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地球生命科学(泉 賢太郎)
Showing the original Japanese · View translation
地層と化石から、地球の環境と生物の移り変わりをたどる研究室。

AboutAbout the lab
地層に残る、環境と生物の歴史。
この
過去の
古生物の
化石の
Key terms
- 顕生代
- 約5億4100万年前から
現在までの 地質時代。 生物が 多様化した ことで 特徴づけられる - 生痕化石
- 巣穴・
這った 跡・糞など、 生き物の 活動 その ものが 地層に 残った 化石 - 十脚類
- エビ・
カニ・ ヤドカリなどが 含まれる、 歩く 脚が 10本ある 甲殻類の なかま
ResearchResearch themes
顕生代を
*Illustrative image更新世の北西太平洋の古環境
第四紀更新世の
*Illustrative image生痕化石から読む行動
巣穴や
*Illustrative image十脚類の多様性
エビや
MembersFaculty
- Associate Professor泉 賢太郎
VoicesStudent voices
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Report an errorAbout the images
The top and research theme images are illustrative and were not taken at the lab. They are cropped from Wikimedia Commons images. Cropped CC BY-SA images are provided under the same CC BY-SA license as the original (version shown on each line).
- Top image: “Layers of sedimentary rock formed on the earth's surface. 5034” AlixSaz / CC BY 4.0 (cropped)
- 更新世の
北西太平洋の 古環境: “Bermuda Pleistocene sediments” Alessio Rovere / CC BY-SA 4.0 (cropped) - 生痕化石から
読む 行動: “Diplocraterion trace fossil (Kope Formation, Upper Ordovician; Maysville West roadcut, Mason County, Kentucky, USA) 2” James St. John / CC BY 2.0 (cropped) - 十脚類の
多様性: “Harpactoxanthopsis quadrilobata fossil crab IT” James St. John / CC BY 2.0 (cropped) - Related lab (非線形解析学
(白川 健) ): “Big wave breaking in Santa Cruz” Brocken Inaglory / CC BY-SA 3.0 (cropped) - Related lab (幾何解析、
微分幾何学、 情報幾何学 (前田 瞬) ): “Modell einer Schraubenfläche konstanter negativer Krümmung -Schilling V, 4 - 231” Ramona Trusheim / CC BY-SA 3.0 (cropped)
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