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Why only the Mediterranean region? quote]
Because it is the most recent (large scale) evaporation sequence and because it is Miocene in age, which I have been discussing on another thread.
Ho yes; it is impossible for creationists to explain all the earth evaporates (includes salt) in their mere 6000 years of biblical magical mystical history.
I bet you want even give it a go, like all creationists you ignore all the difficult questions.
Here are some more evoporite basins f--l
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Late Carboniferous Variscan orogenic front, and the distribution of Permian Rotliegend sedimentary facies and Zechstein halite deposits
Lets see you creationists explain all the world evaporate deposits in the context of a 6000 year old Earth, I bet you cannot.
I am merely explaining the chemistry to you. This is part of geochemistry. If details are going to be a bother, then by all means use this as your excuse to back out now.
Why only the Mediterranean region? quote]
Because it is the most recent (large scale) evaporation sequence and because it is Miocene in age, which I have been discussing on another thread.
Ho yes; it is impossible for creationists to explain all the earth evaporates (includes salt) in their mere 6000 years of biblical magical mystical history.
I bet you want even give it a go, like all creationists you ignore all the difficult questions.
Here are some more evoporite basins f--l
![]()
![]()
Late Carboniferous Variscan orogenic front, and the distribution of Permian Rotliegend sedimentary facies and Zechstein halite deposits
Lets see you creationists explain all the world evaporate deposits in the context of a 6000 year old Earth, I bet you cannot.
So, salt is the only Na sink you know. Right? If you can do calculation, then you "should" have converted to a YEC already.
That is what I called "half-bottle" knowledge.
So, salt is the only Na sink you know. Right? If you can do calculation, then you "should" have converted to a YEC already.
That is what I called "half-bottle" knowledge.
Not at all, let's stick to the Med for the moment
Why would volcanic activity in early earth give so much CO2? Which is nearly all inorganic in origin.
The most abundant gas typically released into the atmosphere from volcanic systems is water vapor (H20), followed by carbon dioxide (C02) and sulfur dioxide (S02).
Is it fair to say that all CO3 in the early ocean was given by CO2 in the air? If so, how quickly would the CO2 in the air be reduced in concentration?
If you like, here might be some thinking you can do:
The increase of global temperature will also increase the dissolution rate of solid carbonate on land
Can you make a model on this process? Plug in some values and see how it works.
The increase of global temperature will also increase the dissolution rate of solid carbonate on land
Hmm, I'm still seeing a pattern here. Juv displays ignorance of a subject, a scientist posts (including details and citations). Juv denies it (no detail, no citations). And then Juv tells the scientists to come up with a mechanism for him.
I guess you do not appreciate that I showed you a list of reference and showed you the abst and conclusion of a particular article. Fine. I won't do it again unless you request for it. Thank you for saving me some time.
You are very cocky.
...
If you do not participate in the goal searching process with me, then once I formated my question, I won't even talk to you, because you would have no idea on what I am talking about at that time.
Read again my reply. I***t.
I don't think you know enough sodium sinks in the ocean to ask me this question. And, if you think all the sinks are "in the ocean" (means under the seawater), you are further wrong.
...
So, smart guy, I don't expect you give me any answer that I don't know.
OK: From the USGS site :
There is a little table comparing hot spot, convergent and divergent plate boundaries. In each case the top two major volume % components of volcanic gases are H2O and CO2.
QED.
(Oh, and one other question, what is the point you wish to make about the "inorganic" origin of carbon here? I don't understand what you are getting at?)
Well, I suppose one could hypothesize that shortly after the proto-oceans "rained out" and air was high in CO2 that an equilibrium could be established using the above mentioned reactions (I am tired of typing out the reactions in detail over and over considering that you have put almost no effort into this science discussion) and an attendant rate expression.
Rather than asking the questions all the time, try making a scientific point as well. While I'm obviously happy to talk the science, I was rather under the impression you thought you could talk the science as well. Right now all I see from you are questions and cut-n-paste references.
I look forward to your submitting some science here.
There may be a way to bring the two sub-discussions here together;
we are talking about salinity in the oceans and carbonate chemistry in the oceans.
Indeed, carbon dioxide solubility in the oceans is impacted not only by temperature but also salinity. (SOURCE)
Maybe there is a common ground we can exploit here?
So do tell me, again, why I'm the one who has to go "do" things while all you do is "cut-n-paste"? I am beginning to wonder if all you got is "questions" for others to answer for you or if you understand the science?
I thought we were having a "discussion" here and not just you telling me what to do.
Here's a perfect chance for you to do some simple "teaching":
Explain the mechanism, please.
If you do not like to do anything, that is fine with me.
Increase temperature <-- more CO2 in air --> more acidic the rain, the surface water --> faster dissolution on limestone. Also, warmer temperature will also speed up the dissolution.
What else to explain?
I like this type of post. Simple, thoughtful and challenging. Much better than your lengthy "explanation".
Let me think about it for a moment.
If you like, here might be some thinking you can do:
The increase of global temperature will also increase the dissolution rate of solid carbonate on land, and will thus increase the input of Mg, Ca to the ocean. In turn, they will make the ocean water more alkaline. In this consideration, there will be a time lag between the lowering of pH in the ocean and later increase of pH due to the Mg/Ca input. How long would the time lag be? Are we seeing this effect today? I guess the time is not long enough for us to see any change on the river water chemistry. So everybody cried on the "crisis".
Can you make a model on this process? Plug in some values and see how it works.