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from the
Ordovician near Caney Springs, Tennessee are good zone fossils. A zone fossil must have a short time span but a common animal of the time. Graptolites became
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were connected by stalklike structures to a central region.
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361:Paleozoic life of the Northwest Territories
356:Paleozoic life of Newfoundland and Labrador
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164:"Clonograptus | graptolite genus"
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227:89b25c74-a006-4f35-95dd-df836af1922f
299:. You can help Knowledge (XXG) by
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16:Genus of marine worm-like animals
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351:Paleozoic life of New Brunswick
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58:Scientific classification
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40:Graptolites, like this
295:-related article is a
248:Paleobiology Database
366:Hemichordate stubs
126:. Groups of these
48:at the end of the
346:Graptolite genera
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180:Taxon identifiers
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42:Amplexograptus
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301:expanding it
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188:Clonograptus
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140:zone fossils
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81:Hemichordata
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124:graptolites
340:Categories
150:References
144:Ordovician
64:Kingdom:
203:Q5135059
197:Wikidata
76:Phylum:
69:Animalia
50:Devonian
240:3660004
217:1413866
146:rocks.
132:Species
128:animals
100:Genus:
88:Class:
46:extinct
266:411409
224:NZOR:
291:This
261:WoRMS
253:33548
212:IRMNG
120:genus
118:is a
297:stub
138:are
134:of
122:of
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