Here's a quite amazing round of fossilised hardwood from the Rattlesnake Hills located in the east of Washington State. Growth rings are clearly visible in pic1, arching from bottom left to top right.
I have no definite info. on the geological period - although I do have a date for the Cody Shale of the Rattlesnake Hills, placing it at Late Cretaceous (specifically the Campanian Faunal Stage, between 74 and 80 million years ago).
The dealer that I bought this piece from had ID'd the species as beech. Now this guy is one of the most experienced and knowledgeable dealers of petrified wood in the US and not surprisingly the microscopic, fossil evidence fully supports his identification. Consistent with beech wood, the microscope shows a vessel (or pore) structure that is semi-diffuse to diffuse-porus. This is evidenced by the higher concentration of pores in the early springwood with vessels still being laid down in mid to late summer.
This is a lovely piece (I will post a close-up of the whole round in the Close-up/Macro forum). Whilst some areas of fossilisation has left a very detailed record of the original cell structure, other parts are fuzzy and indistinct.
Taken with Olympus SP-350 thru Meiji EMZ-5T. Please use the scale bar from pic1 to infer scale in pic2.
Hope you enjoy.
[UPDATE] I have posted an image of the cross section in the Macro Forum and it should provide a useful frame of reference for these images.
Please see: Close-up/Macro Forum posting.
Bruce


