|
Brochocoleus Tobini
''Brochocoleus'' is an extinct genus of beetles in the family Ommatidae, known from the Early Jurassic to the Early Late Cretaceous. 9 species are currently recognised, with many species being reassigned to other genera by Kirejtshuk's major systematic revision in 2020. * †''Brochocoleus alatus'' Ponomarenko, 1994 Ulan-Argalant Formation, Mongolia, Barremian * †''Brochocoleus cossiphus'' Ponomarenko, 1994 Dzun-Bain Formation, Mongolia, Aptian * †''Brochocoleus keenani'' Jarzembowski, Yan, Wang & Zhang, 2013 Weald Clay, United Kingdom, Barremian * †''Brochocoleus maculatus'' (Whalley 1985) Charmouth Mudstone Formation, United Kingdom, Sinemurian * †''Brochocoleus maximus'' Jarzembowski, Yan, Wang & Zhang, 2013 Purbeck Group, United Kingdom, Berriasian * †''Brochocoleus planus'' Ponomarenko, 1994 Dzun-Bain Formation, Mongolia, Aptian * †''Brochocoleus punctatus'' Hong, 1982 (type species) Chijinbao Formation, China, Aptian * †''Brochocoleus rostratus'' Ponomaren ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Animal
Animals are multicellular, eukaryotic organisms in the Kingdom (biology), biological kingdom Animalia. With few exceptions, animals Heterotroph, consume organic material, Cellular respiration#Aerobic respiration, breathe oxygen, are Motility, able to move, can Sexual reproduction, reproduce sexually, and go through an ontogenetic stage in which their body consists of a hollow sphere of Cell (biology), cells, the blastula, during Embryogenesis, embryonic development. Over 1.5 million Extant taxon, living animal species have been Species description, described—of which around 1 million are Insecta, insects—but it has been estimated there are over 7 million animal species in total. Animals range in length from to . They have Ecology, complex interactions with each other and their environments, forming intricate food webs. The scientific study of animals is known as zoology. Most living animal species are in Bilateria, a clade whose members have a Symmetry in biology#Bilate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Charmouth Mudstone Formation
The Charmouth Mudstone Formation is a geological formation in England. It preserves fossils dating back to the early part of the Jurassic period (Sinemurian–Pliensbachian). It forms part of the lower Lias Group. It is most prominently exposed at its type locality in cliff section between Lyme Regis and Charmouth (alongside the underlying Blue Lias) but onshore it extends northwards to Market Weighton, Yorkshire, and in the subsurface of the East Midlands Shelf and Wessex Basin. The formation is notable for its fossils, including those of ammonites and marine reptiles and rare dinosaur remains. The formation played a prominent role in the history of early paleontology, with its Lyme Regis-Charmouth exposure being frequented by fossil collectors including Mary Anning. Stratigraphy Shales With Beef Member The Shales With Beef Member is around 28–30 metres thick in the Lyme Regis-Charmouth region and predominantly consists of thinly bedded medium to dark grey mudstone, blocky ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Allophalerus
''Allophalerus'' is an extinct genus of beetle in the family Ommatidae. Systematics * †''Allophalerus antiquus'' (Ponomarenko 1964) Karabastau Formation, Kazakhstan, Oxfordian * †''Allophalerus aphaleratus'' (Ponomarenko 1969) Kyzyl-Kiya, Kyrgyzstan, Pliensbachian * †''Allophalerus bontsaganensis'' (Ponomarenko 1997) Dzun-Bain Formation, Mongolia, Aptian * †''Allophalerus incertus'' (Ponomarenko 1969) Dzhil Formation, Kyrgyzstan, Hettangian * †''Allophalerus latus'' (Tan et al. 2007) Yixian Formation, China, Aptian * †''Allophalerus maximus'' (Ponomarenko 1968) Karabastau Formation, Kazakhstan, Oxfordian * †''Allophalerus okhotensis'' (Ponomarenko 1993) Emanra Formation, Russian Federation, Turonian * †''Allophalerus tenuipes'' (Ponomarenko 1964) Karabastau Formation, Kazakhstan, Oxfordian * †''Allophalerus verrucosus'' (Ponomarenko 1966) Zaza Formation The Zaza Formation is a geological formation located in Buryatia (Russia). It dates to the Lower Cret ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pareuryomma
