1:TheamountofairexchangedisevenlowerinREMthanNREMbecause,althoughbreathingismorerapidinREM,itisalsomoreirregular,withbrimlayersofrockdocumentingtheendoftheCretaceousupintorocksrepresentingthebeginningoftheCenozoic(theeraaftertheMesozoic).
OThefossilrecordsuggeststhattherewasanabruptextinctionofmanyplantsandanimalsattheendoftheMesozoicera.
OFewfossilsoftheMesozoicerahavesurvivedintherocksthatmarktheendoftheCretaceous.
OFossilsfromtheCretaceousperiodoftheMesozoicuptothebeginningoftheCenozoicerahavebeenremovedfromthelayersofrockthatsurroundedthem.
OPlantsandanimalsfromtheMesozoicerawereunabletosurviveintheCenozoicera.
5:Sociologistsviewprimarygroupsasbridgesbetweenindividualsandthelargersocietybecausetheytransmit,mediate,andinterpretasociety'sculturalpatternsandprovidethesenseofonenesssocriticalforsocialsolidarity.
OSociologiststhinkthatculturalpatternsestablishconnectionsbetweentheindividualandthelargersociety.
OSociologistsbelievethatindividualswithasenseofonenessbridgethegapbetweensocietyandprimarygroups.
OSociologiststhinkprimarygroupscontributetosocialsolidaritybecausetheyhelpmaintainasociety'sculturalpatterns.
OSociologistsbelievethattheculturalpatternsthatprovidesocialsolidarityariseasbridgesfromprimarygroups.
Glaciersmoveslowlyacrossthelandwithtremendousenergy,carvingintoeventhehardestrockformationsandtherebyreshapingthelandscapeastheyengulf,push,drag,andfinallydepositrockdebrisinplacesfarfromitsoriginallocation.
CAsaglaciermoves,itleavesbehindrockformationsthathavebeenengulfed,pushed,anddraggedbytheglacier.
CGlaciersreshapethelandscapebycarvingintorockandtransportingtheresultingdebristodistantlocations.
CGlacierscarvethehardestrockformationswithgreatenergyandslowlyreshapethemintodebris.
CThetremendousenergyofslowlymovingglacierstransportsand
finallydepositsrockdebrisintolarge
rockformations.
Thoughitmaybedifficulttoimaginefromalaterperspective,astrainofcriticalopinioninthe1920spredictedthatsoundfilmwouldbeatechnicalnoveltythatwouldsoonfadefrom
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