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wyandottecaver wrote:a note of caution.
sediments in caves are invariably sediments transported there. Seems obvious. But when you think about organic material, or even the entire sediment layer, being deposited topside..perhaps in a shallow marsh, stream bank, etc etc. then 20,000 yrs later sediments get washed away by erosion and re-deposited in a cave. Then, 100 yrs later some guy comes along and says hey look...this was put here 20,000 yrs ago.
I was once in a cave that had tall sediment banks about 6' tall on each side of a small stream. The sediments were very nicely layered with alternating bands of differing fine silts and clays material. As we were walking along we too were speculating on age of the sediments and wondering about finding bears teeth or pleistocene mammal bones. Then we saw a very modern broken in half 8" clay pot like youd buy at wallmart.. completely imbedded in the sediment like you had just cut a cake and exposed it about halfway up. Thus, 3 FEET of silt and clay sediments from topside had been deposited over that pot in no more than the last 50-75 years and probably less.
Something to think about.
wyandottecaver wrote:think in geologic time scales. Not to put too fine a point on it... Lots of geologic work has been done on caves by people who dont really understand them. You CAN NOT assume anything about the history of any sediment in a cave short of some of the cosmic ray dating and even that has assumptions. That clay 100ft above the CURRENT water table wasn't always. It still had to get transported there by water sometime.
Example 2.
Clays and organics get layed down topside 30,500 yrs ago. 30,000 yrs ago the glaciers melt and they get washed into a ancient cave. 15,000 yrs ago a landslide plugs a local stream creating a temporay lake that re-infiltrates the old cave passages on the valley wall and then when the landslide plug is breached and the water levels rapidly drop again washes the old sediments to the oxygen poor bottom of the new marsh in the valley floor and burys them under new recently created sediments . 10,000 yrs ago both the "new" sediments above them and the "old" sediments are once again washed from the now dry marsh by erosion from a seasonal flood event downstream into yet another smaller, younger (5,000 yrs old at that time.) cave and the old sediments deposited OVER the younger stream bank sediments that were eroded first. Both these are deposited in the "upper" levels of the cave.... Shortly after that the cave stream breaches a chert layer and in 100 yrs rapidy downcuts through shales and soft limestones allowing it to pirate more water and reach another strata 80ft below where it cuts another 20 ft in 10,000 years leaving our sediments safe from further disturbance.
Thus our 30,500 yr old clay is now in a 15,000 yr old cave and has spent 500 yrs on the surface, 5,000 yrs buried under younger sediments and water in a anoxic marsh, 25,000 yrs underground and 10,000 yrs ago was deposited on top of sediments only 10-15,000 yrs old in a passage 100ft above the current water table. A guy comes in looking for organics.....
Joseph W. Dixon wrote:You might want to take some preliminary samples and test them to see how much organic matter is even in them. Any soil testing lab in the country should be able to tell you that and it isn't very expensive. If you have a soils or agronomy department on campus they might even do it for free. I'd also talk with someone at your college or university in the soils department, especially someone who has worked with paleosols, since that is essentially what you'd be working with. I have never used a Munsell chart on cave sediments, but all of the cave sediments I can recall (here in Iowa) have a high chroma which would be indicitive of low amounts of organic matter. I would honestly be curious to know just how much organic matter you'd find in your samples.
jharman2 wrote:Allen,
I know of at least one MS thesis that was conducted in a nearby cave that used paleomagnetic dating to determine the age of cave sediments. I don't claim to understand the technology or its pros and cons or how it compares to radiometric methods, but it may be something you want to look into.
kkerrigan wrote:I'm also a geology student, possibly looking to do a hydrogeology related thesis (still need to figure that whole thing out, haha.) I actually just read a short article today which may be of interest to you. The authors used paleomagnetic analysis of sediment dating, but I believe used a lab at Pittsburgh university, and I doubt it was an undergrad thesis topic, but still interesting. The book in which the article I read (and probably other relevant articles) is/are found is entitled "Studies of Cave Sediments: Physical and Chemical Records of Paleoclimate", edited by Ira D. Sasowsky and and John Mylroie. Google book link: http://books.google.com/books?id=E4QCpb-3f1MC&pg=PA75&lpg=PA75&dq=kooken+cave+sediment&source=bl&ots=8SYC9elSyL&sig=zQWSlWTALnRHjY3vHirY_SfkPmI&hl=en&ei=f7bETJTBJ8OqlAfk6NDgAg&sa=X&oi=book_result&ct=result&resnum=1&ved=0CBMQ6AEwAA#v=onepage&q=kooken%20cave%20sediment&f=false This isn't the complete article, unfortunately, but if it's interesting enough I'm sure you could order it.
Page 71-82, Paleomagnetic Analysis of a Long Term Sediment Trap, Kooken Cave, Huntingdon County, PA, USA. Not precisely what you were talking about but close-ish!
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