Galerie d'images
Toutes les images de la base — taxons, formations et intervalles géologiques.
⚠ La fonctionnalité de récupération des images est en cours de test, des images non pertinentes peuvent apparaître.
3,072 image(s)
New species of Mesozoic benthic foraminifera from the former British Petroleum micropalaeontology collection, Ophthalmidium dracomaris n. sp. (1) holotype (NHMUK PM PF 74496); (2–5) paratypes (NHMUK PM PF 74497–74500). (8–9) Eobigenerina calloviensis n. sp.: (8) holotype (NHMUK PM PF 74504); (9) paratype (NHMUK PM PF 74505). (10–12) Trochammina fordonensis n. sp.: (10) holotype (NHMUK PM PF 74501); (11–12) paratype (NHMUK PM PF 74502–74503). (13–15) Arenoturrispirillina swiecickii n. sp.: (13) holotype (NHMUK PM PF 74506); (14–15) paratype (NHMUK PM PF 74507 + NHMUK PM PF 74552). (16–17) Ataxophragmium mariae n. sp.: (16) holotype (NHMUK PM PF 74553); (17) paratype (NHMUK PM PF 74554).
Barriolucio (España). Accesos a la localidad.
Jurassic Forest, Cathedral of Ferns - Blue Mountains, New South Wales.
A life reconstruction of the middle Jurassic sauropod, Spinophorosaurus nigerensis, from the nigerian Irhazer Shale.
HKU zh:香港大學 Stephen Hui Geological Museum zh:許士芬地質博物館 Mesozoic 中生代 rocks Oct 2016
locuri preistorice din satul cobilea provin din erele paleozoica si mezoica si cenozoic
Graph of relative Dinosaur fossil populations from each period of geologic time in the Mesozoic, ordered by major clade
1 Quality Square, Ludlow
1 Dinham, Ludlow
1 - 5 Upper Linney
1 - 5 Castle Street
1 - 2 Broad Street
1 - 13 Temeside
'The Kitchen Door' in Quality Square, Ludlow
"The Vaults"
Pseudocidaris mammosa Stage : Kimmeridgian 157.3 ± 1.0 Ma and 152.1 ± 0.9. (million years ago)
Etage: Kimméridgien, Sous-étage: inférieur, Zone: Rasenia cymodoce, Sous-zone: Lithacosphinctes achilles, Horizon: Lithacosphinctes achilles. -150.8 à –155.7 millions d'années.
Fig 2. Geological section of the “Mittlerer Kimmeridge”. This figure is based on Fischer and modified from Lallensack et al. Beds yielding terrestrial fossils are listed.
Steinbruch Langenberg. Steilgestellte Schichten des Jura.
Formation d'âge Kimmeridgien (jaune orangé) et Tithonien (Barre tithonique, en gris sur la photo). On peut remarquer que les strates ont été plissées. L'âge des mouvements tectoniques ayant déformé la structure est donc plus jeune que le Tithonien.
The GSSP for the Hirnantian stage in the ICS geological timescale (uppermost Ordovician stage), located in the Wangjiawan profile (an outcrop of black shale, brownishly weathered siliceous shale and chert layers of the Wufeng Formation) along the G241 road, about 40 km north of Yichang, Hubei, China. An exact golden spike is missing in the profile (2025) but a memorial plague marks the place. The GSSP occurs at the first appearance of fossils of the graptolite species Normalograptus extraordinarius. It was ratified in 2006.
Eleniceras cf. curvicostatum (Tzankov), Lower Hauterivian, Kalotina, Bulgaria Cr1 963X1 at the Sofia University 'St. Kliment Ohriski' Museum of Paleontology and Historical Geology
Eleniceras aff. stevrecensis Breskovski, Lower Hauterivian, Dragoman, Bulgaria, Cr1 959 - Cr1 960 X 1 at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology
DUVALIA POLYGONALIS (BLAINVILLE) HAUTERIVIAN TEKE DERE SHUMEN SOFIA UNIVERSITY 'ST. KLIMENT OHRIDSKI' MUSEUM OF PALEONTOLOGY AND HISTORICAL GEOLOGY
Distoloceras belimelensis sp.n. Lower Hauterivian, Belimel, Montana Province, Cr1 970X1 (Coll. G. Mandov) at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology
Crioceratites (C.) villiersianum bituberculatum (Sarkar) Hauterivian, Belimel, Cr1 929X1 at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology
Acrioceras (Aspinoceras) dilatatum (d'Orbigny) Upper Hauterivian, Belimel, Montana Province, (Coll. G. Mandov) at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology
Acanthodiscus vaceki (Neumayr & Uhlig) Lower Hauterivian, Dragoman, Bulgaria, Cr1 976X1 (Coll. G. Mandov) at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology
Life reconstruction of two species of Protonympha in the Devonian Catskill delta of New York
Monte San Nicola in Sicily, Italy, south of Butera in the province of Caltanissetta. The red line below the '5' on the rock marks the basis of the Gelasian (Lower Pleistocene) 2.58 million years ago. The Gelasian is a geologic age named after the nearby city of Gela in southern Sicily.
Monte San Nicola in Sicily, Italy, south of Butera in the province of Caltanissetta. The rocks seen here are of marine origin and date from the late Pliocene and Pleistocene.
Monte San Nicola in Sicily, Italy, south of Butera in the province of Caltanissetta. The red line below the '5' on the rock marks the basis of the Gelasian (Lower Pleistocene) 2.58 million years ago. The Gelasian is a geologic age named after the nearby city of Gela in southern Sicily. A geologist is seen at work at the red line.
Monte San Nicola in Sicily, Italy, south of Butera in the province of Caltanissetta. The red line below the '5' on the rock marks the basis of the Gelasian (Lower Pleistocene), 2.58 million years ago. The Gelasian is a geologic age named after the nearby city of Gela in southern Sicily. Two geologists are seen at work at the red line.
Monte San Nicola in Sicily, Italy, south of Butera in the province of Caltanissetta. The red line below the '5' on the rock marks the basis of the Gelasian (Lower Pleistocene), 2.58 million years ago. The Gelasian is a geologic age named after the nearby city of Gela in southern Sicily.
Monte San Nicola in Sicily, Italy, south of Butera in the province of Caltanissetta. The red line below the '5' on the rock marks the basis of the Gelasian (Lower Pleistocene), 2.58 million years ago. The Gelasian is a geologic age named after the nearby city of Gela in southern Sicily.
Monte San Nicola in Sicily, Italy, south of Butera in the province of Caltanissetta. The red line below the '5' on the rock marks the basis of the Gelasian (Lower Pleistocene), 2.58 million years ago. The Gelasian is a geologic age named after the nearby city of Gela in southern Sicily.
Kalksandskalk fra København kalk Fm med omlejrede bryozoer (netmønster) og skalstumper
Koralkalk fra Faxe kalkbrud
Main floristic types from the earliest Danian: Cheirolepidiaceae, shrubs and other low–diversity flora. doi:10.1371/journal.pone.0052455.g007
Glacialt forstyrret koralkalk, Faxe
Eekaulostomus cuevasae gen. and sp. nov. from the Danian marine deposits of the Belisario Domínguez quarry, near Palenque, Chiapas, southeastern Mexico. 1, General view of IGM 4716, holotype and single specimen known. 2, Idealized line drawing of the same specimen.
Bryozobanker i Stevns klint, set fra stranden ved Boesdal kalkbrud (i let diset vejr)
Grå flint med fossiler af søpindsvin, Krauseparken i København