''Pareuryomma'' is an extinct genus of Ommatine beetle. It is known from three species, ''P. angustum, P. cardiobasis'' and P''. tylodes'', all known from the Aptian aged Yixian Formation of China. The genus was first described in 2012, and formerly included the species ''Pareuryomma ancistrodonta'' from the Middle Jurassic Jiulongshan Formation, China, which was transferred to the genus '' Omma'' in 2020. The species ''P. angustum'' was formerly thought to be part of ''Brochocoleus ''Brochocoleus'' is an extinct genus of beetles in the family Ommatidae, known from the Early Jurassic to the Early Late Cretaceous. 9 species are currently recognised, with many species being reassigned to other genera by Kirejtshuk's major sys ...''. The genus is characterised by "slender body, long and subparallelsided or slightly narrowed head with moderately prominent eyes and more or less prominent temples, narrow pronotum with more or less explanate lateral carinae, elytra with the veins mo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hauterivian
The Hauterivian is, in the geologic timescale, an age in the Early Cretaceous Epoch or a stage in the Lower Cretaceous Series. It spans the time between 132.9 ± 2 Ma and 129.4 ± 1.5 Ma (million years ago). The Hauterivian is preceded by the Valanginian and succeeded by the Barremian.See Gradstein ''et al.'' (2004) for a detailed geologic timescale Stratigraphic definitions The Hauterivian was introduced in scientific literature by Swiss geologist Eugène Renevier in 1873. It is named after the Swiss town of Hauterive at the shore of Lake Neuchâtel. The base of the Hauterivian is defined as the place in the stratigraphic column where the ammonite genus ''Acanthodiscus'' first appears. A reference profile for the base (a GSSP) was officially ratified by the International Union of Geological Sciences in December of 2019, and is placed in La Charce, France. The top of the Hauterivian (the base of the Barremian) is at the first appearance of ammonite species ''Spitidiscus hugii'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brochocoleus Tobini
''Brochocoleus'' is an extinct genus of beetles in the family Ommatidae, known from the Early Jurassic to the Early Late Cretaceous. 9 species are currently recognised, with many species being reassigned to other genera by Kirejtshuk's major systematic revision in 2020. * †''Brochocoleus alatus'' Ponomarenko, 1994 Ulan-Argalant Formation, Mongolia, Barremian * †''Brochocoleus cossiphus'' Ponomarenko, 1994 Dzun-Bain Formation, Mongolia, Aptian * †''Brochocoleus keenani'' Jarzembowski, Yan, Wang & Zhang, 2013 Weald Clay, United Kingdom, Barremian * †''Brochocoleus maculatus'' (Whalley 1985) Charmouth Mudstone Formation, United Kingdom, Sinemurian * †''Brochocoleus maximus'' Jarzembowski, Yan, Wang & Zhang, 2013 Purbeck Group, United Kingdom, Berriasian * †''Brochocoleus planus'' Ponomarenko, 1994 Dzun-Bain Formation, Mongolia, Aptian * †''Brochocoleus punctatus'' Hong, 1982 (type species) Chijinbao Formation, China, Aptian * †''Brochocoleus rostratus'' Ponomaren ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Turonian
The Turonian is, in the ICS' geologic timescale, the second age in the Late Cretaceous Epoch, or a stage in the Upper Cretaceous Series. It spans the time between 93.9 ± 0.8 Ma and 89.8 ± 1 Ma (million years ago). The Turonian is preceded by the Cenomanian Stage and underlies the Coniacian Stage. At the beginning of the Turonian an oceanic anoxic event (OAE 2) took place, also referred to as the Cenomanian-Turonian boundary event or the "Bonarelli Event". Stratigraphic definition The Turonian (French: ''Turonien'') was defined by the French paleontologist Alcide d'Orbigny (1802–1857) in 1842. Orbigny named it after the French city of Tours in the region of Touraine (department Indre-et-Loire), which is the original type locality. The base of the Turonian Stage is defined as the place where the ammonite species '' Watinoceras devonense'' first appears in the stratigraphic column. The official reference profile (the GSSP) for the base of the Turonian is located in the Roc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brochocoleus Rostratus
