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GeoRef Subject
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Ocala Group (1)
-
Oligocene
-
lower Oligocene
-
Rupelian (2)
-
-
Suwannee Limestone (1)
-
upper Oligocene (1)
-
-
Paleocene
-
lower Paleocene
-
Danian (1)
-
K-T boundary (3)
-
-
-
Wilcox Group (1)
-
-
Pysht Formation (1)
-
-
upper Cenozoic
-
Tamiami Formation (1)
-
-
-
Laurentide ice sheet (2)
-
Mesozoic
-
Cretaceous
-
Comanchean
-
Edwards Formation (1)
-
-
Lower Cretaceous
-
Albian
-
upper Albian (1)
-
-
Aptian
-
lower Aptian (1)
-
-
Barremian (2)
-
Berriasian (1)
-
Cupido Formation (1)
-
Edwards Formation (1)
-
Hauterivian (3)
-
Mural Limestone (3)
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Valanginian (1)
-
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Middle Cretaceous (1)
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Upper Cretaceous
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Campanian (1)
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Cenomanian (4)
-
K-T boundary (3)
-
Maestrichtian
-
lower Maestrichtian (1)
-
-
Ripley Formation (1)
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Santonian (2)
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Senonian (7)
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Smoky Hill Chalk Member (1)
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Turonian (1)
-
-
-
Jurassic
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Lower Jurassic
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Hettangian (1)
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lower Liassic (2)
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Pliensbachian (2)
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Sinemurian (2)
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Toarcian (2)
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upper Liassic (1)
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Middle Jurassic
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Bajocian (1)
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Bathonian (3)
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Callovian (3)
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Dogger (2)
-
-
Upper Jurassic
-
Hanifa Formation (1)
-
Kimmeridgian (2)
-
Oxfordian
-
middle Oxfordian (1)
-
-
Portlandian (2)
-
Smackover Formation (2)
-
Tithonian (2)
-
-
-
lower Mesozoic (1)
-
Triassic
-
Lower Triassic
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Griesbachian (1)
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Induan (1)
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Olenekian (1)
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Permian-Triassic boundary (4)
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Middle Triassic
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Anisian (1)
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Ladinian (1)
-
-
Montney Formation (1)
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Takla Group (1)
-
Upper Triassic
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Baldonnel Formation (1)
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Carnian (5)
-
Luning Formation (2)
-
Norian (10)
-
Rhaetian (1)
-
-
-
-
MIS 11 (1)
-
MIS 5 (1)
-
MIS 7 (2)
-
Moldanubian (1)
-
Paleozoic
-
Bird Spring Formation (3)
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Cambrian
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Lower Cambrian
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Atdabanian (1)
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Poleta Formation (1)
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Terreneuvian
-
Fortunian (1)
-
-
Zabriskie Quartzite (1)
-
-
Middle Cambrian
-
Burgess Shale (1)
-
Marjum Formation (1)
-
Wheeler Formation (3)
-
-
Upper Cambrian
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Mount Simon Sandstone (1)
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Potsdam Sandstone (2)
-
Wonewoc Formation (2)
-
-
-
Carboniferous
-
Avonian (1)
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Ely Limestone (1)
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Hale Formation (2)
-
Lower Carboniferous
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Asbian (2)
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Dinantian (11)
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-
Middle Carboniferous (2)
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Mississippian
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Borden Group (2)
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Chainman Shale (1)
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Charles Formation (1)
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Leadville Formation (1)
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Lower Mississippian
-
Fort Payne Formation (1)
-
Kinderhookian
-
Banff Formation (1)
-
-
Lodgepole Formation (3)
-
Osagian (2)
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Tournaisian (4)
-
-
Madison Group (2)
-
Middle Mississippian
-
Visean
-
Great Scar Limestone (1)
-
-
-
Mission Canyon Limestone (2)
-
Upper Mississippian
-
Chesterian
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Imo Formation (2)
-
-
Fayetteville Formation (2)
-
Hartselle Sandstone (1)
-
Meramecian
-
Saint Louis Limestone (1)
-
Sainte Genevieve Limestone (2)
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Salem Limestone (1)
-
-
Pitkin Limestone (2)
-
Serpukhovian (2)
-
-
Valmeyeran (1)
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Windsor Group (1)
-
-
Namurian (1)
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Pennsylvanian
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Hermosa Group (1)
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Lower Pennsylvanian
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Morrowan (4)
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Middle Pennsylvanian
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Atokan (2)
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Breathitt Formation (1)
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Desmoinesian (4)
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Kanawha Formation (1)
-
-
Upper Pennsylvanian
-
Gzhelian (2)
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Holder Formation (1)
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Missourian (1)
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Virgilian (2)
-
-
-
Upper Carboniferous
-
Westphalian (1)
-
-
-
Devonian
-
Beaverhill Lake Group (2)
-
Cedar City Formation (1)
-
Guilmette Formation (1)
-
Lower Devonian
-
Coeymans Formation (4)
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Emsian (15)
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Gedinnian (1)
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Helderbergian (1)
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Lochkovian (7)
-
Manlius Formation (3)
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Pragian (4)
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Siegenian (2)
-
York River Formation (1)
-
-
Middle Devonian
-
Cedar Valley Formation (2)
-
Columbus Limestone (3)
-
Detroit River Group (6)
-
Eifelian (13)
-
Givetian
-
Horn Plateau Formation (1)
-
-
Hamilton Group (10)
-
Ludlowville Formation (2)
-
Moscow Formation (5)
-
Onondaga Limestone (5)
-
Tully Limestone (1)
-
Winnipegosis Formation (1)
-
-
Ramparts Formation (2)
-
Swan Hills Formation (4)
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Traverse Group (3)
-
Upper Devonian
-
Duperow Formation (1)
-
Famennian
-
lower Famennian (1)
-
Wabamun Group (2)
-
-
Frasnian
-
upper Frasnian (1)
-
-
Grosmont Formation (1)
-
Nisku Formation (4)
-
Palliser Formation (1)
-
Strunian (1)
-
-
Waterways Formation (2)
-
Zlichovian (1)
-
-
Ellis Bay Formation (5)
-
Exshaw Formation (2)
-
Helderberg Group (2)
-
Keyser Limestone (2)
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lower Paleozoic (4)
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middle Paleozoic (1)
