Road Trip through
Tertiary Texas!
Dave Grant, Ocean Institute - Sandy Hook, NJ

 

Our objective was to study lower Eocene outcrops along the Colorado River in Bastrop.

Locked in these sediments is evidence of Paleocene-to-Eocene Climatic Events that some researchers say are related to the Earth's 100,000 year-long orbital eccentricities reported by Milankovitch.

   

The deposits are primarily sedimentary layers that include river terraces, sandstone, carbonaceous sand, silt, beach sand, lignite and mudstone.

The layers demonstrate a transgressive sequence of rising sea levels that have covered much of coastal Texas over the last 55-million years.

 
   

 
A tense moment and potential traffic jam near the river is defused when our mission is explained.
   
Evidence of biological activity in marine sediments: The fossilized burrows of crustaceans Thalassinoides and Ophiomorpha

   

 
Argiope aurantia
Local biological curiosities included spiders weaving webs (Left), and great masses of resting daddy-long-legs under cool shaded ledges (Below).

 

 
Moths resting during the heat of the day.

 

 

Botanical curiosities included lichens, poison oak sedges and an assortment of famous Texas wildflowers.

 

 

 

 

 

 
Bio-hazard: Dave's heel after an
encounter with fire ants.

 
Cliff swallows helped manage the insect population near the river.

 
   

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