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II

           Ontheotherhand,theprevalenceofveryearlylifeformswassingularinthehighestdegree. Thoughthelimestoneformationwas,ontheevidenceofsuchtypicalimbeddedfossilsasventriculites,positivelyandunmistakablyComanchianandnotaparticleearlier,thefreefragmentsinthehollowspaceincludedasurprisingproportionfromorganismshithertoconsideredaspeculiartofarolderperiods-evenrudimentaryfishes,mollusks,andcoralsasremoteastheSilunanorOrdovician. Theinevitableinferencewasthatinthispartoftheworldtherehadbeenaremarkableanduniquedegreeofcontinuitybetweenthelifeofoverthreehundredmillionyearsagoandthatofonlythirtymillionyearsago. HowfarthiscontinuityhadextendedbeyondtheOligoceneAgewhenthecavernwasclosedwasofcoursepastallspeculation. Inanyevent,thecomingofthefrightfuliceinthePleistocenesomefivehundredthousandyearsago-amereyesterdayascomparedwiththeageofthiscavity-musthaveputanendtoanyoftheprimalformswhichhadlocallymanagedtooutlivetheircommonterms. 

           Lakewasnotcontenttolethisfirstmessagestand,buthadanotherbulletinwrittenanddispatchedacrossthesnowtothecampbeforeMoultoncouldgetback. AfterthatMoultonstayedatthewirelessinoneoftheplanes,transmittingtome-andtotheArkhamforrelayingtotheoutsideworld-thefrequentpostscriptswhichLakesenthimbyasuccessionofmessengers. Thosewhofollowedthenewspaperswillremembertheexcitementcreatedamongmenofsciencebythatafternoon’sreports -reportswhichhavefinallyled,afteralltheseyears,totheorganizationofthatveryStarkweather-MooreExpeditionwhichIamsoanxioustodissuadefromitspurposes. 

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