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Oquirrh Formation (1)
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Ordovician
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El Paso Group (1)
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Tremadocian (1)
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Middle Ordovician
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Black River Group (3)
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Chazy Group (1)
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Darriwilian (3)
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Decorah Shale (1)
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Llandeilian (1)
-
-
Montoya Group (2)
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Trenton Group (3)
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Upper Ordovician
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Ashgillian (10)
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Caradocian (3)
-
Cincinnatian
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Maysvillian (4)
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Richmondian (4)
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Edenian (1)
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Fairview Formation (1)
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Hirnantian (4)
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Katian (3)
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Kope Formation (1)
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Maquoketa Formation (2)
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Mohawkian (2)
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Red River Formation (11)
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Sandbian (4)
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Trentonian (4)
-
-
-
Permian
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Guadalupian
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Capitanian (1)
-
Cherry Canyon Formation (1)
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Roadian (1)
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Wordian (1)
-
-
Khuff Formation (1)
-
Lower Permian
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Cherry Canyon Formation (1)
-
Cisuralian
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Artinskian (5)
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Asselian (2)
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Kungurian (2)
-
Sakmarian (2)
-
-
Leonardian (3)
-
Qixia Formation (1)
-
Wolfcampian (4)
-
-
Maokou Formation (1)
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McCloud Limestone (1)
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Middle Permian (2)
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Upper Permian
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Lopingian
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Changhsingian (2)
-
Wuchiapingian (1)
-
-
Permian-Triassic boundary (4)
-
-
-
Read Bay Formation (1)
-
Road River Formation (2)
-
Rondout Formation (1)
-
Shoo Fly Complex (2)
-
Silurian
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Lockport Formation (2)
-
Lower Silurian
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Brassfield Formation (2)
-
Llandovery
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Aeronian (2)
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Interlake Formation (1)
-
Rhuddanian (3)
-
Telychian (4)
-
-
Wenlock
-
Homerian (1)
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Sheinwoodian (4)
-
-
Whirlpool Sandstone (1)
-
-
Middle Silurian
-
Clinton Group (1)
-
Keefer Sandstone (1)
-
Racine Dolomite (1)
-
Rochester Formation (1)
-
Waldron Shale (5)
-
-
Niagaran (6)
-
Upper Silurian
-
Ludlow
-
Ludfordian (2)
-
-
Pridoli (8)
-
Salina Group (1)
-
-
-
upper Paleozoic
-
Copacabana Group (1)
-
-
-
Phanerozoic (16)
-
Precambrian
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Archean
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Neoarchean (1)
-
-
upper Precambrian
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Proterozoic
-
Neoproterozoic
-
Doushantuo Formation (1)
-
Ediacaran (17)
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Infracambrian (1)
-
Vendian (9)
-
-
Paleoproterozoic (1)
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Sinian
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Doushantuo Formation (1)
-
-
-
-
-
-
igneous rocks
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igneous rocks
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kimberlite (1)
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ophiolite (4)
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metamorphic rocks
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metasedimentary rocks (1)
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-
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ophiolite (4)
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minerals
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carbonates
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halides
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halite (2)
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-
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minerals (2)
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native elements
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oxides
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phosphates
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sodalite group
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-
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orthosilicates
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zircon group
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sheet silicates
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clay minerals
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smectite (1)
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illite (1)
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mica group
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sulfates
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troilite (1)
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Primary terms
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absolute age (64)
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Africa
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Tertiary
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Deep Sea Drilling Project
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Leg 12
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Integrated Ocean Drilling Program
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Expedition 307
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IODP Site U1316 (1)
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Tahiti Sea Level Expedition
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intrusions (4)
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Invertebrata
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Brachiopoda
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Inarticulata
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Heliolitida
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Echinodermata
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Mollusca
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Ostreoidea
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Pterioida
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Cephalopoda
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-
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Nautiloidea (4)
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Gastropoda
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Hyolithes (1)
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Tentaculitida
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Porifera
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Calcarea
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Demospongea
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Stromatoporoidea