''Brochocoleus'' is an extinct genus of beetles in the family Ommatidae, known from the Early Jurassic to the Early Late Cretaceous. 9 species are currently recognised, with many species being reassigned to other genera by Kirejtshuk's major systematic revision in 2020. * †'' Brochocoleus alatus'' Ponomarenko, 1994 Ulan-Argalant Formation, Mongolia, Barremian * †'' Brochocoleus cossiphus'' Ponomarenko, 1994 Dzun-Bain Formation, Mongolia, Aptian * †'' Brochocoleus keenani'' Jarzembowski, Yan, Wang & Zhang, 2013 Weald Clay, United Kingdom, Barremian * †''Brochocoleus maculatus'' (Whalley 1985) Charmouth Mudstone Formation, United Kingdom, Sinemurian * †'' Brochocoleus maximus'' Jarzembowski, Yan, Wang & Zhang, 2013 Purbeck Group, United Kingdom, Berriasian * †'' Brochocoleus planus'' Ponomarenko, 1994 Dzun-Bain Formation, Mongolia, Aptian * †'' Brochocoleus punctatus'' Hong, 1982 (type species) Chijinbao Formation, China, Aptian * †'' Brochocoleus rostratus'' Po ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brochocoleus Punctatus
''Brochocoleus'' is an extinct genus of beetles in the family Ommatidae, known from the Early Jurassic to the Early Late Cretaceous. 9 species are currently recognised, with many species being reassigned to other genera by Kirejtshuk's major systematic revision in 2020. * †'' Brochocoleus alatus'' Ponomarenko, 1994 Ulan-Argalant Formation, Mongolia, Barremian * †'' Brochocoleus cossiphus'' Ponomarenko, 1994 Dzun-Bain Formation, Mongolia, Aptian * †''Brochocoleus keenani'' Jarzembowski, Yan, Wang & Zhang, 2013 Weald Clay, United Kingdom, Barremian * †''Brochocoleus maculatus'' (Whalley 1985) Charmouth Mudstone Formation, United Kingdom, Sinemurian * †'' Brochocoleus maximus'' Jarzembowski, Yan, Wang & Zhang, 2013 Purbeck Group, United Kingdom, Berriasian * †''Brochocoleus planus'' Ponomarenko, 1994 Dzun-Bain Formation, Mongolia, Aptian * †'' Brochocoleus punctatus'' Hong, 1982 (type species) Chijinbao Formation, China, Aptian * †''Brochocoleus rostratus'' Ponom ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brochocoleus Planus
''Brochocoleus'' is an extinct genus of beetles in the family Ommatidae, known from the Early Jurassic to the Early Late Cretaceous. 9 species are currently recognised, with many species being reassigned to other genera by Kirejtshuk's major systematic revision in 2020. * †'' Brochocoleus alatus'' Ponomarenko, 1994 Ulan-Argalant Formation, Mongolia, Barremian * †'' Brochocoleus cossiphus'' Ponomarenko, 1994 Dzun-Bain Formation, Mongolia, Aptian * †''Brochocoleus keenani'' Jarzembowski, Yan, Wang & Zhang, 2013 Weald Clay, United Kingdom, Barremian * †''Brochocoleus maculatus'' (Whalley 1985) Charmouth Mudstone Formation, United Kingdom, Sinemurian * †'' Brochocoleus maximus'' Jarzembowski, Yan, Wang & Zhang, 2013 Purbeck Group, United Kingdom, Berriasian * †'' Brochocoleus planus'' Ponomarenko, 1994 Dzun-Bain Formation, Mongolia, Aptian * †'' Brochocoleus punctatus'' Hong, 1982 (type species) Chijinbao Formation, China, Aptian * †''Brochocoleus rostratus'' Pono ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Berriasian
In the geological timescale, the Berriasian is an age/stage of the Early/Lower Cretaceous. It is the oldest subdivision in the entire Cretaceous. It has been taken to span the time between 145.0 ± 4.0 Ma and 139.8 ± 3.0 Ma (million years ago). The Berriasian succeeds the Tithonian (part of the Jurassic) and precedes the Valanginian. Stratigraphic definition The Berriasian Stage was introduced in scientific literature by Henri Coquand in 1869. It is named after the village of Berrias in the Ardèche department of France. The largely non-marine English Purbeck Formation is in part of Berriasian age.In fact, the first rocks to be described of this age were the beds of the English Purbeck Formation, named as the Purbeckian by Alexandre Brongniart in 1829 following description by Henry De la Beche, William Buckland, Thomas Webster and William Henry Fitton. The base of the Berriasian, which is also the base of the Cretaceous System, has traditionally been placed at the first ap ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
