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Author Topic:   Age Correlations and an Old Earth: Part II.
Minnemooseus
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Posts: 3945
From: Duluth, Minnesota, U.S. (West end of Lake Superior)
Joined: 11-11-2001
Member Rating: 10.0


Message 121 of 306 (169184)
12-16-2004 10:47 PM
Reply to: Message 118 by JonF
12-16-2004 9:41 PM


Natural Carbon isotope fractionation
From:
Principles of Isotope Geology
Gunter Faure
1977, John Wiley & Sons, Inc.
I suspect there is a more recent edition out, but the above is the one I have.
From Chapter 20 - Carbon, p. 379:
quote:
Carbon (Z=6) has two stable isotopes: 12C=98.89 percent and 13C=1.11 percent. In addition, radioactive 14C occurs in nature due to its formation in the upper atmosphere by an (n,p) reaction on stable 14N.
and
quote:
The isotopes of carbon are fractionated by a variety of natural processes, including photosynthesis and isotope exchange reactions among carbon compounds. Photosynthesis leads to enrichment of 12C in biologically synthesized organic compounds. On the other hand, isotope exchange reactions between CO2 gas and aqueous carbonate species tent to enrich carbonates in13C. As a result, the isotopic abundance of 13C in terrestrial carbon varies by about 10 percent.
Of course, the book goes on into a greater detail discussion of this.
I didn't dig around, to find out what influence on Carbon dating these fractionations have. I am confident it is not a fatal influence.
Moose

This message is a reply to:
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RAZD
Member (Idle past 1435 days)
Posts: 20714
From: the other end of the sidewalk
Joined: 03-14-2004


Message 122 of 306 (169193)
12-16-2004 11:24 PM
Reply to: Message 98 by johnfolton
12-16-2004 12:01 PM


Re: Speculations
kettle refers to the shape of the lake in profile -- like a kettle cut in half (the more common known lake profile is like a flattened wok).
it doesn't necessarily have anything to do with the way it was formed. it could be in a rocky substrate, in which case ice could have little effect.
Lake Suigetsu is at "(3535'N, 13553'E) near the coast of the Sea of Japan" from the pdf article.
latitude 35o35' would be about 3.5 of the 4 degrees between horizontal lines and longitude 135o53'would be about where the 136o longitude line crosses the coast below Fukui (not the big lake NE of Kyoto).
see also Earth View

we are limited in our ability to understand
by our ability to understand
RebelAAmerican.Zen[Deist
{{{Buddha walks off laughing with joy}}}

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johnfolton 
Suspended Member (Idle past 5621 days)
Posts: 2024
Joined: 12-04-2005


Message 123 of 306 (169198)
12-17-2004 12:00 AM
Reply to: Message 117 by RAZD
12-16-2004 9:30 PM


Re: Speculations
Razd, I agree with you in respect to the clays settling continually, likely more in the winter. My problem is not with the last 5,000 or so years as much as with how the kettle lake formed in respect to additional varves. The microbiological factors of C14 to C12 being a carbon source for anaerobic bacteria has been documented in the natural. It would appear the dissolved concentration of C-14 & C-12 would decrease the lower in the core sample due to C-14 & C-12
carbonates bubbling upward slowly. It would be interesting if this slightly rising concentration between each varve would of affected the core samples with Carbonate fractionate residues converting c12 to c13 and the possiblility of leaving C14 unaffected to contaminate the c-14 to c-12 ratio's. If so this would give a proportional line of error, no matter if you look at it from a old earth senerio or an young earth senerio.
It would be interesting to see if Moose geology book has more information in respect to C14 being able to fractionate or if its just c12 fractionating into c13.
When they dated the core samples was the leachate dated too? or was it simply discarded? Has it been determined if the leachate still contains C14, C12 & c13 in solution, and if it does what is the ratio. This would be extremely interesting what the ratio of C-14 to C-12 if any existed within the leachate of the core's sampled.
This message has been edited by Craig, 12-17-2004 12:24 AM

This message is a reply to:
 Message 117 by RAZD, posted 12-16-2004 9:30 PM RAZD has replied

Replies to this message:
 Message 124 by RAZD, posted 12-17-2004 1:01 AM johnfolton has not replied
 Message 125 by Minnemooseus, posted 12-17-2004 1:57 AM johnfolton has replied

RAZD
Member (Idle past 1435 days)
Posts: 20714
From: the other end of the sidewalk
Joined: 03-14-2004


