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Message-ID: <111073873399511107522027905911941@fvd39nx4.liverwork.rest>
To: <bruce@untroubled.org>
Date: Wed, 18 Jan 2023 05:48:44 -0800
From: "Dementia Warning" <DementiaWarning@liverwork.rest>
Subject: Common food linked to dementia
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Hi,

Harvard scientists warn:
http://www.liverwork.rest/l/lt11HU11107WM27FG/5220A9059IE11941OW14SO33995EO3235043478
You may be skyrocketing your dementia risk… simply by putting this on your dinner plate.

Countless studies link this food to memory loss - even in people in their 50s. No wonder one in three Americans dies in a nursing home, unable to recognize their loved ones.

Millions of Americanseat this almost every single day… often without knowing the damage it does to your brain. Are you?

Find out for yourself now…
http://www.liverwork.rest/l/lt12GD11107IS27WR/5220Q9059AL11941NW14FR33995BB3235043478
Bernice

P.S. Fortunately, as soon as you STOP eating this food…

Your brain cells start to regenerate… protecting your precious memories… and blessing you with the crystal clear thinking you had before middle-age.
http://www.liverwork.rest/l/lt13KY11107JX27EP/5220A9059MU11941QK14PF33995QE3235043478
But first, check out what this food is and see if you're eating it.





http://www.liverwork.rest/l/lt14NV11107MG27TH/5220W9059VU11941NU14AF33995VE3235043478













Peloneustes is known from the Peterborough Member (formerly known as the Lower Oxford Clay) of the Oxford Clay Formation.[2] While Peloneustes has been listed as coming from the Oxfordian stage (spanning from about 164 to 157 million years ago[1]) of the Upper Jurassic,[7] the Peterborough Member actually dates to the Callovian stage (spanning from about 166 to 164 million years ago[1]) of the Middle Jurassic.[2] The Peterborough Member spans from the late lower Callovian to the early upper Callovian, occupying the entirety of the Middle Callovian.[46] It overlays the Kellaways Formation[46] and is overlain by the Stewartby Member of the Oxford Clay Formation.[47] The Peterborough Member is primarily composed of grey bituminous (asphalt-containing)[46] shale and clay[48] rich in organic matter.[49] These rocks are sometimes fissile (splittable into thin, flat slabs).[47] The member is about 16–25 metres (52–82 ft) thick, stretching from Dorset to Humber.[46] The Peterborough Member represents an epicontinental sea during a time of rising sea levels.[49] When it was deposited, it would have been located at a latitude of 35°N.[47] This sea, known as the Oxford Clay sea, was largely encircled by islands and continents, which provided the seaway with sediment.[47] Its proximity to land is demonstrated by the preservation of terrestrial fossils such as driftwood in the Oxford Clay, in addition to a clastic dike in the lower levels of the Peterborough Member, with the dike's formation being facilitated by rainwater.[48] The southern region of the Oxford Clay Sea was connected to the Tethys Ocean, while it was connected to more boreal regions on its northern side. This allowed for faunal interchange to occur between the Tethyan and boreal regions. This sea was approximately 30–50 metres (100–160 ft) deep within 150 kilometres (93 mi) of the shoreline.[47][2] map of the world in the Jurassic, indicating the Oxford Clay Formation was located near a warm temperate climate Map of the world in the Jurassic, the Oxford Clay Formation is located at E1 The surrounding land would have had a Mediterranean climate, with dry summers and wet winters, though it was becoming increasingly arid. Based on information from δ18O isotopes in bivalves, the water temperature of the seabed of the Peter













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