ジャドフタ層とは - わかりやすく解説 Weblio辞書

ジャドフタ層

出典: フリー百科事典『ウィキペディア（Wikipedia）』 (2023/08/31 04:42 UTC 版)

ジャドフタ層^[2]^[6]^[7]（ジャドフタそう、Djadochta Formation^{[注 2]}、ジャドフタ累層^[4]）とは、中央アジアのゴビ砂漠に位置し、7500万年前から7100万年前にかけての後期白亜紀（上部白亜系）の化石を多く含む層である^[7]。砂海 (sand sea)環境を示す風成層 (eolian deposit)を主体とし、それと同時異相関係を示す湖成層および河川成層から構成される^[7]。模式地（type locality）は「燃える崖 Flaming Cliffs^{[注 3]}」で著名なバインザク (Bayn Dzak）で、恐竜、哺乳類、そして他の化石爬虫類の化石がこの層から発見されている^[10]。

脚注

注釈

^ バルンゴヨト層^[2]、バルンゴヨット累層^[4]とも
^ Djadochta はDjadokhta、Djadokata、Dzhadokhtskayaとも転写される
^ 「炎の崖」^[1]や「フレイミング・クリフ」^[8]、「燃え上がる崖」^[9]とも
^ Bain Dzak, Bayanzag, Bayn Zag, Bayan Zagとも書かれる
^ Tugrik, Toogreeg, Toogreek, Tugreek, Tugrug, Turgrugyin, Tugrugeen, Tögrögiin, Tugrikiin, Tugrikinとも書かれる
^ Udan Sayr, Udan Sair, Ulaan Sair, Üüden Sairとも書かれる。ウダンサイル^[2]、ウディンサイール^[28]とも。
^ Oka Tolgaとも書かれる
^ Dzamyn Khondt, Zamin Khond, or Dzamin Khondとも書かれる
^ Alag Teeg, Alag Teerとも書かれる
^ 炭酸塩岩の一種
^ ネメグト累層とも^[4]
^ ただし、のちにジャドフタ層であることは否定されネメグト層 (Nemegt Formation)から産出したことが指摘されている^[137]。

出典

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