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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Africa
-
Central Africa
-
Angola (1)
-
-
East Africa
-
Kenya
-
Lake Magadi (2)
-
-
Lake Natron (2)
-
Lake Turkana (2)
-
-
East African Lakes
-
Lake Magadi (2)
-
Lake Natron (2)
-
Lake Tanganyika (2)
-
Lake Turkana (2)
-
-
North Africa
-
Atlas Mountains
-
Moroccan Atlas Mountains
-
High Atlas (1)
-
-
-
Morocco
-
Moroccan Atlas Mountains
-
High Atlas (1)
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-
-
Southern Africa
-
Namibia (4)
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South Africa
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Northern Cape Province South Africa (1)
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-
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West Africa
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Taoudenni Basin (1)
-
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Arctic region (1)
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Asia
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Arabian Peninsula
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Oman (2)
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Saudi Arabia (1)
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United Arab Emirates
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Abu Dhabi (1)
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Far East
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China
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Guangxi China (1)
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Guizhou China (3)
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Nanpanjiang Basin (5)
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Shandong China (2)
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Indonesia
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Japan
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Kyushu (1)
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Middle East
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Atlantic Ocean
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South Atlantic
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Australasia
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Death Valley (1)
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Europe
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Oceania
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U. S. Rocky Mountains
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Western U.S. (1)
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commodities
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brines (1)
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oil and gas fields (7)
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petroleum
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elements, isotopes
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carbon
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C-13 (1)
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C-13/C-12 (23)
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C-14 (2)
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chemical ratios (1)
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isotope ratios (25)
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isotopes
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radioactive isotopes
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C-14 (2)
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stable isotopes
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C-13/C-12 (23)
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Fe-54 (1)
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Fe-56 (1)
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N-15/N-14 (2)
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metals
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alkaline earth metals
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magnesium
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Mg/Ca (1)
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strontium
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iron
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molybdenum (1)
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rare earths
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nitrogen
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N-15/N-14 (2)
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oxygen
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O-18/O-16 (15)
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phosphorus (1)
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sulfur
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S-34/S-32 (2)
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fossils
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Chordata
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Cloudina (1)
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Skolithos (1)
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Invertebrata
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Brachiopoda (3)
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Echinodermata
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Crinozoa
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Mollusca
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Cephalopoda
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Porifera
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Demospongea (2)
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Protista
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Foraminifera
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Fusulinina (1)
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Miliolina
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Vermes
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Annelida (1)
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Polychaeta
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Serpulidae (1)
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Metazoa (7)
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microfossils
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Conodonta (6)
