Graticula: Difference between revisions
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The Graticulaceae closely resemble the Cretaceous [[Solenoporaceae]], and are only really differentiated by their stratigraphic position.<ref name=Brooke1998/> |
The Graticulaceae closely resemble the Cretaceous [[Solenoporaceae]], and are only really differentiated by their stratigraphic position.<ref name=Brooke1998/> |
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''Graticula'' mineralized with calcite.<ref name="Cozar2006">{{cite |
''Graticula'' mineralized with calcite.<ref name="Cozar2006">{{cite journal|journal=[[Sedimentary Geology]]|doi=10.1016/j.geobios.2005.09.002}}</ref> |
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==References== |
==References== |
Revision as of 21:05, 2 September 2015
Graticula Temporal range:
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Scientific classification | |
(unranked): | Archaeplastida |
Division: | Rhodophyta |
Class: | Florideophyceae |
Stem group: | Corallinales |
Family: | Graticulaceae |
Genus: | Graticula |
Species | |
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Synonyms | |
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Craticula, formerly incorrectly named Graticula,[1] is a genus of Palaeozoic coralline alga.[2] They form the framework of reef rocks in the Silurian of Gotland, from the Högklint, Slite and Halla groups.[3]
The Graticulaceae closely resemble the Cretaceous Solenoporaceae, and are only really differentiated by their stratigraphic position.[2]
Graticula mineralized with calcite.[4]
References
- ^ Brooke, C.; Riding, R. (2000). "Graticula and its derivatives, replacement name for the alga Craticula Brooke". Lethaia. 33 (2): 82–82. doi:10.1080/00241160050150203Template:Inconsistent citations
{{cite journal}}
: CS1 maint: postscript (link) - ^ a b Brooke, C.; Riding, R. (1998). "Ordovician and Silurian coralline red algae". Lethaia. 31 (3): 185–195. doi:10.1111/j.1502-3931.1998.tb00506.xTemplate:Inconsistent citations
{{cite journal}}
: CS1 maint: postscript (link) - ^ Attention: This template ({{cite doi}}) is deprecated. To cite the publication identified by doi:10.1016/j.sedgeo.2006.04.009, please use {{cite journal}} (if it was published in a bona fide academic journal, otherwise {{cite report}} with
|doi=10.1016/j.sedgeo.2006.04.009
instead. - ^ Sedimentary Geology. doi:10.1016/j.geobios.2005.09.002.
{{cite journal}}
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