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ຍຸກຄຣີເຕຊຽດ ອ້າງອີງ ແຫຼ່ງຂໍ້ມູນອື່ນ ລາຍການການນຳທາງUCMP Berkeley Cretaceous pageBioerosion website at The College of Wooster

ແມ່ແບບ:ຍຸກທາງທໍລະນີຍຸກຈູແຣດຊິກຍຸກພາລີໂອຈີນອັງກິດທໍລະນີການໂລກມະຫາຍຸກມີໂຊໂຊອິກຍຸກຈູແຣດຊິກຍຸກພາລີໂອຈີນມະຫາຍຸກຊີໂນໂຊອິກພາສາລາແຕັງຫີນປູນຄສ 1822ຊັ້ນຫີນແອ່ງປາຣີການຊີກາກໂບນັດຄັອກໂຄລິດໄດໂນເສົາແມ່ແບບ:Phanerozoic eonໝວດໝູ່:ທໍລະນີວິທະຍາໝວດໝູ່:ຍຸກຄຣີເຕຊຽດໝວດໝູ່:ມະຫາຍຸກມີໂຊໂຊອິກແມ່ແບບ:ໂຄງທໍລະນີວິທະຍາ












ຍຸກຄຣີເຕຊຽດ




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ແມ່ແບບ:ຍຸກທາງທໍລະນີ


ຍຸກຈູແຣດຊິກ←ຍຸກຄຣີເຕຊຽດ→ຍຸກພາລີໂອຈີນ


ຍຸກຄຣີເຕຊຽດ (ອັງກິດ: Cretaceous) ເປັນຍຸກໜຶ່ງທາງທໍລະນີການຂອງໂລກ ຢູ່ໃນມະຫາຍຸກມີໂຊໂຊອິກ. ຍຸກຕຣີເຕຊຽດຢູ່ຖັດຈາກຍຸກຈູແຣດຊິກ ຄືປະມານ 145.5 ± 4.0 ລ້ານປີກ່ອນ ແລະ ຢູ່ກ່ອນໜ້າຍຸກພາລີໂອຈີນ ຫຼື ປະມານ 65.5 ລ້ານປີກ່ອນເຖິງ 23.03 ລ້ານປີກ່ອນ, ຖືເປັນຍຸກທີ່ຍາວນານທີ່ສຸດ ແແລະ ກິນເວລາເກືອບເຄິ່ງໜຶ່ງຂອງມະຫາຍຸກມີໂຊໂຊອິກ. ຈຸດສິ້ນສຸດຂອງຍຸກຄຣີເຕຊຽສເປັນຮອຍຕໍ່ລະຫວ່າງ ມະຫາຍຸກມີໂຊໂຊອິກກັບມະຫາຍຸກຊີໂນໂຊອິກ.


ຊື່ ຄຣີເຕຊຽດ ມາຈາກພາສາລາແຕັງ, creta ແປວ່າຫີນປູນ. ຍຸກນີ້ກຳນົດໂດຍນັກທໍລະນີວິທະຍາຊາວແບນຊິກ, ຊອງ ໂດມາລິວ ດັນລົວ (Jean d'Omalius d'Halloy) ເມື່ອ ຄສ 1822 ໂດຍອາໄສຊັ້ນຫີນໃນແອ່ງປາຣີ ແລະ ຕັ້ງຊື່ດັ່ງກ່າວຈາກປະລິມານຫີນປູນ ເຊິ່ງເປັນການຊີກາກໂບນັດຈາກເປືອກຂອງສັດບໍ່ມີກະດູກສັນຫຼັງໃນທະເລ ໂດຍສະເພາະແມ່ນຄັອກໂຄລິດ ທີ່ພົບໃນຍຸກຄຣີເຕຊຽດຕອນປາຍໃນທະວີບເອີຣົບ ແລະ ເກາະອັງກິດ. ຍຸກຄຣີເຕຊຽດເປັນຍຸກທີ່ຮູ່ງເຮືອງທີ່ສຸດຂອງໄດໂນເສົາ ແລະ ເມື່ອປາຍຍຸກຄຣີເຕຊຽດເມື່ອ 65 ລ້ານປີກ່ອນ ໄດ້ເກີດການສູນພັນຄັ້ງໃຫຍ່ທີ່ເຮັດໃຫ້ສິ່ງທີ່ມີຊີວິດເຖິງ 94% ສູນພັນ ຊຶ່ງຮວມທັງໄດໂນເສົາດ້ວຍ.



ອ້າງອີງ





ແຫຼ່ງຂໍ້ມູນອື່ນ


  • UCMP Berkeley Cretaceous page

  • Bioerosion website at The College of Wooster

ແມ່ແບບ:Phanerozoic eon




ໝວດໝູ່:ທໍລະນີວິທະຍາ
ໝວດໝູ່:ຍຸກຄຣີເຕຊຽດ
ໝວດໝູ່:ມະຫາຍຸກມີໂຊໂຊອິກ
ແມ່ແບບ:ໂຄງທໍລະນີວິທະຍາ









ດຶງຂໍ້ມູນຈາກ "https://lo.wikipedia.org/w/index.php?title=ຍຸກຄຣີເຕຊຽດ&oldid=51491"










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