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Fusulinina (1)
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problematic microfossils (4)
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Plantae
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algae
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Chlorophyta
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Tasmanites (1)
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diatoms (2)
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Epiphyton (1)
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Rhodophyta (1)
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problematic fossils
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problematic microfossils (4)
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geochronology methods
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Ar/Ar (1)
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U/Pb (1)
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geologic age
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Cenozoic
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Quaternary
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Holocene
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upper Holocene (1)
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Pleistocene
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Lake Lahontan (2)
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middle Pleistocene (1)
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upper Pleistocene (1)
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Tertiary
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Neogene
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Miocene
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lower Miocene
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Aquitanian (1)
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upper Miocene
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Messinian
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Messinian Salinity Crisis (1)
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-
-
Paleogene
-
Eocene
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Green River Formation (2)
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Lake Uinta (1)
-
-
Oligocene
-
upper Oligocene
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Chattian (1)
-
-
-
-
-
-
Lake Bonneville (2)
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Albian (1)
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Middle Cretaceous (1)
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Upper Cretaceous
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Cenomanian (1)
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Jurassic
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Carmel Formation (1)
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Middle Jurassic
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Norphlet Formation (1)
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Upper Jurassic
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Kimmeridgian (1)
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Oxfordian (2)
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Smackover Formation (2)
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-
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Navajo Sandstone (1)
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Triassic
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Lower Triassic
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Induan (1)
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Permian-Triassic boundary (8)
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Smithian (1)
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Middle Triassic
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Anisian (1)
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Moenkopi Formation (2)
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Upper Triassic
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Carnian (1)
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Norian (2)
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Rhaetian
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Penarth Group (2)
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-
-
-
-
Paleozoic
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Arbuckle Group (1)
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Cambrian
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Lower Cambrian (2)
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Middle Cambrian
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Flathead Sandstone (1)
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Zhangxia Formation (1)
-
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Upper Cambrian
-
Copper Ridge Dolomite (1)
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Furongian (2)
-
Maynardville Limestone (1)
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Nopah Formation (1)
-
-
-
Carboniferous
-
Mississippian
-
Lower Mississippian
-
Tournaisian (1)
-
-
-
Pennsylvanian
-
Hermosa Group (1)
-
Middle Pennsylvanian
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Moscovian (1)
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Paradox Formation (1)
-
-
-
-
Devonian
-
Lower Devonian
-
Emsian (1)
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Pragian (1)
-
-
Old Red Sandstone (1)
-
Upper Devonian
-
Famennian
-
upper Famennian (1)
-
-
-
-
Ordovician
-
Lower Ordovician
-
Manitou Formation (1)
-
-
Upper Ordovician
-
Bighorn Dolomite (1)
-
Katian (1)
-
-
-
Permian
-
Guadalupian
-
Capitan Formation (1)
-
Grayburg Formation (1)
-
-
Upper Permian
-
Permian-Triassic boundary (8)
-
Zechstein (1)
-
-
-
Silurian
-
Lockport Formation (1)
-
Middle Silurian (1)
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Niagaran (1)
-
Upper Silurian (1)
-
-
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Precambrian
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Archean
-
Gilman Formation (1)
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Mesoarchean (1)
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Neoarchean (1)
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Paleoarchean (1)
-
