找回密碼
 To register

QQ登錄

只需一步,快速開始

掃一掃,訪問微社區(qū)

打印 上一主題 下一主題

Titlebook: Geological and Biological Effects of Impact Events; Eric Buffetaut,Christian Koeberl Book 2002 Springer-Verlag Berlin Heidelberg 2002 Biod

[復制鏈接]
41#
發(fā)表于 2025-3-28 15:55:23 | 只看該作者
42#
發(fā)表于 2025-3-28 22:36:13 | 只看該作者
43#
發(fā)表于 2025-3-28 23:09:01 | 只看該作者
44#
發(fā)表于 2025-3-29 04:12:35 | 只看該作者
Effects of the Cretaceous-Tertiary Boundary Event on Bony Fishes,apse of their food chain based on plankton. No extinction of planktivorous families, the intermediate level between plankton and piscivores, is observed. This fact is explain by ecological reasons (representatives of these families were living in brackish or freshwater) and by taxonomical reasons (p
45#
發(fā)表于 2025-3-29 08:53:44 | 只看該作者
,Petrographic and Geochemical Studies in the Cretaceous-Tertiary Boundary, Pernambuco — Paraíba Basion is determined by micropalaentological considerations, stable isotope data, and the presence of phosphatised fragments. Most of the particular characteristics described here, such as the geochemical anomalies (iridium, total organic carbon and fluorine) and the presence of a tsunami deposit, of po
46#
發(fā)表于 2025-3-29 14:12:33 | 只看該作者
Ostracods Prove that the Frasnian/Famennian Boundary Mass Extinction was a Major and Abrupt Crisis, from samples collected close to the Frasnian/Famennian boundary in principal reference sections all over the world. Their study shows that about 75% of all marine species disappeared abruptly close to this boundary.
47#
發(fā)表于 2025-3-29 19:00:48 | 只看該作者
Lateral Variations in End-Permian Organic Matter in Northern Italy,stry of the oceans. The cause of these disturbances remains controversial. One valuable source of information for the end-Permian event is that contained within sedimentary organic matter. We have used organic geochemical methods to investigate end-Permian organic matter in the Dolomites of northern
48#
發(fā)表于 2025-3-29 23:17:18 | 只看該作者
Stable-Isotope and Trace Element Stratigraphy of the Jurassic/Cretaceous Boundary, Bosso River Gorgact structure, was found to have a radiometric age (145 Ma) indistinguishable from the stratigraphic age of the J/K boundary. Thus, it is conceivable that at the boundary, if indeed coeval with this impact structure, a record of the environmental changes associated with the impact event might exist.
49#
發(fā)表于 2025-3-29 23:53:35 | 只看該作者
50#
發(fā)表于 2025-3-30 04:41:06 | 只看該作者
 關于派博傳思  派博傳思旗下網站  友情鏈接
派博傳思介紹 公司地理位置 論文服務流程 影響因子官網 吾愛論文網 大講堂 北京大學 Oxford Uni. Harvard Uni.
發(fā)展歷史沿革 期刊點評 投稿經驗總結 SCIENCEGARD IMPACTFACTOR 派博系數(shù) 清華大學 Yale Uni. Stanford Uni.
QQ|Archiver|手機版|小黑屋| 派博傳思國際 ( 京公網安備110108008328) GMT+8, 2025-10-5 07:43
Copyright © 2001-2015 派博傳思   京公網安備110108008328 版權所有 All rights reserved
快速回復 返回頂部 返回列表
连平县| 东方市| 陆丰市| 衢州市| 建水县| 浮山县| 奉节县| 察哈| 清水河县| 宁阳县| 宿迁市| 石嘴山市| 祁东县| 合肥市| 城固县| 连江县| 江城| 巴彦县| 丰顺县| 西华县| 酒泉市| 陈巴尔虎旗| 吴堡县| 泗阳县| 泽州县| 贵溪市| 浦县| 蓬溪县| 宁夏| 瓦房店市| 尉氏县| 施甸县| 榆林市| 西乡县| 祥云县| 大荔县| 潞西市| 丽水市| 武川县| 南陵县| 五华县|