Message 124 of 306 (169226)
12-17-2004 1:01 AM
Reply to: Message 123 by johnfolton
12-17-2004 12:00 AM


Re: Speculations
craig writes:
. My problem is not with the last 5,000 or so years as much as with how the kettle lake formed in respect to additional varves.
And you also need to explain how a different method of suddenly causing the varves can (1) look exactly like the annual varves in thickness, composition, types of organic samples, types of pollen, etcetera, etcetera, (2) have imbedded in them organic samples that just happen to test to the correct C14 age without needing a sudden totally discontinuous change in the behavior of radioactive decay and (3) makes exactly the same changes to tree rings around the world and ice layers at opposite ends of the earth.
It would be interesting if this slightly rising concentration between each varve would of affected the core samples with Carbonate fractionate residues converting c12 to c13 and the possiblility of leaving C14 unaffected to contaminate the c-14 to c-12 ratio's. If so this would give a proportional line of error, no matter if you look at it from a old earth senerio or an young earth senerio.
It would be interesting to see if Moose geology book has more information in respect to C14 being able to fractionate or if its just c12 fractionating into c13.
no, that just does not happen. read about it -- learn.
you might try: Radiometric Dating ... he discusses several methods of radiometric dating, including the other two methods mentioned in the OT ... that also corroborate the C14 dates.
I repeat: other methods CONFIRM the dating of both the varves and the radio carbon methods, and they also CORRELATE for climate and other events. There is no way that bubbling carbonate in the bottom of a lake in japan can change the ice layers in antarctica and greenland or the calcite deposits in a cave in the US.

we are limited in our ability to understand
by our ability to understand
RebelAAmerican.Zen[Deist
{{{Buddha walks off laughing with joy}}}

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Minnemooseus
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Posts: 3945
From: Duluth, Minnesota, U.S. (West end of Lake Superior)
Joined: 11-11-2001
Member Rating: 10.0


Message 125 of 306 (169238)
12-17-2004 1:57 AM
Reply to: Message 123 by johnfolton
12-17-2004 12:00 AM


Re: Speculations
Craig, referring to my message 121 writes:
It would be interesting to see if Moose geology book has more information in respect to C14 being able to fractionate or if its just c12 fractionating into c13.
The chemical processes lightly touched on in message 121 DO NOT change one isotope of Carbon into another.
Quoting myself from 121:
quote:
On the other hand, isotope exchange reactions between CO2 gas and aqueous carbonate species tend to enrich carbonates in13C.
What this is saying, as I understand it, is that when C03 disolved in water comes in contact with atmospheric CO2, there is an exchange of C between the two phases. In this exchange, the 12C tends to slightly preferentially go into the atmospheric CO2, and the 13C tends to slightly preferentially go into the disolved carbonate (CO3). This would cause in any precipitated CO3 (I presume as CaCO3) to be higher in 13C.
I don't know how this process might effect 14C in the sediments. It would seem that it would also be slightly enriched. BUT the Carbon dating is NOT being done on the carbonate (per someone upthread), but rather on organic carbon from plant debris.
Moose
ps: Doing all these sub and superscripts sure is a pain.

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 Message 123 by johnfolton, posted 12-17-2004 12:00 AM johnfolton has replied

Replies to this message:
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PaulK
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Posts: 17828
Joined: 01-10-2003
Member Rating: 2.5


Message 126 of 306 (169245)
12-17-2004 2:35 AM
Reply to: Message 115 by johnfolton
12-16-2004 8:25 PM


Re: Speculations
You claimed:
quote:
This article specifically factually addressed C-14 has been consumed by anaerobic bacteria in a controlled study.
As I pointed out that was clearly false. The article specifically stated that there was virtually no C14 in the kerogen - and as a result virtually none in the bacteria either.
Having shown that you now say:
quote:
PaulK, The scientists know the bacteria are consuming the kerogen, because they designed their experiment so that kerogen was the only source of carbon available for the bacteria to eat.
But that is not at issue and does not help your case at all because it provides absolutely NO evidence that it could upset the ratio of C14 to C12.
You know it would have been far better to admit that you were wrong than to suddenly try to switch the subject. It's tactics like that that get creationists their - deserved - reputation for dishonesty.

