在科罗拉多州的一个热带雨林,距离白纪-三级纪的边界1.4百万年后
1Department of Earth Sciences, Denver Museum of Nature & Science, Denver, CO 80205, USA. kjohnson@dmns.org
概括
科罗拉多州一个多样化的低旧世化石叶片遗址揭示了意想不到的热带雨林在白三世灭绝事件后仅在140万年内勃发展. 这一发现挑战了以前关于灭绝后植物恢复的假设.
科学领域:
- 古植物学是古植物学.
- 古气候学 古气候学
- 地质地质地质地质地质地
背景情况:
- 甲-三世 (K-T) 灭绝事件对全球动植物产生了重大影响,导致了物种贫困的古世植物群落.
- 以前的理解认为,古世植物的低多样性归因于K-T灭绝的后果.
研究的目的:
- 为了调查在科罗拉多州的卡斯尔洛克发现的异常多样化的低旧世化石叶片遗址.
- 了解K-T边界后不久支持高多样性热带雨林生态系统的环境条件.
主要方法:
- 来自城堡岩石遗址的化石叶子垃圾分析.
- 化石植物与现存的赤道雨林垃圾的比较.
- 丹佛盆地和拉拉迈德前沿山脉的地质上下文分析.
主要成果:
- 城堡岩遗址展示了极其多样化的化石垃圾,相当于现代赤道雨林.
- 这种高度多样化的植物大约存在于64.1亿年前,在K-T边界140万年之内.
- 雨林位于丹佛盆地边缘,位于同源沉积岩中.
结论:
- 拉拉米德前线山脉创造的当地地理条件,加上平衡的气候,促进了热带雨林的建立.
- 这些发现表明,本地化的环境因素,而不是广泛的灭绝后恢复,允许这个地区的早期古世雨林.
更多相关视频
08:09Measuring and Mapping Patterns of Soil Erosion and Deposition Related to Soil Carbonate Concentrations Under Agricultural Management
Published on: September 12, 2017
10:14Reconstructing Terrestrial Paleoclimate and Paleoecology with Fossil Leaves Using Digital Leaf Physiognomy and Leaf Mass Per Area
Published on: October 25, 2024
相关概念视频
Migration
Migration is long-range, seasonal movement from one region or habitat to another. This common strategy, carried out by many different organisms around the world, is an adaptive response that typically corresponds to changes in an organism’s environment, like resource availability or climate. Migrations can involve huge groups of thousands of animals as well as single individuals traveling alone and can range from thousands of kilometers to just a few hundred meters.
Global Climate Change
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
Threats to Biodiversity
There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
Ecological Succession
Ecological succession is influenced by the processes of facilitation, inhibition, and toleration. Facilitation occurs when early successional species create more favorable ecological conditions for subsequent species, such as enhanced nutrient, water, or light availability. In contrast, inhibition happens when early successional species create unfavorable ecological conditions for potential successive species, such as limiting resource availability. In some cases, later successional species...
The Fossil Record
The fossil record documents only a small fraction of all organisms that have ever inhabited Earth. Fossilization is a rare process, and most organisms never become fossils. Moreover, the fossil record only exhibits fossils that have been discovered. Nevertheless, sedimentary rock fossils of long-lived, abundant, hard-bodied organisms dominate the fossil record. These fossils offer valuable information, such as an organism's physical form, behavior, and age. Studying the fossil record helps...
Rab Cascades
Rab GTPases act in a regulated cascade during membrane fusion, helping the lipid bilayers mix. The Rab family of proteins are active when bound to GTP, and inactive when bound to GDP. Hence, they act as guanine nucleotide-dependent molecular switches. Rab-GTP recognizes and binds to long or short-range tethering proteins to capture the target vesicle. These tethers coordinate with SNAREs on the vesicle and the target membrane to assemble the trans SNARE complex that locks the mixing bilayers.
