Recent shallow marine Ostracoda of the Ikerssuak (Bredefjord) District, Southwest Greenland

Autor: David N. Penney

From a study of 15 grab samples collected from the littoral and sublittoral of the Ikerssuak (Bredefjord) district, SW Greenland, one myodocopid and 18 podocopid ostracod species were recovered. These constitute an indigenous fauna and the majority h

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1c4365291be323898cbaa54c3914f77a
https://www.j-micropalaeontol.net/8/55/1989/

Quaternary marine stratigraphy and geochronology in central West Greenland

Autor: Karen Luise Knudsen, Kaare Lund Rasmussen, David N. Penney, Ole Bennike, Karen Bille Hansen

Publikováno v: ResearcherID
BENNIKE, OLE, HANSEN, KAREN BILLE, KNUDSEN, KAREN LUISE, PENNEY, DAVID N & RASMUSSEN, KAARE LUND 1994, ' Quaternary marine stratigraphy and geochronology in central West Greenland ', Boreas, vol. 23, no. 2, pp. 194-215 . https://doi.org/10.1111/j.1502-3885.1994.tb00599.x

A new stratigraphic framework is proposed for the Quaternary of a portion of central West Greenland, based primarily on faunal and geochronologic studies of shallow shelf deposits. Twenty‐four occurrences of pre‐Holocene deposits were already kno

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::390dcc81578e55aae05b7846ff18b991
https://doi.org/10.1111/j.1502-3885.1994.tb00599.x

Palaeontology and taphonomy of Late Quaternary fossil assemblages at Somersham, Cambridgeshire, England, and the problem of reworking

Autor: Richard Gilbert West, J. Eric Robinson, David N. Penney, K.L. Knudsen, Richard C. Preece

Publikováno v: Journal of Quaternary Science. 9:357-366

Assemblages of foraminifers, ostracods and molluscs from temperate Ipswichian Stage (last temperate stage) sediments and overlying cold Devensian Stage (last cold stage) sediments at Somersham in the southern Fenland of Cambridgeshire have been analy

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::4209896084fd7d80c6802d8a632e5688
https://doi.org/10.1002/jqs.3390090406

Late Pliocene to early Pleistocene ostracod stratigraphy and palaeoclimate of the Lodin Elv and Kap København formations, East Greenland

Autor: David N. Penney

Publikováno v: Palaeogeography, Palaeoclimatology, Palaeoecology. 101:49-66

The Ostracoda documented in the Lodin Elv Formation in East Greenland provide us with data to reconstruct palaeotemperatures during the Late Pliocene. Palaeotemperature estimations use the overlap of temperature ranges of extant species in the deposi

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::7323e5e1aeeaa774a9cbea9d0bdd8f68
https://doi.org/10.1016/0031-0182(93)90151-8

Late and Middle Pleistocene deposits at Somersham, Cambridgeshire, U.K.:A model for reconstructing fluvial/estuarine depositional environments

Autor: V.R. Switsur, John T. Hollin, G.F. Miller, Richard C. Preece, Colin A. Whiteman, J. A. Catt, C.P. Hart, Liping Zhou, David N. Penney, R. Andrew, M. E. Pettit, Richard Gilbert West, K.L. Knudsen

Publikováno v: West, R G, Andrew, R, Catt, J A, Hart, C P, Hollin, J T, Knudsen, K L, Miller, G F, Penney, D N, Pettit, M E, Preece, R C, Switsur, V R, Whiteman, C A & Zhou, L P 1999, ' Late and Middle Pleistocene deposits at Somersham, Cambridgeshire, U.K. A model for reconstructing fluvial/estuarine depositional environments ', Quaternary Science Reviews, vol. 18, no. 10-11, pp. 1247-1314 . https://doi.org/10.1016/S0277-3791(98)00067-5

Gravel quarries at Somersham, Cambridgeshire, have yielded evidence for a Pleistocene channel of the R. Great Ouse, containing temperate stage sediments between cold stage sediments. In the earlier cold stage, fluviatile gravels and floodplain loessi

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6cfc3df916c8dd81756adbcc7183ebda
https://pure.au.dk/portal/da/publications/late-and-middle-pleistocene-deposits-at-somersham-cambridgeshire-uk(eb434c41-829b-44dc-a5f9-506db8c53de6).html