cameral

This became known as Cameral science(the new modern Public administration).

A cameral measurement instrument of the wealth of the farm.

Cameral deposits are normal which develop apically and more ventrally.

As with most actinocerids, cameral deposits are common.

Cameral deposits are also more extensive in the ventral half of the pragmocone.

Thick cameral deposits develop ventrally, but are only thin dorsally (Sweet, 1964).

Cameral deposits are common and concentrated ventrally.

No cameral deposits are known.

Cameral deposits are well developed.

Some Palaeozoic nautiloid genera, especially those with long, straight shells, are distinguished by cameral deposits.

Apical chambers in adults have cameral deposits.

Endosiphuncular or cameral deposits are unknown.

There is a tendency for the chambers to develop cameral deposits, which were used as ballast to balance the long gas-filled shell.

The shells are formed of aragonite, although the cameral deposits may consist of primary calcite.

Connecting rings are thin, septal necks orthochoantic, and without known endosiphuncular or cameral deposits.

Cameral deposits are known from the dorsal side, the ventral side of the type specimen lost from erosion.

Chambers are short and contain cameral deposits which are more concentrated apically and ventrally.

Cameral deposits are confined apically and, where observed, siphonal deposits are simple annuli.

But later research on their internal structures, such as the siphuncle, cameral deposits, and others, showed that these actually belong to a number of groups, even different orders.

Parietal deposits within the siphuncle from endocones in advanced genera and cameral deposits are found in some.

Cameral deposits, which are generally well developed, are formed along the front and backside of the septa, referred to as episeptal and hyposeptal.

The discovery of cameral desposits in the phragmocones of Belemnotheutis in 1952 made it clear that they were capable of controlling buoyancy.

Cameral depostis are well developed on the convex side, toward the apex while only thin on the concave side, making the curvature exogastric.

Cameral deposits are well developed and are thick,almost filling the ventral portion of the more apical chambers but also found in dorsal chambers as well.

At this time, Russia was experimenting with the cameral system, meaning that every student graduating in law and economics from a Russian university had to take two years of chemistry.