Andere Kunden interessierten sich auch für
![Paleoclimatological Implications of Fossil Tortoise Bones]( "Paleoclimatological Implications of Fossil Tortoise Bones")
Paleoclimatological Implications of Fossil Tortoise Bones35,99 €![Guide to the Collection of Fossil Fishes in the Department of Geology and Paleontology]( "Guide to the Collection of Fossil Fishes in the Department of Geology and Paleontology")
Guide to the Collection of Fossil Fishes in the Department of Geology and Paleontology33,99 €![Fossil Record 2]( "Fossil Record 2")
Fossil Record 2251,99 €![Fossil Plants]( "Fossil Plants")
Fossil Plants49,99 €![The Lost World of Fossil Lake]( "The Lost World of Fossil Lake")
The Lost World of Fossil Lake43,99 €![Catalogue of the Fossil Bryozoa in the Department of Geology: British Museum (Nautral History) the Jurassic Bryozoa]( "Catalogue of the Fossil Bryozoa in the Department of Geology: British Museum (Nautral History) the Jurassic Bryozoa")
Catalogue of the Fossil Bryozoa in the Department of Geology: British Museum (Nautral History) the Jurassic Bryozoa38,99 €![A Fossil History of Southern African Land Mammals]( "A Fossil History of Southern African Land Mammals")
A Fossil History of Southern African Land Mammals122,99 €
The Cambrian Period (542 to 488 Ma) marks the
beginning of an abundant fossil record, and the
Burgess Shale Biota was the first fully described
fossil assemblage that contains a relatively
complete picture of a benthic Cambrian community.
More Burgess Shale-type (BST) fossil assemblages
have been discovered since then and are ready to be
utilized to test hypotheses about the ecology of the
Cambrian explosion, which is the most important
event in the evolution of metazoans. This book
focuses on the Kaili Biota
(http://hdl.handle.net/1811/24227), an important
deposit bridging the stratigraphic gap between
Chengjiang Biota and Burgess Shale Biota. It allows
us to gain a more complete understanding of the
Cambrian life through the window of BST deposits.
The book is divided into four parts. Part 1 includes
stratigraphic background of Kaili Formation. Part 2
contains discussions on taphonomy. Part 3 provides
new observation for Cambrian paleoecology, including
animal-substrate relations, spawning habits, teiring
community, and faunal succession. Part 4 presents
hypotheses on arthropod, echinoderm evolution, and
the evolution of biosphere.
beginning of an abundant fossil record, and the
Burgess Shale Biota was the first fully described
fossil assemblage that contains a relatively
complete picture of a benthic Cambrian community.
More Burgess Shale-type (BST) fossil assemblages
have been discovered since then and are ready to be
utilized to test hypotheses about the ecology of the
Cambrian explosion, which is the most important
event in the evolution of metazoans. This book
focuses on the Kaili Biota
(http://hdl.handle.net/1811/24227), an important
deposit bridging the stratigraphic gap between
Chengjiang Biota and Burgess Shale Biota. It allows
us to gain a more complete understanding of the
Cambrian life through the window of BST deposits.
The book is divided into four parts. Part 1 includes
stratigraphic background of Kaili Formation. Part 2
contains discussions on taphonomy. Part 3 provides
new observation for Cambrian paleoecology, including
animal-substrate relations, spawning habits, teiring
community, and faunal succession. Part 4 presents
hypotheses on arthropod, echinoderm evolution, and
the evolution of biosphere.