Batrachospermum Occurrence:- (1) Batrachospermum is fresh water alga. (2) It is found in clear, cool, and running streams. (3) Deepwater plants are dark violet or reddish in color. But the shallow-water species are olive green. (4) The intensity of light changes the color of pigments. (5) The thallus is attached to the substratum. Vegetative structure (1) The thallus of an adult plant is soft, thick, filamentous. (2) It is freely branched and gelatinous. (3) The central axis is made up of a single row of large cells. Whorls of branches of limited growth are developed on this axis. (4) These branches are filamentous and dichotomously arranged. (5) The main axis is corticated. It consists of a row of elongated cylindrical cells. (6) It is differentiated into nodes and internodes. (7) There are two types of branches that arise from the nodes: Branches of limited growth Branches of unlimited growth Batra
Geological Time Table
Meaning of time Scale:
Geological time scale may be a table showing the
sequence of earth science periods within the history of earth.
Geological Time Table |
It additionally
shows the lengths of your time totally different earth science periods square
measure assumed to own occupied it's measured in a lot of years.
it's been made
by learning rock strata, wherever these are exposed by excavations or mining or
wherever rivers have cut deeply into the earth’s crust.
Scientists have established that lower the rock
layer the older it's and therefore the additional ancient square measure the
fossils it contains.
With a data of rates of abrasion and deposition, the
intervals occupied by totally different periods will be calculable roughly by
measure the relative thicknesses of the rock strata.
By the technique of radiometric geological dating
(i.e. by measure the rates of decay of radioactive materials within the rocks) additional
correct geological dating will currently be provided.
within the table of time
scale, the results of all such works square measure summarized.
Table additionally shows the kinds of plants that
are found throughout totally different periods. the planet has been calculable
to be regarding 4600 million years previous.
Life is believed to own originated
regarding 3000-3500 million years past on the planet.
Major Divisions and Subdivisions of time Scale:
Geological time has been divided into some major
divisions known as eras .
every era has been divided into
periods, that square measure then divided into epochs.
Different periods square measure recognized in the
main on the premise of:
(i) Changes in composition of fossils, and
(ii) The incidence of major earth science events
(e.g. episodes of mountain building or major changes in level of seas).
The earliest era is eon, that began regarding 4600
million years past. it's few fossils.
plethoric fossils are rumored within the
succeeding eras viz. Palaeozoic, Mesozoic and Cenozoic era.
Geological Eras:
A geological time may be a terribly division of
time, lasting tens of a lot of years.
Its starting and finish square measure
recognized by major changes in layers of rocks and fossils within the earth.
As
mentioned higher than, the earliest era is eon It began regarding 4600 a lot of
years past.
Its period has been 4030 a lot of years.
Palaeozoic era began regarding 570 a lot of years
past. Mesozoic era began regarding 225 a lot of years past.
Cenozoic era is
that the most up-to-date era. It began regarding sixty five million years past,
when the Mesozoic era, and it's still continued.
Eras square measure divided into periods and epochs.
Geological Periods:
A geological time is split additional into many
subdivisions known as periods .
thus a amount may be a
major subdivision of a geological time.
Major periods of Palaeozoic era square
measure Permian, Carboniferous, Devonian, Silurian, geological period and
Cambrian.
Mesozoic era is split into 3 periods viz. Cretaceous, geological
period and period.
Similarly Cenozoic era is split into 2 periods viz.
Quarternary and Tertiary.
The oldest best-known amount of time scale is
Cambrian (began regarding 570 million years ago) whereas the foremost recent
amount is Quaternary (began regarding two.5 million years ago).
Periods square measure divided into epochs.
Geological Epochs:
A subdivision of a geological time is named a earth
science epoch.
Recent, Pleistocene, Pliocene, Miocene, Oligocene, Eocene and
epoch square measure the epochs of Periods Quaternary and Tertiary of Cenozoic
era .
Major Events of time Scale:
1.. Bryophytes evolved on the planet throughout the
Silurian of Paleozoic era (i.e. between 395 to 430 million years ago) and
square measure still extant.
2. Pteridophytes evolved someday in period,
dominated the planet throughout Carboniferous and square measure still extant.
3. Gymnosperms evolved someday at the top of
Triassic period (i.e. regarding 225 million years ago) Mesozoic era, dominated
the planet someday throughout Palaeocene epoch (i.e. regarding sixty five
million years ago) and square measure still extant.
4. Angiosperms evolved throughout Jurassic of
Mesozoic era and square measure currently dominating the planet within the
Holocene epoch of period of Cenozoic era.
A outline of time scale is given in Table
Geological Time Table |
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