Nummulites ( lat. Nummulites , from lat. Nummulus - coin) - a genus of unicellular organisms of the Foraminifera order. The remains of nummulite are known from Upper Cretaceous and Paleogene sediments of the tropics and subtropics of Europe, Asia, Africa and America.
| Nummulite |
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| Superfamily : | Nummulitoidea |
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| International Scientific Name |
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Nummulites Lamarck , 1801 |
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Content
A calcareous, thin-pore-impregnated shell, spirally symmetrically curled and shaped like a rounded plate or biconvex (less often to spherical); the number of revolutions is very large, the height, as well as their width increases very gradually; the number of chambers is very large, the last revolutions are mostly closed in the form of a ring surrounding the entire shell (the transition from the spiral arrangement of the chambers to the circular one), the last revolutions completely enclose the previous ones, the hole is simple, the system of channels in the walls of the sink and its partitions is very well developed. In the subgenus Numullina, the cavities of the chambers continue along the sides to the shell axis, and only the last turn of it is usually visible from the outside; the partitions are radial, in various ways curved or crimped, sometimes branched and dividing the sides of the chambers into small chambers; this includes only one modern look and a number of minerals. They are close to nummulites and belong to the same family (Nummulitinae) and subfamily (Nummulitidae) from the genera Polystomella , Operculina , Cyclammina , which also have modern representatives.
The steep slope of kuesta in the Crimea consists of a stratum of durable mshankovy and nummulite limestone lying on top of it.
Characteristic of the Eocene sediments of the oceanic type. These include large calves, calcareous, circular or lenticular, ranging in size from the size of a pinhead to a silver ruble. The shell is composed of many spiral-increasing turns, divided by transverse partitions into numerous interconnected chambers. Nummulites appear already in the Carboniferous system and exist to this day, but the greatest development reached in the age of the Eocene . Shucks nummulites overwhelmed sometimes huge column nummulitovyh limestone widely distributed over the earth's surface to reveal even the snowy peaks of the Pyrenees , the Alps , the Carpathians and the Himalayas , certainly suggesting that in comparatively recent geological times, these mountains did not exist, and in their place was overflowing huge Eocene ocean , at the bottom of which myriad buried nummulites and other organisms modern to them.
According to the World Register of Marine Species , as of July 2016, the genus includes 6 species, 2 of which became extinct [1] :
- Nummulites barroni Chapman, 1900
- † Nummulites gizehensis (Forsskål, 1775 in Niebuhr, 1775)
- Nummulites hyalinus Hofker, 1956
- † Nummulites laevigata (Bruguiere, 1792)
- Nummulites lenticulus Blainville, 1825
- Nummulites niasi Verbeek, 1896