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Paper 59

The Marine-Life Era on Urantia

Life Carrier

2. The First Continental Flood Stage
The Invertebrate-Animal Age

59:2.1The pe­ri­odic phe­nom­ena of land el­e­va­tion and land sink­ing char­ac­ter­is­tic of these times were all grad­ual and non­spec­tac­u­lar, be­ing ac­com­pa­nied by lit­tle or no vol­canic ac­tion. Through­out all of these suc­ces­sive land el­e­va­tions and de­pres­sions the Asi­atic mother con­ti­nent did not fully share the his­tory of the other land bod­ies. It ex­pe­ri­enced many in­un­da­tions, dip­ping first in one di­rec­tion and then an­other, more par­tic­u­larly in its ear­lier his­tory, but it does not pre­sent the uni­form rock de­posits which may be dis­cov­ered on the other con­ti­nents. In re­cent ages Asia has been the most sta­ble of all the land masses.

59:2.2350,000,000 years ago saw the be­gin­ning of the great flood pe­riod of all the con­ti­nents ex­cept cen­tral Asia. The land masses were re­peat­edly cov­ered with wa­ter; only the coastal high­lands re­mained above these shal­low but wide­spread os­cil­la­tory in­land seas. Three ma­jor in­un­da­tions char­ac­ter­ized this pe­riod, but be­fore it ended, the con­ti­nents again arose, the to­tal land emer­gence be­ing fif­teen per cent greater than now ex­ists. The Caribbean re­gion was highly el­e­vated. This pe­riod is not well marked off in Eu­rope be­cause the land fluc­tu­a­tions were less, while the vol­canic ac­tion was more per­sis­tent.

59:2.3340,000,000 years ago there oc­curred an­other ex­ten­sive land sink­ing ex­cept in Asia and Aus­tralia. The wa­ters of the world’s oceans were gen­er­ally com­min­gled. This was a great lime­stone age, much of its stone be­ing laid down by lime-se­cret­ing al­gae.

59:2.4A few mil­lion years later large por­tions of the Amer­i­can con­ti­nents and Eu­rope be­gan to emerge from the wa­ter. In the West­ern Hemi­sphere only an arm of the Pa­cific Ocean re­mained over Mex­ico and the pres­ent Rocky Moun­tain re­gions, but near the close of this epoch the At­lantic and Pa­cific coasts again be­gan to sink.

59:2.5330,000,000 years ago marks the be­gin­ning of a time sec­tor of com­par­a­tive quiet all over the world, with much land again above wa­ter. The only ex­cep­tion to this reign of ter­res­trial quiet was the erup­tion of the great North Amer­i­can vol­cano of east­ern Ken­tucky, one of the great­est sin­gle vol­canic ac­tiv­i­ties the world has ever known. The ashes of this vol­cano cov­ered five hun­dred square miles to a depth of from fif­teen to twenty feet.

59:2.6320,000,000 years ago the third ma­jor flood of this pe­riod oc­curred. The wa­ters of this in­un­da­tion cov­ered all the land sub­merged by the pre­ced­ing del­uge, while ex­tend­ing far­ther in many di­rec­tions all over the Amer­i­cas and Eu­rope. East­ern North Amer­ica and west­ern Eu­rope were from 10,000 to 15,000 feet un­der wa­ter.

59:2.7310,000,000 years ago the land masses of the world were again well up ex­cept­ing the south­ern parts of North Amer­ica. Mex­ico emerged, thus cre­at­ing the Gulf Sea, which has ever since main­tained its iden­tity.

59:2.8The life of this pe­riod con­tin­ues to evolve. The world is once again quiet and rel­a­tively peace­ful; the cli­mate re­mains mild and equable; the land plants are mi­grat­ing far­ther and far­ther from the seashores. The life pat­terns are well de­vel­oped, al­though few plant fos­sils of these times are to be found.

59:2.9This was the great age of in­di­vid­ual an­i­mal or­gan­is­mal evo­lu­tion, though many of the ba­sic changes, such as the tran­si­tion from plant to an­i­mal, had pre­vi­ously oc­curred. The ma­rine fauna de­vel­oped to the point where ev­ery type of life be­low the ver­te­brate scale was rep­re­sented in the fos­sils of those rocks which were laid down dur­ing these times. But all of these an­i­mals were ma­rine or­gan­isms. No land an­i­mals had yet ap­peared ex­cept a few types of worms which bur­rowed along the seashores, nor had the land plants yet over­spread the con­ti­nents; there was still too much car­bon diox­ide in the air to per­mit of the ex­is­tence of air breathers. Pri­mar­ily, all an­i­mals ex­cept cer­tain of the more prim­i­tive ones are di­rectly or in­di­rectly de­pen­dent on plant life for their ex­is­tence.

59:2.10The trilo­bites were still promi­nent. These lit­tle an­i­mals ex­isted in tens of thou­sands of pat­terns and were the pre­de­ces­sors of mod­ern crus­taceans. Some of the trilo­bites had from twenty-five to four thou­sand tiny eye­lets; oth­ers had aborted eyes. As this pe­riod closed, the trilo­bites shared dom­i­na­tion of the seas with sev­eral other forms of in­ver­te­brate life. But they ut­terly per­ished dur­ing the be­gin­ning of the next pe­riod.

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.

59:2.12There were many va­ri­eties of shell an­i­mals, but their shells were not then so much needed for de­fen­sive pur­poses as in sub­se­quent ages. The gas­tropods were pres­ent in the wa­ters of the an­cient seas, and they in­cluded sin­gle-shelled drills, peri­win­kles, and snails. The bi­valve gas­tropods have come on down through the in­ter­ven­ing mil­lions of years much as they then ex­isted and em­brace the mus­sels, clams, oys­ters, and scal­lops. The valve-shelled or­gan­isms also evolved, and these bra­chiopods lived in those an­cient wa­ters much as they ex­ist to­day; they even had hinged, notched, and other sorts of pro­tec­tive ar­range­ments of their valves.

59:2.13So ends the evo­lu­tion­ary story of the sec­ond great pe­riod of ma­rine life, which is known to your ge­ol­o­gists as the Or­dovi­cian.

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