This message is a reply to:
 Message 115 by johnfolton, posted 12-16-2004 8:25 PM johnfolton has replied

Replies to this message:
 Message 127 by johnfolton, posted 12-17-2004 11:24 AM PaulK has replied

johnfolton 
Suspended Member (Idle past 5621 days)
Posts: 2024
Joined: 12-04-2005


Message 127 of 306 (169360)
12-17-2004 11:24 AM
Reply to: Message 126 by PaulK
12-17-2004 2:35 AM


Re: Speculations
PaulK,
PaulK: As I pointed out that was clearly false. The article specifically stated that there was virtually no C14 in the kerogen - and as a result virtually none in the bacteria either.
Craig: They cultured the bacteria from the New Albany Shale that that was so old that that the C14 was completely decayed. They then fed these New Albany Shale cultured bacteria new kerogen that was these bacteria's only carbon source.
The reason they fed these cultured bacteria only kerogen as its carbon source was because there was no C14 in the bacteria they cultured.
http://nai.nasa.gov/news_stories/news_detail.cfm?ID=87
But because the New Albany Shale is so old, the C-14 has completely decayed. The kerogen in the shale no longer contains any C-14.
"We grew bacteria collected from this rock and measured the C-14 content of their cells," says Petsch. "These measurements showed that these living bacteria contain very little to no C-14.
The scientists know the bacteria are consuming the kerogen, because they designed their experiment so that kerogen was the only source of carbon available for the bacteria to eat.

This message is a reply to:
 Message 126 by PaulK, posted 12-17-2004 2:35 AM PaulK has replied

Replies to this message:
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Loudmouth
Inactive Member


Message 128 of 306 (169367)
12-17-2004 11:37 AM
Reply to: Message 116 by johnfolton
12-16-2004 8:55 PM


Re: Speculations
quote:
We at least agree C-14 & C12 is bubbling away increasing the concentration in the above varve layers. It does appear that C-14 and C-12 are a bit different. C-14 is an extremely unstable isotope, while C-12 is not.
C14 and C12 are different, but not different enough for the bacteria to preferentially eat one isotope and not the other. The very fact that C14 is unstable gives us the ability to date the leaves. The instability of C14 is the very reason that carbon dating works.
quote:
Since we agree that C-14 & C-12 concentrations are increase in solution in the varves above. I'm suspecting that its being re-absorbed by hydrogen bonds onto the leaf surface at a different ratio.
Bzzz, wrong. The leaf and insect samples are treated to remove loosely bound debris from the samples. Also, the most likely form of carbon being released by anaerobic bacteria is methane which has very little to no reactivity through hydrogen bonds. Methane and other gases released by the bacteria would not react with the leaves in any way that would affect carbon dating.
quote:
I doubt there is anyway to test for hydrogen bonded carbon. Instead of carbon assimulated within the kerogens.
We are not talking about kerogen, we are talking about leaves. Also, the very study you cite does not claim that the bacteria were able to change the carbon date of the kerogen, so your claim is empty anyway.
quote:
The water in the varves would supply the hydrogen to bond to the kerogen particles surfaces. I'm suspecting they are not bonding at the same ratio they were absorbed while living. Do you have evidence that they would bond at the same ratio?
Do you have any evidence that waste products from bacteria bind to the leaves?

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 Message 116 by johnfolton, posted 12-16-2004 8:55 PM johnfolton has not replied

johnfolton 
Suspended Member (Idle past 5621 days)
Posts: 2024
Joined: 12-04-2005


Message 129 of 306 (169368)
12-17-2004 11:41 AM
Reply to: Message 125 by Minnemooseus
12-17-2004 1:57 AM


Re: Speculations
minnemooseus, If C12 is bubbling out of solution more readily than is C13 which tends to go into solution. If C14 tends to go into solution as C13 is as a carbonate, then C12 is bubbling out of solution at a greater rate. I do like your senerio that CO2 is a gas containing C12, and C13 tendancy to be dissolved as calcium carbonate CaCO3. If C14 tends to form calcium carbonate then you have the means of disrupting the C14 to C12 ratio by calcium carbonate bonds to the leafs outer surface (kerogen).
This message has been edited by Craig, 12-17-2004 11:48 AM

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 Message 125 by Minnemooseus, posted 12-17-2004 1:57 AM Minnemooseus has not replied

Replies to this message:
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Coragyps
Member (Idle past 764 days)
Posts: 5553
From: Snyder, Texas, USA
Joined: 11-12-2002


Message 130 of 306 (169369)
12-17-2004 11:43 AM
Reply to: Message 125 by Minnemooseus
12-17-2004 1:57 AM


Re: Speculations
I don't know how this process might effect 14C in the sediments.
Fractionation such as your reference talks about depends almost completely on the mass of the isotope in question - just the mass, nothg else. So a process that enriches a sediment in 13C will enrich it a little more in 14C, because it's even heavier. This phenomenon has been measured many times with oxygen, where 16O, 17O, and 18O are all stable. And sulfur, with four stable isotopes.