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Fortescue Group (1)
-
Gunflint Iron Formation (1)
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Noonday Dolomite (1)
-
upper Precambrian
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Proterozoic
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Damara System (1)
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Mesoproterozoic (3)
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Neoproterozoic
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Cryogenian (1)
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Dengying Formation (1)
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Doushantuo Formation (1)
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Ediacaran (3)
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Otavi Group (1)
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Vendian (1)
-
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Paleoproterozoic (1)
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Sinian
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Dengying Formation (1)
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Doushantuo Formation (1)
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-
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metamorphic rocks
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turbidite (3)
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minerals
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carbonates
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aragonite (3)
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calcite (4)
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dolomite (4)
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oxides
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-
silicates
-
framework silicates
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silica minerals
-
quartz (1)
-
-
-
orthosilicates
-
nesosilicates
-
zircon group
-
zircon (1)
-
-
-
-
sheet silicates
-
clay minerals
-
stevensite (1)
-
-
-
-
sulfates
-
barite (1)
-
gypsum (1)
-
-
sulfides
-
pyrite (3)
-
-
-
Primary terms
-
absolute age (4)
-
Africa
-
Central Africa
-
Angola (1)
-
-
East Africa
-
Kenya
-
Lake Magadi (2)
-
-
Lake Natron (2)
-
Lake Turkana (2)
-
-
East African Lakes
-
Lake Magadi (2)
-
Lake Natron (2)
-
Lake Tanganyika (2)
-
Lake Turkana (2)
-
-
North Africa
-
Atlas Mountains
-
Moroccan Atlas Mountains
-
High Atlas (1)
-
-
-
Morocco
-
Moroccan Atlas Mountains
-
High Atlas (1)
-
-
-
-
Southern Africa
-
Namibia (4)
-
South Africa
-
Northern Cape Province South Africa (1)
-
-
-
West Africa
-
Taoudenni Basin (1)
-
-
-
Arctic region (1)
-
Asia
-
Arabian Peninsula
-
Oman (2)
-
Saudi Arabia (1)
-
United Arab Emirates
-
Abu Dhabi (1)
-
-
-
Far East
-
China
-
Guangxi China (1)
-
Guizhou China (3)
-
Nanpanjiang Basin (5)
-
North China Platform (1)
-
Shandong China (2)
-
Sichuan Basin (1)
-
Sichuan China (3)
-
Yangtze Platform (2)
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Yunnan China (1)
-
-
Indonesia
-
Sunda Arc (1)
-
-
Japan
-
Kyushu (1)
-
-
-
Middle East
-
Iraq (1)
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Mesopotamia (1)
-
Turkey (1)
-
-
-
Atlantic Ocean
-
North Atlantic
-
North Sea (1)
-
Northeast Atlantic (1)
-
Tongue of the Ocean (1)
-
-
South Atlantic
-
Santos Basin (1)
-
Southwest Atlantic (1)
-
-
-
Australasia
-
Australia
-
Great Artesian Basin (1)
-
Queensland Australia (2)
-
Western Australia
-
Pilbara (1)
-
Pilbara Craton (1)
-
-
-
-
bacteria (7)
-
brines (1)
-
Canada
-
Eastern Canada
-
Baffin Island (1)
-
Ontario
-
Thunder Bay District Ontario
-
Thunder Bay Ontario (1)
-
-
-
-
Nunavut
-
Baffin Island (1)
-
-
Western Canada
-
British Columbia (1)
-
-
-
carbon
-
C-13 (1)
-
C-13/C-12 (23)
-
C-14 (2)
-
-
Caribbean region
-
West Indies
-
Bahamas (5)
-
Cayman Islands
-
Grand Cayman Island (1)
-
-
-
-
Cenozoic
-
Quaternary
-
Holocene
-
upper Holocene (1)
-
-
Pleistocene
-
Lake Lahontan (2)
-
middle Pleistocene (1)
-
upper Pleistocene (1)
-
-
-
Tertiary
-
Neogene
-
Miocene
-
lower Miocene
-
Aquitanian (1)
-
-
upper Miocene
-
Messinian
-
Messinian Salinity Crisis (1)
-
-
-
-
-
Paleogene
-
Eocene
-
Green River Formation (2)
-
Lake Uinta (1)
-
-
Oligocene
-
upper Oligocene
-
Chattian (1)
-
-
-
-
-
-
Chordata
-
Vertebrata (1)
-
-
climate change (1)
-
crust (1)
-
crystal growth (1)
-
data processing (1)
-
diagenesis (22)
-
ecology (1)
-
education (1)
-
Europe
-
Alps
-
Eastern Alps
-
Dolomites
-
Latemar Massif (1)
-
-
-
-
Central Europe
-
Poland (1)
-
Switzerland
-
Jura Switzerland (1)
-
Swiss Jura Mountains (1)
-
-
-
Jura Mountains
-
Swiss Jura Mountains (1)
-
-
Southern Europe
-
Iberian Peninsula
-
Duero Basin (1)
-
Spain
-
Aragon Spain (1)
-
Betic Cordillera (1)
-
Castilla y Leon Spain (1)
-
Castilla-La Mancha Spain (1)
-
Madrid Basin (1)
-
Prebetic Zone (1)
-
-
-
Italy
-
Apennines
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Advanced two- and three-dimensional insights into Earth's oldest stromatolites (ca. 3.5 Ga): Prospects for the search for life on Mars
Messinian seep-carbonates marking the transition to the evaporite deposits in the Romagna sector of the northern Apennines (Italy)
Microbialites of modern siliciclastic rock coasts
Insights into the Devonian–Carboniferous transition and Hangenberg Event from δ 13 C carb and 87 Sr/ 86 Sr chemostratigraphy of shallow platform carbonate strata of northwestern Colorado
TAPHONOMIC CONTROLS ON MICROBIALITE TEXTURES FROM THE STEAMBOAT POINT MEMBER, UPPER ORDOVICIAN BIGHORN DOLOMITE, WESTERN TETON MOUNTAINS, USA
Composite microbialites: Thrombolite, dendrolite, and stromatolite associations in a modern environment, Pozo Bravo lake, Salar de Antofalla, Catamarca Puna, Argentina
False biosignatures on Mars: anticipating ambiguity
The Limagne Basin: a journey through modern and fossil microbial deposits
Revisiting the phosphorite deposit of Fontanarejo (central Spain): new window into the early Cambrian evolution of sponges and the microbial origin of phosphorites
Photogrammetry of sequence and bioherm morphology in the Paradox Formation, Utah, U.S.A.: A test of the coherence of Pennsylvanian (Moscovian) glacio-eustatic sea-level change
Depositional system and lake-stage control on microbialite morphology, Green River Formation, eastern Uinta Basin, Colorado and Utah, U.S.A.
