Page 29 - Atlas of Creation Volume 1
P. 29

Harun Yahya



























                                                                                   The skin and scales of this fish from the Triassic Period
                                                                                   (250 to 203 million years ago) are fossilized with all
                                                                                   their details intact. This sample reveals that fish had
                                                                                   the same scale structure 250 million years ago.


                  The complete fossilization of a living thing's soft parts, even including fur, feathers or skin, is
             encountered only rarely. Remains of some soft-tissued life forms of the Precambrian Period (dating back
             4.6 billion to 543 million years ago) have been very well preserved. There are also soft-tissue remains

             that permit internal structures from the Cambrian Period (543 to 490 million years ago), to be examined
             in addition to hard-tissue remains of living things right down to the present day. Fossil remains of
             animal fur and hairs preserved in amber, and fossil remains dating back 150 million years are other

             examples that permit detailed investigation. Mammoths compacted in Siberian ice packs or insects and
             reptiles trapped in amber in Baltic forests have also become fossilized together with their soft-tissue
             structures.
                  Fossils can vary considerably in terms of size, according to the type of organism preserved. Very
             different fossils have been obtained from the fossilized microorganisms to giant fossils from animals that

             lived together as groups or herds, in a communal lifestyle. One of the most striking examples of such
             giant fossils is the sponge reef in Italy. Resembling a giant hill, this reef is composed of 145-million-year-
             old limestone sponges that developed at the bottom of the ancient Sea of Tethys, and later rose up as the

             result of the movement of tectonic plates. It contains specimens of the life forms living in sponge reefs
             during the Triassic Period. The Burgess Shale in Canada and Chengjiang in China are among the largest
             fossil beds containing thousands of
             fossils from the Cambrian Period.
             The amber beds in the Dominican

             Republic and along the western
             shores of the Baltic Sea are other
             major sources of fossil insects. The

             Green River fossil beds in the U.S.
             state of Wyoming, the White River
             fossil beds in Central America, the
             Eichstatt beds in Germany and the
             Hajoula fossil beds in Lebanon are

             other examples that can be cited.



                   THE GREATEST SPONGE REEF
                                           ON EARTH

             This sponge reef of 145 million years old is a
           trace of the Tethys Ocean floor. The sponges of
             our day are no different from those that make
              up the hill. These sponges make it clear that
                  they have not undergone any evolution.




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