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Amphipora (4)
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Protista
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Miliolina
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Rotaliina
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Nodosariacea (1)
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Miogypsinidae
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Nummulitidae
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Operculina (1)
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-
-
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Radiolaria (11)
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Tintinnidae
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Vermes
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isostasy (3)
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isotopes
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radioactive isotopes
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-
stable isotopes
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C-13/C-12 (33)
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Mg-26/Mg-24 (2)
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O-18/O-16 (40)
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S-34/S-32 (3)
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Sr-87/Sr-86 (9)
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lava (2)
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magmas (1)
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Malay Archipelago
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Timor
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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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upper Albian (1)
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lower Aptian (1)
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Barremian (2)
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Jurassic
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upper Liassic (1)
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Upper Jurassic
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middle Oxfordian (1)
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Portlandian (2)
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Tithonian (2)
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lower Mesozoic (1)
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Carnian (5)
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Rhaetian (1)
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metal ores
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metals
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magnesium
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Sr-87/Sr-86 (9)
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iron (1)
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manganese (3)
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nickel (1)
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platinum group
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rare earths
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neodymium
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zinc (2)
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metamorphic rocks
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museums (2)
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nodules (1)
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North America
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ocean circulation (5)
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Ocean Drilling Program
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Leg 167
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ODP Site 1012 (1)
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ODP Site 1017 (1)
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ODP Site 1018 (1)
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ODP Site 1019 (1)
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ODP Site 1020 (1)
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Leg 210
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ODP Site 1276 (1)
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ODP Site 1277 (1)
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ocean floors (7)
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ocean waves (2)
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Oceania
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Marshall Islands
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Polynesia
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Tahiti (4)
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Tuamotu Islands (1)
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Hawaii
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Kohala (1)
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Kona (1)
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Mauna Kea (1)
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Cnidaria
MEDITERRANEAN IMPRINT ON CORAL DIVERSITY IN THE INCIPIENT RED SEA (BURDIGALIAN, SAUDI ARABIA)
Corallite sizes of reef corals: decoupling of evolutionary and ecological trends
New insights on the latest Messinian-to-Piacenzian stratigraphic series from the Dahra Massif (Lower Chelif Basin, Algeria): Lago Mare, reflooding and bio-events
Type material of Paraconularia planicostata (Dawson) from the Upper Mississippian of Nova Scotia, Atlantic Canada
Late Cambrian Pywackia is a cnidarian, not a bryozoan: Insights from skeletal microstructure
A hydrozoan from the eurypterid-dominated Silurian Bertie Group Lagerstätten of North America
Conulariid soft parts replicated in silica from the Scotch Grove Formation (lower Middle Silurian) of east-central Iowa
Reconstructing past disturbance in coral communities using U-Th dating of dead coral skeletons
Behavioural and Environmental Significance of the Rosetted trace Fossil Dactyloidites ottoi (Geinitz, 1849) from the Early Cretaceous (Berriasian) of Kachchh, Western India
Corals and a cephalopod from the Whirlpool Formation (latest Ordovician, Hirnantian), Hamilton, Ontario: biostratigraphic and biogeographic significance
Three common sampling techniques in Pleistocene coral reefs of the Red Sea: a comparison
Abstract Line Intercept Transects (LIT), Point Intercept Transects (PIT) and Photoquadrats (PQ) are the most common quantitative sampling techniques in modern and fossil coral reefs. Data from coral reefs obtained by the different methods are generally compared between various reef ages and localities. Quaternary reefs from warmer interglacial periods, which represent climate scenarios projected for the future, are particularly interesting for comparisons with modern reefs. Importantly, fossil reefs differ from modern reefs because they are diagenetically altered and time-averaged. While several studies have compared different quantitative methods in modern reefs, very few have dealt with the comparability among fossil and between fossil and modern reefs. Here, we compare LIT, PIT at 10, 20 and 50 cm intervals and PQ in two Pleistocene reef localities in Egypt. We find that alpha diversity, reef cover and community composition are dependent on the method. Results gained with plotless methods (LIT, PIT) differ strongly from results gained with plot methods (PQ). However, coral cover results are similar with LIT and PIT, and community composition is indistinguishable between the two, but alpha diversity depends on the interval used for PIT. We discuss the implications of our findings for comparing coral reefs of various ages and localities. We recommend surveying Pleistocene reefs with PIT at 20 cm intervals. This is because (1) alpha diversity is well captured, (2) the amount of time-averaging recorded by PIT is reduced compared to PQ, (3) the PIT results can be directly compared to reefs analysed by LIT and (4) the method is less time-consuming than LIT and PQ.