Carbonate fabric diversity and environmental heterogeneity in the late Mesoproterozoic Era
Lipid composition of the microbial mat from a hypersaline environment (Vermelha Lagoon, Rio de Janeiro, Brazil)
The influence of benthic diatoms on the textures of carbonate-coated grains from a fluvial tufa spring in northern California
Microstructure and mineral composition of Holocene stromatolites from Lagoa Vermelha, a hypersaline lagoon in Brazil: Insights into laminae genesis
MICROBIALITE OCCURRENCE AND PATTERNS IN HOLOCENE REEFS OF BORA BORA, SOCIETY ISLANDS
ABSTRACT The Guerrero-Morelos carbonate platform (southwestern Mexico) is one of the rare platforms that persisted throughout the Cenomanian–Turonian oceanic anoxic event 2 (OAE 2). Two sections from this carbonate platform exhibit the typical δ 13 C positive excursion characterizing the OAE 2. This enables the precise distribution of larger benthic foraminifers and their biotic response to paleoenvironmental changes to be characterized during this event. At Axaxacualco, oligotrophic conditions prevailed during the δ 13 C positive excursion in the distal part of the carbonate platform. In the more proximal part, at Barranca del Cañon, OAE 2 impact was more significant and is marked by thick laminated microbialite deposition, indicating mesotrophic conditions. Low phosphorus and trace-element contents confirm the persistence of oligotrophic to mesotrophic conditions throughout OAE 2 in the Central Mexico carbonate platform despite the proximity of the Caribbean-Colombian oceanic plateau. Before the δ 13 C positive excursion, which characterizes the OAE 2, the microfauna assemblage was well diversified, including corals, rudists, and large benthic foraminifera ( Pseudorhapydionina chiapanensis , Pseudorhapydionina dubia , Cuneolina parva , Dicyclina sp., Chrysalidina gradata , and large miliolids). During the δ 13 C positive excursion, significant biotic changes occurred, with increasing dominance of organisms adapted to high-stress conditions. Endobenthic assemblages such as Nezzazatinella sp. and Nezzazata sp. were still present. The green symbiotic benthic foraminifera nearly disappeared, except C. parva and Dicyclina sp. During the basal Turonian, the carbonate platform returned to a more open and oxygenated environment, with the reappearance of pre-OAE microfauna, but without the large benthic foraminifera, which did not survive. The definitive drowning of the Guerrero-Morelos carbonate platform took place after the early Turonian, well above the end of the δ 13 C shift. The deposition of black shale and turbidites, which indicate deeper, anoxic environments, precluded large benthic foraminifera reestablishment. Correlation with the pelagic environments of the Eastbourne section (UK) reveals a synchronicity of biotic responses between basin and platform environments. Low-oxygen conditions are marked by multiple blooms of Heterohelix species in the basin, corresponding to an assemblage dominated by ? Decastronema , Thaumatoporella , and Istriloculina on the carbonate platforms.