It is the second period of the Cainozoic era.

This can be explained by the recent deep subsidence in Cainozoic times.

Many of them still prefer the watery habitats which were so common early in the Cainozoic era.

The system of riverbeds and valleys were formed in the Cainozoic geological period.

The two continents were connected via Antarctica in the early Cainozoic era.

Rocks of the Cainozoic era have very large numbers of gastropod fossils in them.

It followed the Jurassic period, and was followed by the Cainozoic era.

New South Wales has 26,000 km of volcanic rocks from Cainozoic period.

The Cainozoic (Cenozoic) is the present geological era.

Various formations from Cainozoic to Jurassic age are economically significant freshwater aquifers.

After it was the Cainozoic era, (Palaeocene epoch).

The event marks the end of the Mesozoic era and the beginning of the Cainozoic era.

They were overtaken by the flowering plants, which first appeared in the Cretaceous, and became dominant in the Cainozoic era.

Most of the basin is covered by alluvium and lake deposits from the Cainozoic period, and this deposition continues till this day.

There, the coal bearing Carboniferous has been covered later on by Mesozoic and Cainozoic sediments, the thickness of which generally increases to the north.

(1914) "Cainozoic Fossils from Oamaru".

Thus the Cainozoic era is now divided into three periods, the Palaeogene, the Neogene and the Quaternary.

The UNESCO listing is for two separate areas where fossils from the Cainozoic period have been found.

The Eucla Basin is a Cainozoic basin consisting mostly of carbonate sediments and sedimentary rocks.

Or perhaps the increasingly unstable environments of the late Cainozoic associated with climatic deterioration caused a selection for eurytopic organisms well adapted to withstand environmental instability.

After the late Mesozoic breakup of Gondwana, South America spent most of the Cainozoic era as an island continent.

As the Cainozoic era began, the Hesse Depression emerged, part of the great rift fault from Scandinavia to the Mediterranean Sea.

The rock record contains representatives of each period of the Neoproterozoic, Paleozoic, Mesozoic and Cainozoic eras.

Fieldwork has concentrated on mineralisation in greenstones of the Jurassic Alao division and sediments cut by Cainozoic intrusives.

Cainozoic sand dune systems are locally being mined for mineral sands, mainly rutile (a source of titanium ) and zircon, by Iluka Resources and other companies.

During the Cainozoic the continents moved into their present positions.

It is the second period of the Cainozoic era.

Many of them still prefer the watery habitats which were so common early in the Cainozoic era.

Ants became dominant after adaptive radiation at the beginning of the Cainozoic.

Flowering plants and birds also evolved substantially in the Cainozoic.

The system of riverbeds and valleys were formed in the Cainozoic geological period.

The Cainozoic is the age of mammals.

They were dominant land carnivores in South America through much of the Cainozoic.

As a result, the ecological landscape of the Cainozoic has become quite different from the Mesozoic.

They were the dominant predators in South America during the Cainozoic, from 62-2 million years ago.

Rocks of the Cainozoic era have very large numbers of gastropod fossils in them.

It followed the Jurassic period, and was followed by the Cainozoic era.

That is why the last period of the Cainozoic is called the Quarternary.

The Cainozoic (Cenozoic) is the present geological era.

On land, the Cainozoic is the era of mammals, and of birds and flowering plants.

After it was the Cainozoic era, (Palaeocene epoch).

The Cainozoic is spilt down into three periods, and the periods are split into stages.

They lived in the late Paleocene and early Eocene epochs of the Cainozoic.

During the Cainozoic, mammals diverged from a few small, simple, generalized forms into a diverse collection of terrestrial, marine, and flying animals.

The event marks the end of the Mesozoic era and the beginning of the Cainozoic era.

Previously, what is now the Cainozoic was divided into two periods, the Tertiary and the Quaternary.

The Miocene is the first epoch of the Neogene period of the Cainozoic.

The grasslands which feature in many of his paintings did not appear until the Cainozoic, and ceratopsians are known to have been gregarious animals.

In fact, since volcanoes have not been very active in the Cainozoic, the supply of CO has been run down somewhat.

They were overtaken by the flowering plants, which first appeared in the Cretaceous, and became dominant in the Cainozoic era.