Сбор, диагностика и обработка палеонтологических материалов при проведении учебных геологических практик. Учебное пособие на модульной основе
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c)breathing pattern;
d)method of reproduction.
187.The sizes of shells of molluscs of the Gastropods class vary within:
a) from 1 m to 2 m; b) 0.1 mm to 30 cm; c) 0.01 mm to 0.1 mm; d) 0.1 mm to 0.2 mm.
188.Can gastropod shell size change under changing conditions?
a) yes; b) no;
c) sometimes; d) always.
189.What is the purpose of the radula of gastropods:
a)for reproduction;
b)for movement;
c)for grinding and rubbing food;
d)for smelling.
190.The radula of molluscs has the appearance of: a) convex grater;
b) proboscis;
c) corneous plate; d) rhizopod.
191.The teeth of the radula are large, with numerous channels filled with poison, dangerous even for humans. What mollusc of the gastropod class are we talking about?
a) Viviparus M; b) Rapana Sch; c) Conus L;
d) Helix.
192.How do predators of the gastropod class (Rapana Schumaher) destroy the shell of their prey?
a) by drilling;
b) by sulfuric acid;
c) open it with muscles;
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d)break it on the substrate.
193.What were the shells of Monetaria accusys (Cowrie) gastropods used for in North America before 1786?
a) as money;
b) as a building material; c) as a medicine;
d) as an ornamental material.
6.6.11.Bivalves class. Classis Bivalvia
194.What rocks make up bivalves?
a)limestones;
b)gaizes;
c)chalk;
d)tripolith.
195.According to the way of feeding, mollusks of Bivalvia class are:
a) filterers; b) predators; c) scavengers; d) herbivores.
196.In bivalve mollusks, the radula is:
a) present;
b)present in some species;
c)missing;
d)reduced.
197.Systematics of bivalves is based on: a) shell structure;
b) the structure of the dental apparatus; c) shell shape;
d) muscle structure.
198.Dental apparatus of bivalve mollusks is used for: a) drilling and digging;
b) grinding and rubbing food;
c) tight articulation of the valves; d) movement.
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199.The starting order for all bivalves were: a) taxodonts;
b) pachyodonts; c) schizodonts; d) toothless.
200.Time of existence of representatives of the Bivalvia
class:
a) the Cambrian – the Silurian; b) the Ordovician – the Neogene; c) the Cambrian – now;
d) the Triassic – now.
6.6.12.Cephalopods. Classis Cephalopoda
201.What sharply distinguishes cephalopods from others? a) dimensions;
b) developed nervous system; c) method of reproduction; d) way of feeding.
202.Skeleton of cephalopods:
a)internal;
b)external;
c)missing;
d)scattered.
203.Most modern cephalopods have shells: a) internal;
b) external; c) missing; d) scattered.
204.Modern cephalopods with an external shell are represented by the genus:
a) Nipponites;
b) Macrocephalites; c) Nautilus;
d) Orthoceras.
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205.According to the way of feeding, cephalopods are: a) predators;
b) filterers; c) scavengers;
d) herbivorous.
206.The soft body of a cephalopod with an external shell is
located:
a) completely in the sink;
b) occupies ½ of the last whorl; c) occupies ½ of all whorls;
d) occupies ½ of the first whorl.
207.How many hearts do cephalopods have?
a)one;
b)three;
c)five;
d)two.
208.The skeleton of modern cephalopods – octopuses: a) external;
b) internal; c) missing;
d) fragmented.
209.The most fractional divisions of the stratigraphic scale – eons were distinguished by order:
a) ammonoids; b) bactritoids; c) chitoceratids; d) gonyatids.
210.Scientific name for “devil’s fingers”:
a)trilobites;
b)rhincholiths;
c)stalagmites;
d)belemnites.
211. What is the main significance of cephalopods in geology?
a)rock-forming role;
b)paleogeographical significance;
c)stratigraphic significance;
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d) relief-forming role.
212.Time of existence of cephalopods: a) the Cambrian – now;
b) the Cambrian – the Neogene; c) the Ordovician – now;
d) the Silurian – the Paleogene.
6.6.13.Bryozoans type. Phylum Bryozoa
213.Colonies of bryozoans consist of zooids, which are: a) individuals performing different functions;
b) elements of their skeleton; c) skeletal forms;
d) individuals performing only the function of nutrition.
214.Time of existence of bryozoans:
a)the Triassic – the Jurassic;
b)the Ordovician – now;
c)the Cambrian – now;
d)the Cambrian – the Jurassic.
215.Bryozoans of the class ectoproctans are not preserved in the fossil state due to the fact that they:
a) are small;
b) live at great depths;
c) do not have a mineral skeleton; d) are single forms.
216.What rocks form bryozoans?
a)clay;
b)marl;
c)travertine;
d)limestone.
6.6.14.Brachiopods type. Phylum Brachiopoda
217. A distinctive feature of brachiopods is:
a) the presence of an axis of symmetry passing through the tops of the valves;
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b)large sizes;
c)shell shape;
d)way of breathing.
