Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Saccammina"'
Autor:
Theresa Winchester-Seeto, K. N. Bell
The organic linings of agglutinated foraminiferans from the Devonian are documented and described. These linings have been recovered in palynological residues from Australia, France, Pakistan and Siberia and range from the Lochkovian to the Frasnian.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9b0815ed1d509502aeaf53beef455593
https://www.j-micropalaeontol.net/18/27/1999/
https://www.j-micropalaeontol.net/18/27/1999/
Publikováno v:
Journal of Micropalaeontology. 28:143-151
Saccammina minimus sp. nov., a spherical agglutinated organism presumed to be a foraminiferan, is described from the Kaplan Central site in the abyssal eastern Equatorial Pacific (5042 m water depth). The new species is minute in size (32 μm of samp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aa859c31589dae54c64c0536b679c200
https://doi.org/10.1144/jm.28.2.143
https://doi.org/10.1144/jm.28.2.143
Autor:
Susan T. Goldstein
Publikováno v:
The Journal of Foraminiferal Research. 18:311-325
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9f481e439f76ba71abdeaf5e0c13fce1
https://doi.org/10.2113/gsjfr.18.4.311
https://doi.org/10.2113/gsjfr.18.4.311
Publikováno v:
Annals and Magazine of Natural History. 1:215-218
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bdfd076ab5f2939179f39bec1b3e91ab
https://doi.org/10.1080/00222939808677956
https://doi.org/10.1080/00222939808677956
Autor:
William Johnson Sollas
Publikováno v:
Quarterly Journal of the Geological Society. 77:193-212
This remarkable foraminifer, which contributes so largely to the formation of some of our Carboniferous Limestone beds, was first described by H. B. Brady in 1871, and assigned by him to the existing arenaceous genus Saccammina (Sars). His views on i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1a15b1bc1d3a672f8a54902a9fe43055
https://doi.org/10.1144/gsl.jgs.1921.77.01-04.10
https://doi.org/10.1144/gsl.jgs.1921.77.01-04.10
Autor:
John Young
Publikováno v:
Transactions of the Geological Society of Glasgow. 4:263-266
The organism which forms the subject of the following remarks was found, as far back as the year 1864, while on an excursion in the Carluke district, in company with Messrs. Armstrong and Thomson. On that occasion we were conducted to several interes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1ccd98f2041dcd50d452fb5a15e91b78
https://doi.org/10.1144/transglas.4.3.263
https://doi.org/10.1144/transglas.4.3.263
Autor:
Yvon Globensky
Publikováno v:
Canadian Journal of Earth Sciences. 7:768-785
Arenaceous foraminifera have been obtained from the insoluble residues of limestones from the Windsor Group (Valmeyeran—Chesterian) of the Atlantic Provinces of Canada. From the arenaceous foraminifera fauna 10 genera and 27 species have been ident
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f756d6ae9b7e19f595ceb0a4e7322d4a
https://doi.org/10.1139/e70-077
https://doi.org/10.1139/e70-077
Autor:
T. C. Archer
Publikováno v:
Proceedings of the Royal Society of Edinburgh. 7:353-355
Mr Archer exhibited two interesting Foraminifers, one being Saccammina Carteri, which forms a large proportion of the Carboniferous limestone at Elfhills, Northumberland; the other, a gigantic species of the Arenaceous group brought from Persia by th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f92ff41b5c2b00c693b0fadf79190e43
https://doi.org/10.1017/s0370164600042164
https://doi.org/10.1017/s0370164600042164
Autor:
John Young
The Foraminiferal group of organisms, recent and fossil, have always afforded an interesting branch of investigation to those persons who have taken it up, either for examination and study under the microscope, or for the purpose of forming a collect
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6b4743dc3c4aa7bf07347a15dc574698
https://zenodo.org/record/2228242
https://zenodo.org/record/2228242
Autor:
Charles Edmonds
SummaryThe examination of the fossil fauna, the chief forms of which are shown in Tables I and II and Fig. 1, shows that the beds commence at a high horizon of the Seminula Zone and extend to the top of the Dibunophyllum Zone. Also, the “life-zones
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3c00cda6cf6c20a5e24cbff1215975f8
https://zenodo.org/record/1513766
https://zenodo.org/record/1513766