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1. Where on the graptolite colony did the individual animals live? 2. How do graptolites differ from corals in living habit and skeleton? 3. How did the living habits of graptolites contribute to their being a good index fossil? Think about the three criteria for index fossils.

1. Where on the graptolite colony did the individual animals live? 2. How do graptolites differ from corals in living habit and skeleton? 3. How did the living habits of graptolites contribute to their being a good index fossil? Think about the three criteria for index fossils.

Concepts of Biology
Concepts of Biology
1st Edition
ISBN:9781938168116
Author:Samantha Fowler, Rebecca Roush, James Wise
Publisher:Samantha Fowler, Rebecca Roush, James Wise
Chapter15: Diversity Of Animals
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Problem 1ACQ: Figure 15.3 Which of the following statements is false? a. Eumetazoa have specialized tissues and...
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Kingdom Animalia, Phylum Chordata - Graptolites Graptolites (Figure 13) are a group of extinct, sessile and planktonic chordates. They have been confused as bryozoans or fossil plants. Graptolites are microscopic, colonial suspension feeders. Their colonies were composed of chitinous rather than calcareous material. They primarily fossilize by carbonization. Most graptolites are identified as belonging to one of two major categories. The first comprises the dendroid graptolites, which built complex, branching, fan-shaped rhabdosomes (colony). Some dendroid graptolites may have attached their bases to the sea floor. Others are believed to have suspended themselves from some floating objet by a threadlike tute known as the nema. The second category of graptolites is termed graptoloid. They were planktonic forms with distinctive patterns of thecae The graptoloid rhobdosome generally was composed of far fewer stipes than the rhabdosome of dendroids. In their evolution, they underwent a progressive reduction in the number of stipes. In general, Lower Ordovician beds contain graphtolites with more stipes than Middle and Upper Ordovician strata. Silurian graptolites characteristically are constructed of only one stipe. Graptolites are known from rocks of Cambrian through Mississippian age, but they are of greatest importance during the Ordovician and Silurian. Their worldwide distribution and rapid evolution have made them ideal index fossils of special importance in studies of Early Paleozoic strata. Fossil Lab Part 3: Echinoderms, Graptolites, Fossil Plants Theca T Dicellograptus 1X (Ord.) Didymograptus (Ord.) Phyllograptus (Ord.) 1X Enlarged view of a stipe with upper part sectioned Reconstruction of colony of Dictyo Diplograptus rd.-Si Monograptus (Sil.) Tetragraptus %X (Ord.) (Camb.-Miss.) re 13. Graptolites Figure 13. Graptolites Activity 1.2: Graptolites 1. Where on the graptolite colony did the individual animals live? 2. How do graptolites differ from corals in living habit and skeleton? 3. How did the living habits of graptolites contribute to their being a good index fossil? Think about the three criteria for index fossils.
Transcribed Image Text:Kingdom Animalia, Phylum Chordata - Graptolites Graptolites (Figure 13) are a group of extinct, sessile and planktonic chordates. They have been confused as bryozoans or fossil plants. Graptolites are microscopic, colonial suspension feeders. Their colonies were composed of chitinous rather than calcareous material. They primarily fossilize by carbonization. Most graptolites are identified as belonging to one of two major categories. The first comprises the dendroid graptolites, which built complex, branching, fan-shaped rhabdosomes (colony). Some dendroid graptolites may have attached their bases to the sea floor. Others are believed to have suspended themselves from some floating objet by a threadlike tute known as the nema. The second category of graptolites is termed graptoloid. They were planktonic forms with distinctive patterns of thecae The graptoloid rhobdosome generally was composed of far fewer stipes than the rhabdosome of dendroids. In their evolution, they underwent a progressive reduction in the number of stipes. In general, Lower Ordovician beds contain graphtolites with more stipes than Middle and Upper Ordovician strata. Silurian graptolites characteristically are constructed of only one stipe. Graptolites are known from rocks of Cambrian through Mississippian age, but they are of greatest importance during the Ordovician and Silurian. Their worldwide distribution and rapid evolution have made them ideal index fossils of special importance in studies of Early Paleozoic strata. Fossil Lab Part 3: Echinoderms, Graptolites, Fossil Plants Theca T Dicellograptus 1X (Ord.) Didymograptus (Ord.) Phyllograptus (Ord.) 1X Enlarged view of a stipe with upper part sectioned Reconstruction of colony of Dictyo Diplograptus rd.-Si Monograptus (Sil.) Tetragraptus %X (Ord.) (Camb.-Miss.) re 13. Graptolites Figure 13. Graptolites Activity 1.2: Graptolites 1. Where on the graptolite colony did the individual animals live? 2. How do graptolites differ from corals in living habit and skeleton? 3. How did the living habits of graptolites contribute to their being a good index fossil? Think about the three criteria for index fossils.
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