白亜紀と古第三紀の間の大量絶滅とは？ わかりやすく解説

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白亜紀と古第三紀の間の大量絶滅

出典: フリー百科事典『ウィキペディア（Wikipedia）』 (2024/03/10 10:23 UTC 版)

白亜紀と古第三紀の間（K-Pg）の大量絶滅（はくあきとこだいさんきのあいだのたいりょうぜつめつ、英語: Cretaceous–Paleogene extinction event, K–Pg extinction event[注釈 1]、または白亜紀と第三紀の間の（K–T）大量絶滅[注釈 2]）は、約6600万年前に突如起こったとされる、地球上の動植物のうち4分の3の種が絶滅した[2][3][4]大量絶滅である[3]。


脚注

注釈

  1. ^ 英略語のうちKは白亜紀の一般的な略語でドイツ語で白亜紀を意味するKreideに由来する。一方でPgは古第三紀を意味する略語である。
  2. ^ かつて古第三紀は第三紀（Tertiary）と呼ばれることが多かったが、現在この呼び方は国際層序委員会から正式な地質年代の呼称として推奨されていない[1]。
  3. ^ 核爆発や天体衝突といった高圧化で生成される内部構造をもった鉱物。
  4. ^ この巨大津波は海岸線から数十～数百km離れた陸地まで到達したとされる。

出典

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