|
Oliver Bulman
Oliver Meredith Boone Bulman (20 May 1902 – 18 February 1974) was a British palaeontologist. He was Woodwardian Professor of Geology at the University of Cambridge. Early life Oliver Bulman was born in Chelsea to artist Henry Herbert Bulman and his wife Beatrice Elizabeth Boone. He was the second of three children. Education Bulman went to Battersea Grammar School in 1910, but wishing to study geology, which the school did not teach, he became an evening, and later day, student at Chelsea Polytechnic. He gained a London University scholarship in 1920 and went to Imperial College to study geology and zoology. He graduated with a first class BSc in geology in 1923. Bulman went on to a PhD degree jointly with James Stubblefield on the lower Palaeozoic of the Wrekin district, of Shropshire in 1926. Awarded a senior studentship, he worked for a year on Permian amphibians with Walter Frederick Whittard and for two years at Sidney Sussex College, Cambridge, where he studied de ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
University Of Cambridge
, mottoeng = Literal: From here, light and sacred draughts. Non literal: From this place, we gain enlightenment and precious knowledge. , established = , other_name = The Chancellor, Masters and Scholars of the University of Cambridge , type = Public research university , endowment = £7.121 billion (including colleges) , budget = £2.308 billion (excluding colleges) , chancellor = The Lord Sainsbury of Turville , vice_chancellor = Anthony Freeling , students = 24,450 (2020) , undergrad = 12,850 (2020) , postgrad = 11,600 (2020) , city = Cambridge , country = England , campus_type = , sporting_affiliations = The Sporting Blue , colours = Cambridge Blue , website = , logo = University of Cambridge logo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Graptolites
Graptolites are a group of colonial animals, members of the subclass Graptolithina within the class Pterobranchia. These filter-feeding organisms are known chiefly from fossils found from the Middle Cambrian (Miaolingian, Wuliuan) through the Lower Carboniferous ( Mississippian). A possible early graptolite, ''Chaunograptus'', is known from the Middle Cambrian. Recent analyses have favored the idea that the living pterobranch ''Rhabdopleura'' represents an extant graptolite which diverged from the rest of the group in the Cambrian. Fossil graptolites and ''Rhabdopleura'' share a colony structure of interconnected zooids housed in organic tubes (theca) which have a basic structure of stacked half-rings (fuselli). Most extinct graptolites belong to two major orders: the bush-like sessile Dendroidea and the planktonic, free-floating Graptoloidea. These orders most likely evolved from encrusting pterobranchs similar to ''Rhabdopleura''. Due to their widespread abundance, plantkonic l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
