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cephalopods

4 paragraphs · about 1 minute

Every paragraph the index cites under cephalopods, once, in the order of the book. Beside each stand the entries that cite it.

59:2.11Lime-se­cret­ing al­gae were wide­spread. There ex­isted thou­sands of species of the early an­ces­tors of the corals. Sea worms were abun­dant, and there were many va­ri­eties of jel­ly­fish which have since be­come ex­tinct. Corals and the later types of sponges evolved. The ceph­a­lop­ods were well de­vel­oped, and they have sur­vived as the mod­ern pearly nau­tilus, oc­to­pus, cut­tle­fish, and squid.

59:3.5The trilo­bites rapidly de­clined, and the cen­ter of the stage was oc­cu­pied by the larger mol­lusks, or ceph­a­lop­ods. These an­i­mals grew to be fif­teen feet long and one foot in di­am­e­ter and be­came mas­ters of the seas. This species of an­i­mal ap­peared sud­denly and as­sumed dom­i­nance of sea life.

59:3.6–7 · two paragraphs not cited here ·

59:3.6The great vol­canic ac­tiv­ity of this age was in the Eu­ro­pean sec­tor. Not in mil­lions upon mil­lions of years had such vi­o­lent and ex­ten­sive vol­canic erup­tions oc­curred as now took place around the Med­i­ter­ra­nean trough and es­pe­cially in the neigh­bor­hood of the British Isles. This lava flow over the British Isles re­gion to­day ap­pears as al­ter­nate lay­ers of lava and rock 25,000 feet thick. These rocks were laid down by the in­ter­mit­tent lava flows which spread out over a shal­low sea bed, thus in­ter­spers­ing the rock de­posits, and all of this was sub­se­quently el­e­vated high above the sea. Vi­o­lent earth­quakes took place in north­ern Eu­rope, no­tably in Scot­land.

59:3.7The oceanic cli­mate re­mained mild and uni­form, and the warm seas bathed the shores of the po­lar lands. Bra­chio­pod and other ma­rine-life fos­sils may be found in these de­posits right up to the North Pole. Gas­tropods, bra­chiopods, sponges, and reef-mak­ing corals con­tin­ued to in­crease.

59:3.8The close of this epoch wit­nesses the sec­ond ad­vance of the Sil­urian seas with an­other com­min­gling of the wa­ters of the south­ern and north­ern oceans. The ceph­a­lop­ods dom­i­nate ma­rine life, while as­so­ci­ated forms of life pro­gres­sively de­velop and dif­fer­en­ti­ate.

60:1.13130,000,000 years ago the seas had changed very lit­tle. Siberia and North Amer­ica were con­nected by the Bering Strait land bridge. A rich and unique ma­rine life ap­peared on the Cal­i­for­nian Pa­cific coast, where over one thou­sand species of am­monites de­vel­oped from the higher types of ceph­a­lop­ods. The life changes of this pe­riod were in­deed rev­o­lu­tion­ary not­with­stand­ing that they were tran­si­tional and grad­ual.

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See also mollusks