Pelagic environments.
Pelagic sediments are chiefly composed of the microscopic skeletal remains of planktonic animals and plants, variously diluted by non-biogenic components. Such sediments may be carbonate-rich, silica-rich or clay-rich and they change in facies when traced laterally across the ocean and vertically th...
Main Author: | Jenkyns, H |
---|---|
Other Authors: | Reading, H |
Format: | Journal article |
Language: | English |
Published: |
Blackwell Scientific
1986
|
Similar Items
-
PELAGIC OOLITES FROM TETHYAN JURASSIC
by: Jenkyns, H
Published: (1972) -
BLACK SHALES AND CARBON ISOTOPES IN PELAGIC SEDIMENTS FROM THE TETHYAN LOWER JURASSIC
by: Jenkyns, H, et al.
Published: (1986) -
Ancient oceans and continental margins of the Alpine-Mediterranean Tethys: deciphering clues from Mesozoic pelagic sediments and ophiolites
by: Bernoulli, D, et al.
Published: (2009) -
Biotic and geochemical response to anoxic events: the Aptian pelagic succession of the Gargano Promontory (southern Italy)
by: Luciani, V, et al.
Published: (2001) -
Biotic and geochemical response to anoxic events: the Aptian pelagic succession of the Gargano Promontory (southern Italy)
by: Luciani, V, et al.
Published: (2001)