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本文引用的文献

1
Spatial niche partitioning in dinosaurs from the latest cretaceous (Maastrichtian) of North America.北美洲最晚白垩纪(马斯特里赫特阶)恐龙的空间生态位分化。
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2
Cretaceous extinctions: multiple causes.白垩纪大灭绝:多种原因
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3
The Chicxulub asteroid impact and mass extinction at the Cretaceous-Paleogene boundary.希克苏鲁伯小行星撞击与白垩纪-古近纪之交的大灭绝。
Science. 2010 Mar 5;327(5970):1214-8. doi: 10.1126/science.1177265.
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Extraterrestrial cause for the cretaceous-tertiary extinction.外星原因导致白垩纪-第三纪灭绝。
Science. 1980 Jun 6;208(4448):1095-108. doi: 10.1126/science.208.4448.1095.
5
Disruption of the terrestrial plant ecosystem at the cretaceous-tertiary boundary, Western interior.白垩纪-第三纪界线时陆地植物生态系统的破坏,内陆西部。
Science. 1984 Sep 7;225(4666):1030-2. doi: 10.1126/science.225.4666.1030.

恐龙灭绝:填补“300 万年的空白”。

Dinosaur extinction: closing the '3 m gap'.

机构信息

Department of Geology and Geophysics, Yale University, New Haven, CT 06511, USA.

出版信息

Biol Lett. 2011 Dec 23;7(6):925-8. doi: 10.1098/rsbl.2011.0470. Epub 2011 Jul 13.

DOI:10.1098/rsbl.2011.0470
PMID:21752814
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3210679/
Abstract

Modern debate regarding the extinction of non-avian dinosaurs was ignited by the publication of the Cretaceous-Tertiary (K-T) asteroid impact theory and has seen 30 years of dispute over the position of the stratigraphically youngest in situ dinosaur. A zone devoid of dinosaur fossils reported from the last 3 m of the Upper Cretaceous, coined the '3 m gap', has helped drive controversy. Here, we report the discovery of the stratigraphically youngest in situ dinosaur specimen: a ceratopsian brow horn found in a poorly rooted, silty, mudstone floodplain deposit located no more than 13 cm below the palynologically defined boundary. The K-T boundary is identified using three criteria: (i) decrease in Cretaceous palynomorphs without subsequent recovery, (ii) the existence of a 'fern spike', and (iii) correlation to a nearby stratigraphic section where primary extraterrestrial impact markers are present (e.g. iridium anomaly, spherules, shocked quartz). The in situ specimen demonstrates that a gap devoid of non-avian dinosaur fossils does not exist and is inconsistent with the hypothesis that non-avian dinosaurs were extinct prior to the K-T boundary impact event.

摘要

现代关于非鸟类恐龙灭绝的争论是由白垩纪-第三纪(K-T)小行星撞击理论的发表引发的,这场争论已经持续了 30 年,争论的焦点是地层中最年轻的恐龙化石的位置。在白垩纪末期,报道了一个没有恐龙化石的区域,被称为“3 米空白”,这一现象加剧了争议。在这里,我们报告了发现了地层中最年轻的恐龙化石标本:一个角龙的眉骨化石,它位于一个根系不发达的粉砂质泥岩漫滩沉积物中,距离孢粉学定义的边界不超过 13 厘米。K-T 边界是通过三个标准来确定的:(i)白垩纪孢粉类生物数量减少,且没有后续恢复,(ii)存在“蕨类 spike”,以及(iii)与附近的地层剖面相关,该剖面存在主要的天外撞击标记(如铱异常、球粒、冲击石英)。该原位标本表明,不存在没有非鸟类恐龙化石的空白区域,这与非鸟类恐龙在 K-T 边界撞击事件之前就已经灭绝的假说不一致。