Comparison between Recent benthic foraminiferal faunas of the Porcupine Seabight and Western Approaches Continental Slope

Weston, Janice F.

doi:https://doi.org/10.1144/jm.4.2.165

Articles | Volume 4, issue 2

Article
Metrics
Related articles

Articles | Volume 4, issue 2

https://doi.org/10.1144/jm.4.2.165

Articles | Volume 4, issue 2

Article
Metrics
Related articles

01 Aug 1985

| 01 Aug 1985

Comparison between Recent benthic foraminiferal faunas of the Porcupine Seabight and Western Approaches Continental Slope

Janice F. Weston

SSI Limited, Tannery House, Tannery Lane, Send, Woking, Surrey GU23 7EF, U.K.

Cited articles

E., Boltovskoy and R., Wright: Recent Foraminifera, 515 ppDrWJunkb.v., Publishers., 1976.

M., Caralp, A., Lamy and M., Pujos: Contribution a la connaissance de la distribution bathymetrique des foraminiferes dans le Golfe de Gascogne, Revta esp. Micropaleont, 2, 55-84, 1970.

L. H. N., Cooper: Physical and chemical oceanography of the waters bathing the continental slope of the Celtic Sea, J. mar. biol. Ass. U.K., 30, 465-510, 1952.

L. H. N., Cooper and D., Vaux: Cascading over the continental slope of water from the Celtic Sea, J. mar. biol. Ass. U.K., 28, 719-750, 1949.

A. A., Day: The continental slope between Brittany and Ireland, Deep Sea Res, 5, 249-265, 1959.

F.-W., Haake: Benthische Foraminiferen in Oberflachen-Sedimenten und Kernen des Ostatlantiks vor Senegal/Gambia (Westafrika), ‘Meteor’ Forschungsergeb, C32, 1-29, 1980.

N. S., Heaps: A mechanism for local upwelling along the European continental slope, Oceanol. Acta, 3, 449-454, 1980.

W. E., Hendrix: Foraminiferal shell form, a key to sedimentary environment, J. Paleont, 38, 87-89, 1958.

Y., Herman: Paleoclimatic and paleohydrologic record of Mediterranean Deep Sea cores based on pteropods, planktonic and benthic foraminifera, Revta esp. Micropaleont, 13, 171-200, 1981.

N. H., Kenyon, R. H., Belderson and A. H., Stride: Channels, canyons and slump folds on the continental slope between SW Ireland and Spain, Oceanol. Acta, 1, 369-380, 1978.

M. K., Kontrovitz, S. W., Snyder and R. J., Brown: A flume study of the movement of foraminiferid tests, Palaeogeogr., Palaeoclimatol., Palaeoecol, 23, 141-151, 1978.

G. F., Lutze: Depth distribution of benthic foraminifera on the continental margin off NW Africa, ‘Meteo’ Forschungsergeb, C23, 31-80, 1980.

Y., Mart, G. A., Auffret, J. M., Auzende and L., Pastouret: Geological observations from a submersible dive on the Western continental slope of the Armorican Massif, Mar. Geol, 31, M61-M68, 1979.

R. J., Menzies, R. Y., George and G. T., Rowe: Abyssal environment and ecology of the world oceans, 480 ppJohn Wiley & Sons, N.Y., 1973.

K. G., Miller and G. P., Lohmann: Environmental distribution of Recent benthic foraminifera on the Northeast U.S. continental slope, Bull geol. Soc. Am, 93, 200-206, 1982.

J. W., Murray: Production in benthic foraminiferids, J. nat. Hist, 1, 61-68, 1967.

J. W., Murray: .An Atlas of British Recent Foraminiferids, 244 ppHeinemann, London., 1971.

J. W., Murray: Distribution and Ecology of Living Benthic Foraminiferids, 274 ppHeinemann, London., 1973.

J. W., Murray: Benthic Foraminifera: some relationships between ecological observations and palaeoecological interpretations, Benthos ’83, 2nd Int. Symp. Benthic Foraminifera (Pau, April 1983), 465-469, 1984.

J. W., Murray, S., Sturrock and J., Weston: Suspended load transport of foraminiferal tests in a tide- and wave-swept sea, J. Foramin. Res, 12, 51-65, 1982.

J. W., Murray, J. F., Weston and S., Sturrock: Sedimentary indicators of water movement in the western approaches to the English Channel, Cont. Shelf Res, 1, 339-352, 1983.

T. R., Owen: The Geology of the Western ApproachesIn (Eds.), The Ocean Basins and Margins2The North Atlantic, 233–272., 1974.

R. D., Pingree and G. T., Mardell: Slope turbulence, internal waves and phytoplankton growth at the Celtic Sea shelf break, Phil. Trans. R. Soc. Lond, A302, 663-682, 1981.

M., Pujos: Influence des eaux de type mediterranean sur la repartitions de certains foraminiferes benthiques dans le Golfe de Gascogne, Cah. oceanogr, 22, 827-831, 1970.

A., Pujos-Lamy: Repartition bathymetrique des foraminiferes benthiques profonds du Golfe de Gascogne. Comparaison avec d’autres aires oceaniques, Revta esp. Micropaleont, 5, 213-234, 1973.

M. A., Rex: Biological accommodation in the deep sea benthos: comparative evidence on the importance of predation and productivity, Deep Sea Res, 23, 975-987, 1976.

G. T., Rowe and R. L., Haedrich: The biota and biological processes of the continental slopeIn (Eds.), Geology of the Continental SlopesSpecPublsSoceconPalaeontMiner., Tulsa, 27, 49–59., 1979.

W. C., Seiler: Tiefenverteilung benthischer Foraminiferen am portugiesischen KontinentalhangPhDthesis, Kiel, Germany, 107 pp., 1973.

W. C., Seiler: Tiefenverteilung benthischer Foraminiferen am portugiesischen Kontinentalhang, ‘Meteor’ Forschungsergeb, C23, 47-94, 1975.

B. K., Sen Gupta, R. F., Lee and M. S., May: Upwelling and an unusual assemblage of benthic foraminifera on the northern Florida continental slope, J. Paleont, 55, 853-857, 1981.

F. P., Shepard: Submarine Geology, 3rd ed., 517 pp, Harper and Row Publ., 1973.

F. P., Shepard, N. F., Marshall, P. A., McLoughlin and G. G., Sullivan: Currents in Submarine Canyons and other Sea-valleys, AAPG Studies in Geology, 8, 171 pp, Tulsa, Oklahoma., 1979.

S., Sturrock and J. W., Murray: Comparison of low energy and high energy marine middle shelf foraminiferal faunas; Celtic Sea and western English ChannelIn , Microfossils from Recent and Fossil Shelf SeasEllis Horwood Ltd., Chichester, 250–260 for British Micropalaeontological Society., 1981.

L., Watling, P. C., Kinner and D., Maurer: The use of species abundance estimates in marine biological studies, J. Exp. Mar. Biol. and Ecol, 35, 109-118, 1978.

J. F., Weston: Distribution and Ecology of Recent deep sea benthic Foraminifera in the northeast Atlantic OceanUnpublPhDThesis, University of Exeter, 442 pp., 1982.

J. F., Weston: (in prep.) Downslope transport of foraminiferal tests on the European continental slope.