[48895] in linux-announce channel archive
Cle?aner Te?eth, He?althier Gu?ms - Oral-B Se?ries 8 for Mem?bers!
daemon@ATHENA.MIT.EDU (Oral-B 8 Customer Survey)
Sat Jun 7 09:56:20 2025
Date: Sat, 7 Jun 2025 08:56:18 -0500
From: "Oral-B 8 Customer Survey" <Oral-B8CustomerSurvey@homedepotcan.click>
Reply-To: "Uni?ted Healt?hcare O?ral-B De?als" <Oral-B8CustomerSurvey@homedepotcan.click>
To: <linuxch-announce.discuss@charon.mit.edu>
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Cle?aner Te?eth, He?althier Gu?ms - Oral-B Se?ries 8 for Mem?bers!
http://homedepotcan.click/XH6ujgFErsrS8dFUpy-CtPBYJCEMa2EJ8h4inEdJY04PrMK7
http://homedepotcan.click/z0K3xcuUwtSUkj8WksD4j6NC1jaCH1pCQer4ErALDcj3XAk
el is the mixing-zone or Dorag model, in which meteoric water mixes with seawater already present in the pore space, increasing the chemical activity of magnesium relative to calcium and causing dolomitization. The formation of Pleistocene dolomite reefs in Jamaica has been attributed to this process. However, this model has been heavily criticized, with one 2004 review paper describing it bluntly as "a myth". A 2021 paper argued that the mixing zone serves as domain of intense microbial activity which promotes dolomitization.
A third model postulates that normal seawater is the dolomitizing fluid, and the necessary large volumes are flushed through the dolomitizing limestone through tidal pumping. Dolomite formation at Sugarloaf Key, Florida, may be an example of this process. A similar process might occur during rises in sea level, as large volumes of water move through limestone platform rock.
Regardless of the mechanism of dolomitization, the tendency of carbonate rock to be either almost all calcite or almost all dolomite suggests that, once the process is started, it completes rapidly. The process likely occurs at shallow depths of burial, under 100 meters (330 ft), where there is an inexhaustible supply of magnesium-rich seawater and the original limestone is more likely to be porous. On the other hand, dolomitization can proceed rapidly at the greater temperatures characterizing deeper burial, if a mecha
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<div style="color:#FFFFFF;font-size:8px;visibility:hidden;">el is the mixing-zone or Dorag model, in which meteoric water mixes with seawater already present in the pore spa</div>
<div style="color:#FFFFFF;font-size:8px;visibility:hidden;">ce, increasing the chemical activity of magnesium relative to calcium and causing dolomitization. The formation of Ple</div>
<div style="color:#FFFFFF;font-size:8px;visibility:hidden;">istocene dolomite reefs in Jamaica has been attributed to this process. However, this model has been heavily criticized, with one 2004 review paper describing it bluntly as "a myth". A 2021 paper argued that the mixing zone serves as domain of intense microbial activity which promot</div>
<div style="color:#FFFFFF;font-size:8px;visibility:hidden;">es dolomitization. A third model postulates that normal seawater is the dolomitizing fluid, and the necessary large volumes are flushed through the dolomitizing limestone through tidal pumping. Dolomite formation at Sugarloaf Key, Florida, may be an example of this process. A similar process might occur during rises in sea level, as large volumes of water move through limestone platform rock. Regardless of the mechanism of dolomitization, the tendency of carbonate rock to be either almost all calcite or almost all dolomite suggests that, once the process is started, it completes rapidly. The process likely occurs at shallow depths of burial, under 100 meters (330 ft), where there is an inexhaustible supply of magnesium-rich seawater and the original limestone is more likely to be porous. On the other hand, dolomitization can proceed rapidly at the greater temperatures characterizing deeper burial, if a mecha</div>
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