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Tracking Ancient Life Dr Liam Herringshaw [email protected]
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Page 1: Tracking Ancient Life Dr Liam Herringshaw lgh865@hotmail.com.

Tracking Ancient Life

Dr Liam Herringshaw

[email protected]

Page 2: Tracking Ancient Life Dr Liam Herringshaw lgh865@hotmail.com.

Key terms

Bioturbation

Ichnology

(ichnos, Greek: footprint, track, trail)

Trace Fossils

Page 3: Tracking Ancient Life Dr Liam Herringshaw lgh865@hotmail.com.

1. What are trace fossils?

Sedimentary structures produced by life- Burrows, borings, tracks, trails, roots...

Page 4: Tracking Ancient Life Dr Liam Herringshaw lgh865@hotmail.com.

...and dung!

The Lloyds Bank coprolite

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Why they matter

• Fossil record of behaviour

• Fossil record of soft-bodied organisms

• Organism-environment interactions

• Ecological niche creation

• Nutrient flux

• Taphonomy

Luminous lugworm

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UniformitarianismThe present is the key

to the past

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Ichnological principles

1. Same organism; different traces

Arthropod trace fossils

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Ichnological principles

2. Different organisms; same traces

Annelid wormsSea anemones

Phoronids

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Ichnological principles

3. Same trace; different preservation

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2. Traces of Yorkshire

What trace fossils does the museum have?

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3. Common trace fossils

(Burrows, trails; mostly marine)

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Ichnotaxonomy

N.B. Names are for trace fossil only, not organism that made the structure

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Planolites

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SkolithosSkolithos

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Thalassinoides

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Thalassinoides tracemaker?

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Chondrites

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OphiomorphaOphiomorpha

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OphiomorphaOphiomorpha tracemaker? tracemaker?

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Rhizocorallium

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Rusophycus

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Rusophycus tracemaker?

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Trace fossil?

Impression of a jellyfish?

Or a sand volcano?

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Not trace fossils

Shrinkage cracks

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Flute castsFlute casts

Not trace fossilsNot trace fossils

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Hand Specimens:What Have You Got?

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4. The Fossil Record of Behaviour

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Earliest animals?

565 Ma locomotion trails,Newfoundland:

Liu et al. (2010)http://geology.gsapubs.org/content/38/2/123.abstract

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Ediacaran-CambrianEdiacaran-Cambrianboundaryboundary

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Cambrian complexity

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The Cambrian Explosion

Seilacher & Pfluger (1994)

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Onshore to offshore

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Colonization of landColonization of land

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Plant Trace Fossils

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Becoming upright

Trackway analysis shows tetrapods become bipedal in early Triassic

Kubo & Benton (2009)

http://onlinelibrary.wiley.com/doi/10.1111/j.1475-4983.2009.00897.x/full

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The speed of dinosaurs

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5. The speed of dinosaurs?

• Type of footprint?

• Footprint size?

• Animal size?

• Stride length?

• Speed?

• Behaviour?

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Calculating trackmaker speed

v = 0.25*g0.5*SL1.67*h-1.17

Or, more simply:

Hip height = 4 x footprint length

Stride length/ hip height = speed

(<2 = walking, >3 = running)

Sheffield Geology Group – dinosaur speed calculator:http://www.sorbygeology.group.shef.ac.uk/DINOC01/dinocal1.html

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Useful links

www.fossilhub.org