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Cenozoic
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Virtual Museum Tour
360
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Virtual Tour
Dynamic Earth
Earth Evolution
Reconstruct Geological History
The present is the key to the past
Relative Age Introduction
Index Fossil
Absolute Age
Solar System Formation
Solar System Formation
Meteorites
Our Unique Earth
Habitable Earth
Archean
Origin of the Earth's Crust
Origin of the Continents
The Oldest Rock from China
The Earliest Atmosphere & Hydrosphere
Direct Evidence for an early Hydrosphere
O
2
- Free Atmosphere - Banded Iron formation
The Earliest Life on Earth
Indirect Fossil Evidence
Direct Fossil Evidence
Proterozoic
The Onset of Plate Tectonics
Extensive Carbonate Platforms
Stromatolites
Dawn of Multicellular Life
Early Paleozoic
Early Paleozoic Sea
Early Paleozoic Geosphere
Early Paleozoic Climate
Early Paleozoic Biosphere
Benefiting from the Oxygen Boom
Chengjiang Biota
Trilobites
Mollusca
Brachiopoda
Echinodermata
Graptolites
Silurian Reefs
Late Paleozoic
Late Paleozoic Geosphere
Oxygen of the Atmosphere
Life moves onto Land
Diversification of early seedless vascular plants
Diversification of early seed plants
Diversification of Marine Life
Mesozoic
The Breakup of Supercontinent Pangea
The Age of Reptiles
The Age of Reptiles
Reptiles and Birds
Dinosaur Footprints
Dinosaur Eggs
Dinosaur World
Marine Environment
Freshwater Environment
Terrestrial Lake Environment
Plants in the Dinosaur world
Cenozoic
Shaping the Present
Continents in Collision
Break-up of Gondwana – 160 Ma
Indian Continent – Tethys Oceanic Arc Collision – 70-55 Ma
Indian Continent – Asian Continent Collision – 35 Ma
Asian Extrusion – Since 35 Ma
Building the Highest Mountain
Asian Monsoon – At present
Earth Materials
Geological
History of
Hong Kong
Earth Evolution
Reconstruct
Geological History
Solar System
Formation
Archean
Proterozoic
Early
Paleozoic
Late Paleozoic
Mesozoic
Cenozoic
Cenozoic 65 million years ago to present
The Cenozoic is divided into two periods:
Paleogene
65 – 23 million years ago
Neogene
23 million years ago – present
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