Geographical and stratigraphic distribution of fossil coelacanths and the living genus Latimeria
Extinct coelacanths
Fossil coelacanths are well known from a variety of Northern hemisphere localities including (Forey, 1998):
- Middle Devonian, Latvia
- Upper Devonian, Quebec, Canada
- Upper Devonian, Germany
- Devonian, Carboniferous, Permian, Triassic, Cretaceous, USA
- Upper Carboniferous, Permian, Jurassic and Upper Cretaceous, United Kingdom
- Upper Permian, Lower Triassic, China
- Lower Triassic, Spitsbergen, Norway
- Lower Triassic, Greenland
- Middle Triassic, Switzerland
- Upper Triassic, Austria
- Upper Jurassic Solnhofen limestones, Germany
- Middle Triassic, Spain
(Forey, 1998)
Macropoma lewesiensis is from the Upper Cretaceous Chalk, England
Southern hemisphere (Gondwanan) fossil coelacanth taxa (Forey, 1998)
- Devonian, Australia
- Devonian, South Africa
- Lower Triassic, Madagascar
- Lower Jurassic, India
- Lower Cretaceous Santana Formation, Brazil
- Cretaceous, Egypt, Algeria, Democratic Republic of Congo, Morocco, Niger
Extant coelacanths
Living coelacanths (Latimeria) have been discovered off the coasts of
- East Africa
- South Africa
- Madagascar
- Mozambique
- Comoros Islands
- Indonesia (Sulawesi).