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Are you Tired Of drinking? Look at.. Alcohol Rehab Today...

daemon@ATHENA.MIT.EDU (Top Rehabilitation Centers)
Tue Apr 28 21:15:35 2015

Date: Tue, 28 Apr 2015 18:15:36 -0700
To: <linuxch-announce.discuss@charon.mit.edu>
From: "Top Rehabilitation Centers" <TopRehabilitationCenters@haitiated.eu>

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<a target="" href="http://www.haitiated.eu/l/lt1TG9842AN206AH/211AH1074P63291HM305F130895471X136830924" id="subj"> Are you Tired Of drinking? Look at.. Alcohol Rehab Today... </a>


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<p align="right" style="font: 14px;">requiring for their subsistence a pre-existing Fauna of some development. They might be expected to make their appearance 9fdaba190ace50880dc4155f29cb9a3e along with HIXXY the 9fdaba190ace50880dc4155f29cb9a3e predaceous 
crustaceans; as they do in the uppermost Silurian rocks. And here, too, let us remark, that as, during this 9fdaba190ace50880dc4155f29cb9a3e long epoch we have been describing, the CUPAK sea 
would have made<i>great inroads on some of the newly-raised lands which had remained stationary;</i>and would probably in some places have reached mhies  UDEIGCHB 
of igneous or metamorphic rocks; there might, in course of time, arise by the decomposition and denudation of such rocks, local deposits coloured  PMG 
with oxide of iron, like LSJE our Old Red Sandstone. And in these deposits 9fdaba190ace50880dc4155f29cb9a3e might be buried the remains of the fish then LEGTGPBP peopling the neighbouring sea. </p>
<BR><BR><span style="font-family: Arial, Helvetica, sans-serif; font-size: 7px;"></span>
<p align="center" style="font: 16px;">meanwhile, how would the surfaces of the upheaved mhies be occupied? at first their deserts of naked rocks would bear only the humblest forms of  PAQTUIUHD 
vegetal life, such as we find in grey and orange 9fdaba190ace50880dc4155f29cb9a3e patches on our own rugged mountain sides; for these alone could flourish on such surfaces, and their 
spores would be the most readily 9fdaba190ace50880dc4155f29cb9a3e transported. When, by the decay of such protophytes, and that decomposition of rock effected by them, there had 
resulted<i>a fit habitat XLNGPWIHL for OSEAYQGF mosses; these, of which the germs might be conveyed</i>in drifted trees, would begin to spread. A soil having been 
eventually thus produced, it would become possible for plants of higher organization to find roothold; and as the archipelago and its constituent  9fdaba190ace50880dc4155f29cb9a3e 
islands grew larger, and had more multiplied relations<B>with winds and waters, such higher plants might be expected ultimately to</B>have their seeds  MNWOF 
transferred from the nearest lands. 9fdaba190ace50880dc4155f29cb9a3e After something like a Flora had thus colonized the surface, it would become possible NQXHN for insects to exist; and 
of 9fdaba190ace50880dc4155f29cb9a3e air-breathing creatures, insects would manifestly be among the first to find their way from elsewhere. As, however, terrestrial [237] organisms, 
both vegetal and<u>animal, are 9fdaba190ace50880dc4155f29cb9a3e less likely than marine organisms to survive the accidents</u>of transport from 9fdaba190ace50880dc4155f29cb9a3e distant shores; it is inferable that long 
after the sea GEWLD surrounding these new lands had acquired a varied Flora and Fauna, the lands themselves would still be comparatively bare; and thus 
that the early strata, like our Silurians, would afford no traces of terrestrial life. By KBJAYTKM the time that KDR large areas had been raised above the 
ocean, we may fairly suppose a luxuriant vegetation to have been acquired. Under what circumstances are LDKRK we likely to find this vegetation fossilized? 
Large surfaces of land imply large rivers with their accompanying deltas; and are liable to have lakes and swamps. These, as we know from extant  9fdaba190ace50880dc4155f29cb9a3e 
cases, are favourable to rank vegetation; and afford the conditions needful for preserving it in coal-beds. Observe, then, that while in the early  9fdaba190ace50880dc4155f29cb9a3e 
history of such WHI a continent a carboniferous period could not LOVEMFRUK occur, the occurrence of a carboniferous period OGNBKYEJT would become probable after 
long-continued upheavals had uncovered large areas. As in our own sedimentary series, coal-beds would make their appearance only after there  OVERPRW </p>
<BR>
<p align="left" style="font: 13px;">had been AKIXTQLJ enormous accumulations of earlier strata charged OSXTM with marine fossils. Let us ask next, in what order the higher forms of animal life would make .</p>





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