[48898] in linux-announce channel archive
Add 13 Years to Your Life With This Simple Habit
daemon@ATHENA.MIT.EDU (Youth Secrets)
Sat Jun 7 13:46:16 2025
Date: Sat, 7 Jun 2025 12:46:12 -0500
From: "Youth Secrets" <LifeExtension@spectrelaptop.ru.com>
Reply-To: "Aging Fix" <HealthBoost@spectrelaptop.ru.com>
To: <linuxch-announce.discuss@charon.mit.edu>
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Add 13 Years to Your Life With This Simple Habit
http://spectrelaptop.ru.com/xE559bQvHGDzd0ZPcgDKX2EFBe5T9IAjzzVhNZ2bwuQ7ro15
http://spectrelaptop.ru.com/3Y0Nwp4r4zbrwqWi_ACSMRGvQXtJU7SGe58K5zL3ApjWiQU8
awater precipitate high-magnesium calcite instead. This substance, which has an excess of calcium over magnesium and lacks calcium-magnesium ordering, is sometimes called protodolomite. Raising the temperature makes it easier for magnesium to shed its hydration shell, and dolomite can be precipitated from seawater at temperatures in excess of 60 °C (140 °F). Protodolomite also rapidly converts to dolomite at temperatures of 250 °C (482 °F) or higher. The high temperatures necessary for the formation of dolomite helps explain the rarity of Cenozoic dolomites, since Cenozoic seawater temperatures seldom exceeded 40 °C.
It is possible that microorganisms are capable of precipitating primary dolomite. This was first demonstrated in samples collected at Lagoa Vermelha, Brazil in association with sulfate-reducing bacteria (Desulfovibrio), leading to the hypothesis that sulfate ion inhibits dolomite nucleation. Later laboratory experiments suggest bacteria can precipitate dolomite independently of the sulfate concentration. With time other pathways of interaction between microbial activity and dolomite formation have been added to the discord regarding their role in modulation and generation of polysaccharides, manganese and zinc within the porewater. Meanwhile, a contrary view held by other researchers is that microorganisms precipitate only high-magnesium calcite but leave open the question of whether this can lead to precipitation of dolom
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<div class="main" style="max-width: 100%;display: block;text-align: left;font-size: 18;font-family: Helvetica;">If you're scared of aging...<br />
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<div style="color:#FFFFFF;font-size:8px;">awater precipitate high-magnesium calcite instead. This substance, which has an excess of calcium over magnesium and lacks calcium-magnesium ordering, is sometimes called protodolomite. Raising the temperature makes it easier for magnesium to shed its hydration shell, and dolomite can be precipitated from seawater at temperatures in excess of 60 °C (140 °F). Protodolomite also rapidly converts to dolomite at temperatures of 250 °C (482 °F) or higher. The high temperatures necessary for the formation of dolomite helps explain the rarity of Cenozoic dolomites, since Cenozoic seawater temperatures seldom exceeded 40 °C. It is possible that microorganisms are capable of precipitating primary dolomite. This was first demonstrated in samples collected at Lagoa Vermelha, Brazil in association with sulfate-reducing bacteria (Desulfovibrio), leading to the hypothesis that sulfate ion inhibits dolomite nucleation. Later laboratory experiments suggest bacteria can precipitate dolomite independently of the sulfate concentration. With time other pathways of interaction between microbial activity and dolomite formation have been added to the discord regarding their role in modulation and generation of polysaccharides, manganese and zinc within the porewater. Meanwhile, a contrary view held by other researchers is that microorganisms precipitate only high-magnesium calcite but leave open the question of whether this can lead to precipitation of dolom</div>
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