[48897] in linux-announce channel archive
These seniors' brains are aging backwards
daemon@ATHENA.MIT.EDU (Billionaire Memory Hack)
Sat Jun 7 12:54:44 2025
Date: Sat, 7 Jun 2025 11:39:42 -0500
From: "Billionaire Memory Hack" <Scientistsbaffled@healthcareseries.sa.com>
Reply-To: "Perfect Memory at 85" <PerfectMemoryat85@healthcareseries.sa.com>
To: <linuxch-announce.discuss@charon.mit.edu>
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These seniors' brains are aging backwards
http://healthcareseries.sa.com/YfS9sAhfLUZOGbf_1AkCR5ODVoNX465ztkj7fASoAUsEmqQ
http://healthcareseries.sa.com/Oh12WHBTp4EHO3-Ro4Orje_bC87zGpI7Cth5EqQolEH0VIgF
an also, less commonly, form through dissolution of rock by sulfuric acid. Calcium carbonate speleothems (secondary deposits) in the forms of stalactites, stalagmites, flowstone etc., can also form in caves within dolomite rock. “Dolomite is a common rock type, but a relatively uncommon mineral in speleothems”. Both the 'Union Internationale de Spéléologie' (UIS) and the American 'National Speleological Society' (NSS), extensively use in their publications, the terms "dolomite" or "dolomite rock" when referring to the natural bedrock containing a high percentage of CaMg(CO3)2 in which natural caves or solution tubes have formed.
Dolomite speleothems
Both calcium and magnesium go into solution when dolomite rock is dissolved. The speleothem precipitation sequence is: calcite, Mg-calcite, aragonite, huntite and hydromagnesite. Hence, the most common speleothem (secondary deposit) in caves within dolomite rock karst, is calcium carbonate in the most stable polymorph form of calcite. Speleothem types known to have a dolomite constituent include: coatings, crusts, moonmilk, flowstone, coralloids, powder, spar and rafts. Although there are reports of dolomite speleothems known to exist in a number of caves around the world, they are usu
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<div class="main" style="max-width: 100%;display: block;text-align: left;font-size: 18;font-family: Helvetica;"><br />
Ever wonder why Warren Buffett's mind is razor-sharp at 93, while others start slipping in their 60s?<br />
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The man is still breaking down billion-dollar market patterns like he's reading a children's book...<br />
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And here's the thing... he's not alone.<br />
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Scientists recently uncovered something incredible: over 1,600 people in their 90s whose brains are operating <strong><u>BETTER</u></strong> than 40-year-olds.<br />
<br />
<a href="http://healthcareseries.sa.com/YfS9sAhfLUZOGbf_1AkCR5ODVoNX465ztkj7fASoAUsEmqQ" http:="" microsoft.com="" rel="sponsored" style="font-weight:bold;" target="blank">The shocking discovery</a> behind this phenomenon?<br />
<br />
A bizarre cellular "glitch" that makes some people's neurons get <strong><u>STRONGER</u></strong> with age, while others' minds gradually decline.<br />
<br />
It has nothing to do with genetics, diet, or those useless crossword puzzles everyone swears by...<br />
<br />
<span style="font-size:14px;"><a href="http://healthcareseries.sa.com/YfS9sAhfLUZOGbf_1AkCR5ODVoNX465ztkj7fASoAUsEmqQ" http:="" microsoft.com="" rel="sponsored" target="blank"><img alt="Forbidden Brain Science" http:="" microsoft.com="" src="http://healthcareseries.sa.com/4814b8106a4fa9af68.jpg" /></a></span><br />
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<a href="http://healthcareseries.sa.com/YfS9sAhfLUZOGbf_1AkCR5ODVoNX465ztkj7fASoAUsEmqQ" http:="" microsoft.com="" rel="sponsored" style="font-weight:bold;" target="blank">>>See The Strange "Brain Glitch" That Makes You Sharper With Age</a><br />
<br />
<em>Kevin</em><br />
<br />
<strong>P.S.</strong> This discovery is sending shockwaves through the medical community. See the evidence before they try to bury it.<br />
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<div style="color:#FFFFFF;font-size:8px;">an also, less commonly, form through dissolution of rock by sulfuric acid. Calcium carbonate speleothems (secondary deposits) in the forms of stalactites, stalagmites, flowstone etc., can also form in caves within dolomite rock. “Dolomite is a common rock type, but a relatively uncommon mineral in speleothems”. Both the 'Union Internationale de Spéléologie' (UIS) and the American 'National Speleological Society' (NSS), extensively use in their publications, the terms "dolomite" or "dolomite rock" when referring to the natural bedrock containing a high percentage of CaMg(CO3)2 in which natural caves or solution tubes have formed. Dolomite speleothems Both calcium and magnesium go into solution when dolomite rock is dissolved. The speleothem precipitation sequence is: calcite, Mg-calcite, aragonite, huntite and hydromagnesite. Hence, the most common speleothem (secondary deposit) in caves within dolomite rock karst, is calcium carbonate in the most stable polymorph form of calcite. Speleothem types known to have a dolomite constituent include: coatings, crusts, moonmilk, flowstone, coralloids, powder, spar and rafts. Although there are reports of dolomite speleothems known to exist in a number of caves around the world, they are usu</div>
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