDDY TIDAL FLATS OF THE MIRA RIVER ESTUARY, PORTUGAL Available to Purchase
Exceptionally preserved burrows of ichnogenus Asterosoma from the lower Silurian of south China: systematic ichnology, palaeoecology and implications for ecosystem recovery following the late Ordovician mass extinction Available to Purchase
EVALUATING TRACE FOSSILS, FLUVIAL ARCHITECTURE, AND COLONIZATION PATTERNS IN CHANNEL AND OVERBANK DEPOSITS FROM THE MIOCENE VINCHINA FORMATION, WESTERN ARGENTINA Available to Purchase
NEOICHNOLOGY OF A MICROTIDAL CARBONATE INTERTIDAL ZONE: ABU DHABI, U.A.E. Available to Purchase
Chickies Rock, a striking promontory on the Susquehanna River: the early Cambrian type locality of the trace fossil Skolithos and a model site for structural analysis Open Access
Abstract Chickies Rock rises abruptly from the east bank of the Susquehanna River at Columbia, Pennsylvania, where it breaks through a ridge held up by massively bedded quartzite. Here in the 1830s, Samuel Haldeman recognized long straight tubes that he later described as Skolithos linearis , penetrating the quartzite. Uncertain about the nature of these cylindrical ‘vermiform or linear’, unbranched ‘stems’, Haldeman first treated them as a subgenus of Fucoides , to which root-like traces were then often assigned. By the time James Hall first illustrated the species in 1847, Haldeman was sure they were burrows of a worm-like animal, as the name he had chosen implied. Since 1960, Donald Wise has developed a detailed analysis of structural deformation of the Chickies Anticline, using the Skolithos burrows as ‘plumb-bobs’ against which Taconic rotation of the rock fabric can be measured. Wise showed that later Alleghanian deformation produced prominent folds with external rotation up to twice as great as that of the rock fabric itself. Now conserved as a county park, Chickies Rock attracts many visitors. Its cliff-top is a superb viewpoint from which to contemplate progressive westward migration of the Appalachian drainage divide, ongoing since the late Jurassic opening of the Atlantic Ocean.
Selected Karoo geoheritage sites of palaeontological significance in South Africa and Lesotho Open Access
Abstract The main Karoo Basin of South Africa and Lesotho preserves c. 120 myr of Earth's history. The sedimentary rocks of its Karoo Supergroup record massive environmental changes from the glacial Carboniferous to desert dunes and fiery flood basalts in the Early Jurassic. From the early Permian, the Karoo Basin was gradually filled with fluvial and lacustrine deposits, and the alluvial plains were successively colonized by a diverse suite of plants and animals. The fossils of these ancient inhabitants and their behavioural traces form an astounding Gondwanan geoheritage legacy in southern Africa, providing fossil evidence for the moving lithospheric plates and the effects of four mass extinctions and their subsequent biotic recovery. Here, we present six Karoo sites of global geoscientific importance that best display that heritage, with the caveat that these sites only touch upon the Karoo riches that are available for academic research and the emerging palaeotourism industry. It is our hope that these sites will become anchor points for a sustainable geoheritage future in southern Africa.
MEIOFAUNAL BIOTURBATION OF LATE PLEISTOCENE–HOLOCENE GLACIOMARINE MUD IN THE CHAMPLAIN SEA BASIN, EASTERN CANADA: ORIGIN OF BURROWS, THEIR GEOCHEMICAL IMPLICATIONS, AND PALEOENVIRONMENTAL CONTROLS Open Access
NEOICHNOLOGY OF TROPICAL AND ARID SCORPIONS: ENVIRONMENTAL IMPACTS ON BURROW CONSTRUCTION AND FORM Available to Purchase
NEOICHNOLOGICAL ANALYSIS OF MOLE CRICKET BURROWS: IMPLICATIONS OF SUBSTRATE MOISTURE CHANGES ON PRESERVATION AND MORPHOLOGY Available to Purchase
HYBRID NATURE OF A NEW JURASSIC–CRETACEOUS WORM BURROW INDICATED BY MICROBIAL MEDIATION OF ITS WALL FORMATION Available to Purchase
Arthropleura trackway ( Diplichnites cuithensis ) from the Carboniferous, Serpukhovian, Limestone Coal Formation, Clackmannan Group, Linn Park, Glasgow Open Access
HELMINTHOPSIS AND CYLINDRICHNUS ICHNOGUILDS FROM MIOCENE THIN-BEDDED TURBIDITES, TIERRA DEL FUEGO, ARGENTINA Available to Purchase
Preservation of Soft-Bodied Organisms in Early Cambrian Carbonates Available to Purchase
The possible actiniarian sea anemone burrow Bergaueria hemispherica from the Pliensbachian (Lower Jurassic) of the Lusitanian Basin (Central Portugal) Available to Purchase
Abstract The shallow marine carbonate deposits of the S. Miguel Formation in the Lusitanian Basin reveal erosional events exposing stiff substrates with abundant Bergaueria hemispherica . The ichnoassociation represented by B. hemispherica , Thalassinoides suevicus , Spongeliomorpha isp., Asterosoma ludwigae and Rhizocorallium commune is dated from lowermost Pliensbachian by the association with ammonites from the jamesoni Biozone, brevispina Subzone. The unlined forms of B. hemispherica include peripheral and bottom burrow concentrations of shell debris, annular-like structures in the burrow margin and paired burrows-to-linear clusters that are comparable with the penetrative burrowing mechanism, anchoring and feeding behaviours of sea anemones. From the ethological point of view, and comparing with modern behaviours of burrowing anemones, the B. hemispherica from the Lusitanian Basin may represent temporary burrowing and relocation of actiniarian anemones. Their comparison with either thenarian or athenarian actiniarians may evidence a preferred surficial feeding strategy on the organic-rich muddy sediments they burrowed.