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Graptolites

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graptolites [′grap·tə‚līts]
(paleontology)

Graptolites 

(Graptolithina), a subphylum of extinct marine colonial animals of phylum Hemichordata.

Graptolites are known from the Cambrian to the Carboniferous periods; they were most common in the Ordovi-cian. Silurian, and lower Devonian periods. The skeletons of graptolites consisted of chitinous branches formed from little compartments in which the zooids lived. Graptolites were either benthic or planktonic. Planktonic graptolites had a swim bladder filled with gas released by the zooids as a product of their vital processes. There were two classes: Stereostolonata, with hard stolons and functionally varied compartments, and Graptoloidea, without stolons and with uniform compartments. Graptolites are of great importance as index fossils.

REFERENCE

Obut, A. M. “Tip Hemichordata (Gemikhordovye): Podtip Graptolithina (Graptolity).” In Osnovy paleontologii: Iglokozhie, gemikhordovye, pogonofory i shchetinkocheliustnve. Moscow, 1964.

A. M. OBUT



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Graptolites are generally very rare in carbonate rocks, yet, may be rather common in some marly intervals and help to improve stratigraphical correlations.
Distribution of graptoloids in the Ordovician carbonate rocks of the East Baltic area // Graptolites and Stratigraphy / D.
This level is close to the first appearance of Dicellograptus, however, graptolites are extremely rare or absent in the main part of the Uhaku Stage.
 
 
 
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