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Fossil Hunting on Mars and in
Central London
A talk by Michael Morris Franks
For the Astronomical Society of Harringay
20th
May 2010
Three types of Rocks
1) Sedimentary
2) Igneous
3) Metamorphic
Fossils are found mainly in
sedimentary rocks.
Mars has Sedimentary Rocks
Strangely Mars has no Limestone
rocks which is surprising given
that it has CO2 and appears to
have had open water which
should have caused the
formation of limestone. Maria
Zuber , Itay Halevy and Daniel
Scrag of Harvard University have
suggested that thought that the
reason is due to sulphur from
volcanoes which prevented the
formation of limestone.
The two Mars Rover, Spirt and Opportunity have a battery of
cameras and have been spending pictures back to earth for
over five years. Some people have claimed to see evidence
of Fossils in the photographs.
Sir Charles W. Shults III has produced a CD with
photographs which he claims show fossils.
What is the Evidence
1) Sphercules
2) Rotini
3) Sol 34 object
Ockham's Razor
The Knoll criterion, named after Andrew Knoll author of
“Life on a Young Planet. The Knoll criterion is that
anything being put forward as a fossil must not only look
like something that was once alive—it must also not look
like anything that can be made by non-biological means.
Preparing for a trip to Mars
By Looking for Fossils in Central London
1) Portland Stone
a) Roach Stone
b) Whitbed
c) Basebed
2)Flint
3) Sandstone
4) Slate
Roach Stone
Economist Building 25 St James Street
Aptyxiella portlandica (Sowerby), Portland screwstone
Caxton House Tuthill Street London SW1
Grove Whitbed
Bivalue Shell Possibly Camptonectes lamellosus
Isognomon
Red Algae Solenpora grew in Reef Patches
These slides identified by Mark Golden of Albion Stone Plc
Portland Stone Traflagar Square
An artists' impression of the Jurassic sea bed at the time
of the formation of the Portland Stone.
From The Ecology of Fossils, by Dr Stuart McKerrow as
Editor, Pub. Duckwork. 1978
Key
a. Ostrea - the oyster (Liostrea)
b. Calcareous algal mould (Solenoprara)
c. Boring bivalve, burrowing into the agal (Lithophaga)
d. Ostrea - a small curved species (Pleurotomaria)
e. A fossil Top-shell: a marine snail (Pleurotmaria)
f. a tall spiral marine snail (Protocerithium)
Calcareous algae are rubbery mats which trap fine lime
sand and partly precopate calcite (lime) from sea water.
The algae has no internal structure as such and no
tissue is fossilised.
By kind permission of the author
British Library
Fossilised sea sponges in Hauteville limestone located outside the Conference Centre
Fossilied Flint 14 Tufton StreeL London SW1
A selections of small echinoids preserved as flint
Royal Festival Hall London
Sandstone Cobble from Faringdon
Slate Solitary Horn Coral fossilised in slate could be 350-410 million years old.

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Fossil talk

  • 1. Fossil Hunting on Mars and in Central London A talk by Michael Morris Franks For the Astronomical Society of Harringay 20th May 2010
  • 2. Three types of Rocks 1) Sedimentary 2) Igneous 3) Metamorphic
  • 3. Fossils are found mainly in sedimentary rocks. Mars has Sedimentary Rocks
  • 4. Strangely Mars has no Limestone rocks which is surprising given that it has CO2 and appears to have had open water which should have caused the formation of limestone. Maria Zuber , Itay Halevy and Daniel Scrag of Harvard University have suggested that thought that the reason is due to sulphur from volcanoes which prevented the formation of limestone.
  • 5. The two Mars Rover, Spirt and Opportunity have a battery of cameras and have been spending pictures back to earth for over five years. Some people have claimed to see evidence of Fossils in the photographs. Sir Charles W. Shults III has produced a CD with photographs which he claims show fossils.
  • 6. What is the Evidence 1) Sphercules 2) Rotini 3) Sol 34 object
  • 7. Ockham's Razor The Knoll criterion, named after Andrew Knoll author of “Life on a Young Planet. The Knoll criterion is that anything being put forward as a fossil must not only look like something that was once alive—it must also not look like anything that can be made by non-biological means.
  • 8.
  • 9. Preparing for a trip to Mars By Looking for Fossils in Central London 1) Portland Stone a) Roach Stone b) Whitbed c) Basebed 2)Flint 3) Sandstone 4) Slate
  • 10. Roach Stone Economist Building 25 St James Street
  • 11. Aptyxiella portlandica (Sowerby), Portland screwstone
  • 12. Caxton House Tuthill Street London SW1 Grove Whitbed Bivalue Shell Possibly Camptonectes lamellosus
  • 14. Red Algae Solenpora grew in Reef Patches These slides identified by Mark Golden of Albion Stone Plc
  • 16.
  • 17. An artists' impression of the Jurassic sea bed at the time of the formation of the Portland Stone. From The Ecology of Fossils, by Dr Stuart McKerrow as Editor, Pub. Duckwork. 1978 Key a. Ostrea - the oyster (Liostrea) b. Calcareous algal mould (Solenoprara) c. Boring bivalve, burrowing into the agal (Lithophaga) d. Ostrea - a small curved species (Pleurotomaria) e. A fossil Top-shell: a marine snail (Pleurotmaria) f. a tall spiral marine snail (Protocerithium) Calcareous algae are rubbery mats which trap fine lime sand and partly precopate calcite (lime) from sea water. The algae has no internal structure as such and no tissue is fossilised. By kind permission of the author
  • 18. British Library Fossilised sea sponges in Hauteville limestone located outside the Conference Centre
  • 19. Fossilied Flint 14 Tufton StreeL London SW1
  • 20.
  • 21. A selections of small echinoids preserved as flint
  • 24. Slate Solitary Horn Coral fossilised in slate could be 350-410 million years old.