218.Why did many researchers combine bryozoans and brachiopods into one type?
a) similar dimensions;
b) the presence of a lophophore; c) according to the way of feeding;
d) according to the composition of the skeleton.
219.Spiral folded arms with cilia in brachiopods perform the function of:
a) protection; b) attack;
c) nutrition; d) movement.
220.According to the way of feeding brachiopods are:
a)predators;
b)scavengers;
c)filterers;
d)herbivores.
221.According to the shape and structure of the skeleton, brachiopods are the closest:
a) to bryozoans; b) to bivalves;
c) to cephalopods; d) to gastropods.
222.The basis for the division of brachiopods into classes is: a) shell size and shape;
b) habitat depth;
c) the structure of the hinge and the brachidium; d) shell composition and sculpture.
223.The shell of brachiopods most often has the following composition:
a) phosphate; b) calcareous;
c) chitinous-phosphate;
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d) chitinous.
224.Gigantoproductus is: a) bivalve mollusk;
b) cephalopod; c) brachiopod; d) gastropod.
225.Time of existence of brachiopods: a) the Cambrian – now;
b) the Cambrian -the Ordovician; c) the Silurian – now;
d) the Permian – the Paleogene.
226.What rocks are formed by skeletal forms of brachiopods? a) granites;
b) limestones; c) dolomites; d) tripolith.
227.The ratio of extinct and modern species of brachiopods indicates that they are now:
a) flowering;
b) experience decline;
c) their number has not changed; d) extinct.
6.6.15.Echinoderms type. Phylum Echinodermata.
228.A distinctive feature of animals of the echinoderms
type is:
a) skeletal composition; b) ambulacral system; c) five-beam symmetry; d) way of feeding.
229.Skeleton of modern echinoderms:
a)external;
b)internal;
c)missing;
d)various.
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230.The composition of the skeleton of echinoderms: a) calcareous;
b) siliceous; c) chitinous; d) phosphate.
231.Ambulacral system of echinoderms is:
a)sculpture of a skeleton;
b)tubular system;
c)the digestive organ;
d)reproductive organ.
232.Why are echinoderms numerous only in the northern seas of Russia (in the Black they are relics, in the Baltic there only one species, in the Caspian – none)?
a) became extinct; b) are stenohaline; c) are stenobathic;
d) are stenothermous.
233.Why are starfish not preserved as fossils?
a)their skeleton has a specific mineral composition;
b)their skeleton is not intact;
c)they do not have a skeleton;
d)they have a limited distribution area.
234.Representatives of what class of echinoderms still exist? a) Cystoidea (cystoids);
b) Blastoidea (blastoids); c) Crinoidea (crinoids); d) Thecoidea (thecoids).
235.Which representatives of echinoderms show a change in the type of symmetry from five-beam to two-sided?
a) sea lilies; b) sea urchins; c) starfish;
d) blastoids.
236.The division of sea urchins into true and false is based
on:
a) the position of the mouth and anus;
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b)skeletal composition;
c)dimensions;
d)way of feeding.
237.Time of existence of sea urchins: a) O – now;
b) O – R; c) P – T; d) O – T.
238.Animals that existed in the time interval are considered ancient sea urchins:
a) O – T; b) O – R; c) P – T; d) O – S.
239.Sea urchins are of great importance as:
a)rock formers;
b)reef builders;
c)environmental indicators;
d)guiding fauna of the Cretaceous sediments. 240. What is the “Aristotle’s lantern”?
a)limb of crustaceans;
b)trilobite eye;
c)jaw apparatus of sea urchins;
d)the shape of the fossils.
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7. THEMATIC DICTIONARY
Archistratigraphic group of fossils – organisms characterized by the rapidity of evolution, wide geographical distribution and burial in rocks of various material composition.
Biocoenosis is a community of living organisms.
Involute shell – the last whorl of a spirally curled shell overlaps the penultimate one.
Ichnofossils are traces of the vital activity of fossil organisms. Coprofossils are the waste products of fossil organisms.
Correlation is a comparison of rock sections in order to determine the age and identify the stratotype.
Lobed line is a septal line, according to the structure and configuration of which the cephalopods of ectocochlians are divided into orders.
Guide fossil method – determination of the age of sediments from identical guide fossils.
Ontogeny is the individual development of an individual. Oryctocoenosis is a community of fossil organisms.
Paleogeographic reconstructions are the restoration of the environments of past geological epochs.
Radula is an organism’s adaptation for grinding and rubbing food – a kind of convex grater located in the oral cavity and pharynx.
Fossil guide forms are organisms that have a wide geographic distribution and a small vertical distribution.
Rostrum – the main part of the internal skeleton of endocochlian cephalopods – massive, conical or cylindrical.
Stenohaline organisms – living in a strictly defined environment in terms of salinity.
Thanatocenosis is a community of dead organisms. Taphocenosis is a community of buried organisms.
Phylogeny is the historical development of a group of organisms.
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