High palaeolatitude (Hodh, Mauritania) recovery of graptolite faunas after the Hirnantian (end Ordovician) extinction event

Author:

Underwood Charlie J.,Deynoux Max,Ghienne Jean-François

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference49 articles.

1. Graptolite biogeography: implications for palaeogeography and palaeoceanography. In: McKerrow, W.S., Scotese, C.R. (Eds.), Palaeozoic Palaeogeography and Biogeography;Berry;Geol. Soc. Mem.,1990

2. Beuf, S., Biju-Duval, B., De Charpal, O., Rognon, P., Gabriel, O., Bennacef, A., 1971. Les grès du Paleozoı̈que inférieur au Sahara. `Science et Technique du Pétrole', 18, Institut Français du Petrole, 464 pp.

3. Brenchley, P.J., 1984. Late Ordovician extinctions and their relationship to the Gondwana glaciation. In: Brenchley, P.J. (Ed.), Fossils and Climate. Wiley, Chichester, pp. 291–315.

4. Environmental changes close to the Ordovician–Silurian boundary. In: Cocks, L.R.M., Rickards, R.B. (Eds.), A Global Analysis of the Ordovician–Silurian Boundary;Brenchley;Bull. Br. Mus. Nat. Hist.,1988

5. Bathymetric and isotopic evidence for a short-lived Late Ordovician glaciation in a greenhouse period;Brenchley;Geology,1994

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