A New Geologic Age–Started by Us

At first, the thesis of this article, published in the January 28, 2008, issue of World Science, shocked me.  But as I thought about it, it makes sense that the growing impact we humans are having on our planet has altered the planet so much that we have pushed the planet into a whole new geologic epoch.  Scientists call it, aptly, the ‘Anthropocene.’

Jan. 25, 2008
World Science staff

A rad­i­cal pro­pos­al is gain­ing ground among ge­ol­o­gists: We have en­tered a new ge­o­log­ic time pe­ri­od on Earth, thanks to ma­nkind’s own ac­ti­vi­ties.We’ve so dras­tic­ally changed the land­scape through pol­lu­tion and in oth­er ways, it’s time to ac­knowl­edge the new “ep­och” is here, a group of ge­ol­o­gists writes Jan. 25 in GSA To­day, a jour­nal of the Geo­lo­gi­cal So­ciety of Am­er­ica.

An at­las pub­lished by the Unit­ed Na­tions in 2005 showed through sat­el­lite im­ages how var­i­ous parts of the world have phys­i­cal­ly changed in the past two to three dec­ades alone. These im­ages show the mouth of Chi­na’s Yel­low Riv­er in 1979 (a­bove) and 2000 (be­low). A new pen­in­su­la in the low­er im­age arises from sed­i­ment de­posits from the riv­er part­ly re­sult­ing from farm­ing ac­tiv­i­ty, U.N. ex­perts say. (Cour­te­sy U.N. En­vi­ron­ment Pro­gramme) 


The new era would be called the An­thro­po­cene, from the Greek an­thro­pos (man) and ceno (new). “The dom­i­nance of huma­ns has so phys­ic­ally changed Earth that there is in­creas­ingly less jus­tifica­t­ion for link­ing pre- and post-in­dus­tri­al­ized Earth with­in the same ep­och,” the re­search­ers said in an an­nounce­ment of their pro­pos­al.The tra­di­tion­al name for our cur­rent ep­och—soon to be­come the form­er one, if they have their way—is the Hol­o­cene. The Hol­o­cene has spanned the last 10,000 years and fol­lowed the Pleis­to­cene, com­monly called the Ice Age.The re­search­ers at the Un­ivers­ity of Leices­ter, U.K. and the Ge­o­log­i­cal So­ci­e­ty of Lon­don said human im­pact on Earth is show­ing in ma­ny ways: changed ero­sion pat­terns; ma­jor dis­tur­bances to the car­bon cy­cle; glob­al warm­ing; whole­sale changes to plant and an­i­mal life; and ocean acid­i­fi­ca­t­ion.Al­though ge­ol­o­gy is mainly the study of Earth’s rocks, soil and phys­ical struc­ture—rather than an­i­mals and life forms as such—all these fac­tors can ul­ti­mately in­flu­ence that struc­ture, re­search­ers say. Man’s al­tera­t­ions to Earth are “strati­graphic­ally sig­nif­i­cant,” the group said in the an­nounce­ment.

The idea for rec­og­niz­ing a new ge­o­log­ic era is­n’t new, though: No­bel Prize-winning chem­ist Paul Crut­zen sug­gested it in 2002. The U.K. re­search­ers’ work rep­re­sented an at­tempt to further assess his pro­po­sal.

The group said their find­ings pre­s­ent the schol­arly ground­work for con­sid­era­t­ion by the In­terna­t­ional Com­mis­sion on Stra­tig­ra­phy for for­mal adop­tion of the An­thro­po­cene as the new­est ad­di­tion to the ge­o­log­ical timescale.

Be­fore the Hol­o­cene and pre­ced­ing Pleis­to­cene, the ma­jor era pre­ced­ing that is called the Ter­tiary Pe­ri­od, from about 26 to 66 mil­lion years ago. That was when mam­mals largely took over the Earth from the by then-defeated di­no­saurs. All these ages are con­sid­ered part of a larg­er one, called the Ce­no­zo­ic era. Be­fore that was the Mes­o­zo­ic, the age of di­no­saurs; and still ear­li­er, the Pa­le­o­zo­ic, which saw the ev­o­lu­tion­ary ex­plo­sion of the first an­i­mals. Eve­ry­thing be­fore that is the “Pre­cam­bri­an.”* * *Send

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