Summary:
Bryozoans contribute to marine carbonate sediments and rocks: (A) dried colony of Adeonellopsis species from Doubtful Sound, south-western New Zealand, ~25 cm across; (B) bryozoan thicket, 70 m water depth, Otago Shelf, south-eastern New Zealand, dominated by Cinctipora elegans; (C) bryozoan-dominated carbonate sediment from Otago Shelf, south-eastern New Zealand; (D) fossil bryozoan community from the late Permian Deep Bay Formation, Tasmania (photos: originally published in Smith 2009, reproduced with permission).
Type:
Figure
Sub Component:
Normal
Slug:
F56
Highwire: Type:
fragment
Highwire: Parent:
HighWire: Journal/Corpus Code:
csirobk
Highwire: pisa_id:
csirobk;9781486306800/1/other7/F56
Highwire: pisa_master:
csirobk;9781486306800/1/other7/F56
HighWire: Atom Path:
/csirobk/9781486306800/9781486306800/SEC7/F56.atom
Highwire: cpath:
/content/9781486306800/9781486306800/SEC7/F56
Image - Large:
Highwire: cpathalias:
/content/csirobk/9781486306800/9781486306800/SEC7/F56
Image - Medium:
Highwire: Variants:
expansion
Image - Small:
Highwire: State:
Released
Contributors:
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