This message is a reply to:
 Message 125 by Minnemooseus, posted 12-17-2004 1:57 AM Minnemooseus has not replied

Coragyps
Member (Idle past 764 days)
Posts: 5553
From: Snyder, Texas, USA
Joined: 11-12-2002


Message 131 of 306 (169371)
12-17-2004 11:50 AM
Reply to: Message 129 by johnfolton
12-17-2004 11:41 AM


Re: Speculations
Craig, you seem to be just stringing words together here.

This message is a reply to:
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johnfolton 
Suspended Member (Idle past 5621 days)
Posts: 2024
Joined: 12-04-2005


Message 132 of 306 (169388)
12-17-2004 12:27 PM
Reply to: Message 131 by Coragyps
12-17-2004 11:50 AM


Re: Speculations
Coragyps,
Your premise too supports the ratio of C14 to C12 is subject to laws in respect to the atomic weight of C14 being greater than C12. I agree your premise supports C14 disrupting the C14 to C12 ratio, in favor of an young earth.
I however think the ratio might be more disrupted by Mooses senerio. If C14 tends to form carbonates, and C12 tends to form CarbonDioxide. Then this could disrupt the C14 to C12 ratio, by simple carbonate bonds to the surface of the leafs and other organics being dated.
I agree both your senerios appear to be supporting the young earth senerio. It might be that both of your senerios work in tandum. Its refreshing to see it doesn't support an old earth senerio. If all was suggesting C12 increases that would of supported an old earth senerio, its interesting that the evidence is supporting the young earth senerio.
This message has been edited by Craig, 12-17-2004 12:29 PM

This message is a reply to:
 Message 131 by Coragyps, posted 12-17-2004 11:50 AM Coragyps has replied

Replies to this message:
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 Message 135 by PaulK, posted 12-17-2004 1:13 PM johnfolton has not replied
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Loudmouth
Inactive Member


Message 133 of 306 (169390)
12-17-2004 12:30 PM
Reply to: Message 132 by johnfolton
12-17-2004 12:27 PM


Re: Speculations
quote:
I however think the ratio might be more disrupted by Mooses senerio. If C14 tends to form carbonates, and C12 tends to form CarbonDioxide. Then this could disrupt the C14 to C12 ratio, by simple carbonate bonds to the surface of the leafs and other organics being dated in the varves.
Could you please support the hypothesis that carbonate binds to leaves within the varves in a way that prevents removal before the sample is dated?

This message is a reply to:
 Message 132 by johnfolton, posted 12-17-2004 12:27 PM johnfolton has not replied

PaulK
Member
Posts: 17828
Joined: 01-10-2003
Member Rating: 2.5


Message 134 of 306 (169397)
12-17-2004 1:06 PM
Reply to: Message 127 by johnfolton
12-17-2004 11:24 AM


Re: Speculations
You're just confusing yourself. There's no mention of new kerogen and the points you yourself make contradict that.
So again I have to point out that the fact that the bacteria ate the kerogen is not being disputed - and it isn't relevant.
On the other hand your suggestion that bacteria selectively ate C14 from the kerogen is an outright falsehood - the fact is that there was virtually no C14 in the kerogen in the first place.
The only honest thing for you to do is to admit that you misread the article and what it actually says does not help you. Handwaving wildly in the hope that nobody will notice your error is typical creationist behaviour but rather less than honest.

This message is a reply to:
 Message 127 by johnfolton, posted 12-17-2004 11:24 AM johnfolton has not replied

PaulK
Member
Posts: 17828
Joined: 01-10-2003
Member Rating: 2.5


Message 135 of 306 (169401)
12-17-2004 1:13 PM
Reply to: Message 132 by johnfolton
12-17-2004 12:27 PM


Re: Speculations
Craig, if the sediment were enriched in C14 it would appear YOUNGER, not older. How would the sediment being older than the C14 dates show help a young Earth ?

This message is a reply to:
 Message 132 by johnfolton, posted 12-17-2004 12:27 PM johnfolton has not replied

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