[12775] in linux-announce channel archive
Enjoy the lush Rainforest... & Beautiful beaches, of Costa Rica
daemon@ATHENA.MIT.EDU (Visit Costa Rica)
Tue Apr 28 20:28:34 2015
Date: Tue, 28 Apr 2015 20:28:33 -0400
To: <linuxch-announce.discuss@charon.mit.edu>
From: "Visit Costa Rica" <VisitCostaRica@benevered.eu>
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Cannot read our news-letter below as no picture is present? <a href="http://www.benevered.eu/l/lt1LV9841T185KU/190W857KF63225IY305SJ130895471BB136709584"> Go ahead and tap right here to fix.</a>
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<a target="" href="http://www.benevered.eu/l/lt1XT9841S185DU/190H857YB63225BH305JU130895471PS136709584" id="subj"> Enjoy the lush Rainforest... & Beautiful beaches, of Costa Rica </a>
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<p>multiplying only by gamogenesis, must be introduced in considerable numbers that some may propagate. Thus we infer that the earliest traces of life 9fdaba190ace50880dc4155f29cb9a3e
left in the sedimentary deposits near these new shores, will be traces of life as humble as that indicated in the most ancient rocks of Great Britain 9fdaba190ace50880dc4155f29cb9a3e
and Ireland. Imagine now that the processes above indicated, continue—that the emerging lands become wider in extent, and fringed by higher and more 9fdaba190ace50880dc4155f29cb9a3e
varied shores; and that there still go on those ocean-currents MNN 9fdaba190ace50880dc4155f29cb9a3e which, at long intervals, convey from far 9fdaba190ace50880dc4155f29cb9a3e distant shores immigrant forms of life.
What will result? Lapse of 9fdaba190ace50880dc4155f29cb9a3e time will of course favour the introduction of such new forms: 9fdaba190ace50880dc4155f29cb9a3e admitting, as it must, of those combinations of fit
conditions, which can occur only after long intervals. Moreover, the increasing area of the islands, individually and as a group, implies JLIG
increasing length of coast, and therefore a longer line of QMBL contact with the streams and JJENVPPU waves which bring [235] drifting mhies bearing germs of fresh
life. And once more, the comparatively-varied<b>shores, presenting physical conditions which change from mile to mile, will</b>furnish suitable habitats NOTIXRS
for more numerous species. So that as the elevation proceeds, three causes 9fdaba190ace50880dc4155f29cb9a3e conspire to introduce additional marine plants and animals. to what clhies
will the increasing Fauna be 9fdaba190ace50880dc4155f29cb9a3e for a long period confined? Of course, to clhies of which individuals, or their germs, 9fdaba190ace50880dc4155f29cb9a3e are most liable to be carried
far away from their native shores by floating sea-weed or drift-wood; to clhies which are YQVSNIG BRUJYL also least likely to VCAGL perish 9fdaba190ace50880dc4155f29cb9a3e in transit, EVJTLGJCD or from change of
climate; and to those which can best subsist around coasts comparatively bare of life. Evidently then, corals, annelids, 9fdaba190ace50880dc4155f29cb9a3e inferior molluscs, and
crustaceans of low grade, will chiefly constitute 9fdaba190ace50880dc4155f29cb9a3e the early Fauna. The large predatory members of these clhies, will be later in establishing
themselves; both because the new shores must first become well peopled by the creatures they prey on, and because, being more complex, they, or their RBWLA
ova, must be less likely to survive the journey, and the change 9fdaba190ace50880dc4155f29cb9a3e 9fdaba190ace50880dc4155f29cb9a3e of conditions. We may infer, then, that the strata deposited 9fdaba190ace50880dc4155f29cb9a3e next after the
almost “azoic” strata, would contain the remains of invertebrata, allied to those<i>found near</i>9fdaba190ace50880dc4155f29cb9a3e the shores of Australia and South America. Of such
invertebrate remains,<I>the lower beds would furnish comparatively few genera, and those 9fdaba190ace50880dc4155f29cb9a3e of relatively low types; while in the upper beds the</I>
number of genera would be greater, PHSDRBEM and 9fdaba190ace50880dc4155f29cb9a3e the types higher: just as among the fossils of our Silurian system. As this great geologic change slowly
advanced through its long history of earthquakes, volcanic disturbances, minor upheavals and subsidences—as the extent of the archipelago became 9fdaba190ace50880dc4155f29cb9a3e
greater and its smaller islands coalesced into larger ones, while its coast-line grew still longer and more varied, and the neighbouring sea more VONI
thickly inhabited by inferior forms of life; the lowest division of the vertebrata would MPKUDOQML begin 9fdaba190ace50880dc4155f29cb9a3e to be represented. In order of time, fish would
[236] naturally come later than the lower invertebrata; both as being less likely to have their ova transported across the waste of CUUF waters, and as .</p>
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