Ecological Studies on two Carbonate Sediment-Producing Algae. / Bosence, Daniel.

Fossil Algae. ed. / Erik Flügel. Springer Berlin / Heidelberg, 1977. p. 270-278.

Research output: Chapter in Book/Report/Conference proceedingConference contribution

Published

Standard

Ecological Studies on two Carbonate Sediment-Producing Algae. / Bosence, Daniel.

Fossil Algae. ed. / Erik Flügel. Springer Berlin / Heidelberg, 1977. p. 270-278.

Research output: Chapter in Book/Report/Conference proceedingConference contribution

Harvard

Bosence, D 1977, Ecological Studies on two Carbonate Sediment-Producing Algae. in E Flügel (ed.), Fossil Algae. Springer Berlin / Heidelberg, pp. 270-278. https://doi.org/10.1007/978-3-642-66516-5_29

APA

Bosence, D. (1977). Ecological Studies on two Carbonate Sediment-Producing Algae. In E. Flügel (Ed.), Fossil Algae (pp. 270-278). Springer Berlin / Heidelberg. https://doi.org/10.1007/978-3-642-66516-5_29

Vancouver

Bosence D. Ecological Studies on two Carbonate Sediment-Producing Algae. In Flügel E, editor, Fossil Algae. Springer Berlin / Heidelberg. 1977. p. 270-278 https://doi.org/10.1007/978-3-642-66516-5_29

Author

Bosence, Daniel. / Ecological Studies on two Carbonate Sediment-Producing Algae. Fossil Algae. editor / Erik Flügel. Springer Berlin / Heidelberg, 1977. pp. 270-278

BibTeX

@inproceedings{93aca3725ad047599128f1b3514672ef,
title = "Ecological Studies on two Carbonate Sediment-Producing Algae",
abstract = "The bathymetIy and location of Mannin Bay are shown in Fig. 1. A submarine valley leads into the bay and up to a slope that levels off at about 8 m to form a platform with occasional rocky outcrops. The shore is mainly rocky (Dalradian metasediments) but some carbonate beaches and dunes are present. In sheltered lagoons a muddy shore is found. The sea water is normal marine with seasonal water temperature varying from 5 to 15° C. Salinity varies seasonally from 33.5 to 35%o (Lees et al., 1969). The normal marine environment is the result of mixing by tidal currents which, however, are not strong enough to transport the algal clasts (Buller, 1969). Study of the algal bed forms shows that the main hydraulic forces are the oscillatory currents produced by waves.",
author = "Daniel Bosence",
year = "1977",
doi = "10.1007/978-3-642-66516-5_29",
language = "English",
isbn = "978-3-642-66518-9",
pages = "270--278",
editor = "Fl{\"u}gel, {Erik }",
booktitle = "Fossil Algae",
publisher = "Springer Berlin / Heidelberg",

}

RIS

TY - GEN

T1 - Ecological Studies on two Carbonate Sediment-Producing Algae

AU - Bosence, Daniel

PY - 1977

Y1 - 1977

N2 - The bathymetIy and location of Mannin Bay are shown in Fig. 1. A submarine valley leads into the bay and up to a slope that levels off at about 8 m to form a platform with occasional rocky outcrops. The shore is mainly rocky (Dalradian metasediments) but some carbonate beaches and dunes are present. In sheltered lagoons a muddy shore is found. The sea water is normal marine with seasonal water temperature varying from 5 to 15° C. Salinity varies seasonally from 33.5 to 35%o (Lees et al., 1969). The normal marine environment is the result of mixing by tidal currents which, however, are not strong enough to transport the algal clasts (Buller, 1969). Study of the algal bed forms shows that the main hydraulic forces are the oscillatory currents produced by waves.

AB - The bathymetIy and location of Mannin Bay are shown in Fig. 1. A submarine valley leads into the bay and up to a slope that levels off at about 8 m to form a platform with occasional rocky outcrops. The shore is mainly rocky (Dalradian metasediments) but some carbonate beaches and dunes are present. In sheltered lagoons a muddy shore is found. The sea water is normal marine with seasonal water temperature varying from 5 to 15° C. Salinity varies seasonally from 33.5 to 35%o (Lees et al., 1969). The normal marine environment is the result of mixing by tidal currents which, however, are not strong enough to transport the algal clasts (Buller, 1969). Study of the algal bed forms shows that the main hydraulic forces are the oscillatory currents produced by waves.

U2 - 10.1007/978-3-642-66516-5_29

DO - 10.1007/978-3-642-66516-5_29

M3 - Conference contribution

SN - 978-3-642-66518-9

SP - 270

EP - 278

BT - Fossil Algae

A2 - Flügel, Erik

PB - Springer Berlin / Heidelberg

ER -