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THE MEDITERRANEAN LOWER CRETACEOUS

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Table 2<br />

The Early Cretaceous Time Scale<br />

Epoch Age<br />

Late Cretaceous Cenomanian .<br />

retaceous<br />

U<br />

Early<br />

Albian<br />

Aptian<br />

Barremian<br />

Hauterivian<br />

Valanginian<br />

Berriasian<br />

Late Jurassic Tithonian<br />

after Casey,<br />

1964<br />

б<br />

-100-<br />

6<br />

-106-<br />

6<br />

-112-<br />

6<br />

118-<br />

6<br />

124-<br />

6<br />

130-<br />

6<br />

136-<br />

Boundary and duration in m. y.<br />

after Van H i n t e,<br />

1976<br />

8<br />

-100-<br />

-108-<br />

7<br />

-115-<br />

6<br />

-121-<br />

5<br />

-126-<br />

5<br />

-131^<br />

К: Alb<br />

KA Pt<br />

К<br />

4 KBer<br />

-135<br />

after H a r 1 a n d<br />

et al., 1982<br />

According to the different authors, the duration of the Early Cretaceous is<br />

between 36 and 46 million years. The average duration of the Early Cretaceous is<br />

about 6 million years, the maximum duration being 15.5 million years (for the Albian<br />

Age).<br />

Irrespective of some difficulties connected with the application of radiometric<br />

methods, they define along general lines the time interval of the Early Cretaceous<br />

and provide data for a number of interpretations. For example, according to the<br />

studies of P о 1 e v a y a et al. (По л е в а я et al., 1960), in the section of the<br />

Lower Cretaceous along the Bolshaya Laba river the glauconite from two samples<br />

(samples 2603 and VIII) is divided by a marl formation about 300 m thick. These<br />

samples differ by 3 million years in age, which suggests sedimentation rate of about<br />

0.1 mm/year.<br />

12

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