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Nematomorpha Fossil*Maotianshania*Chengjiang biota*
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Nematomorpha Fossil*Maotianshania*Chengjiang biota*
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C hengjiang biota E arly Cambrian(~525 million years ago) We will ship your items within 24 hours upon payment received. We always ship via Global mail, It usually takes 2 to 5 weeks for your items to arrive. you may choose USPS Express service too. It usually takes 4 to 10 days for your items to arrive. For customers living anyw in the U.S.,the shipping and handling charge for this item is $11 .For destinations outside the USA please send us an e-mail. Import duties, taxes and charges are not included in the item price or shipping charges. These charges are the buyer’s responsibility.Please check with your country’s customs office to determine what these additional costs will be prior to bidding/buying. •Payment We accept PAYPAL •Return Policy w e offer a 7 day (from day item arrives in your hands) no hassle return for items you are unsatisfied with. Just inform us, by email within 7 days, and then upon receipt of the item in its original condition, we will refund you the price of the item minus shipping costs to and from. We are only interested in spreading satisfaction. • Combined Shipping method weight(g) of all items in 7 days shipping charge Global insurance is required M atrix size:85mmx62mm ----------------------------------------------------------------------------------------- The first unequivocal evidence of multicellular organisms in the fossil record comes from the Ediacaran faunas, named for the Ediacara Hills of Australia w they were first discovered. The earliest of these come from the Vendian period of the Proterozoic, some 565 million years ago. These were soft-bodied organisms, some of which had a "quilted" appearance, which are entirely preserved as impression or compression fossils. The Cambrian fossils of Chengjiang in Yunnan Province, China (~525 million years ago), and the somewhat younger Burgess Shale Fauna of Field, British Columbia (~515 million years ago) afford a magnificent diversity of organisms that represent all the major phyla in existence today, and some organisms that are as yet of enigmatic origin. This rapid change, in a mere blink of an eye in geological terms, is what is called the "Cambrian Explosion". One postulated reason for this change is the fact that the rising concentration of oxygen, a result of bacterial and plant photosynthesis over the eons, allowed for organisms to be larger in size and lead a more active lifestyle. Larger organisms more easily leave traces in the fossil record. This same time period saw the evolution of hard body parts, thought to be a consequence of the selection pressures brought about by predation. Other mechanisms are theorized to have contributed to the Cambrian explosion, such as a cooling of the Earth and an increase in calcium in marine environments. While the Cambrian Explosion may always be shrouded in some mystery, it is clear that it represents a profound period of life on Earth, w the basic body plans of the major animal phyla were establ...
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