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相关概念视频

Global Climate Change01:50

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 Biodiversity01:50

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...
Predator-Prey Interactions02:39

Predator-Prey Interactions

Predators consume prey for energy. Predators that acquire prey and prey that avoid predation both increase their chances of survival and reproduction (i.e., fitness). Routine predator-prey interactions elicit mutual adaptations that improve predator offenses, such as claws, teeth, and speed, as well as prey defenses, including crypsis, aposematism, and mimicry. Thus, predator-prey interactions resemble an evolutionary arms race.
Conservation of Small Populations02:04

Conservation of Small Populations

Small population sizes put a species at extreme risk of extinction due to a lack of variation, and a consequent decrease in adaptability. This weakens the chances of survival under pressures such as climate change, competition from other species, or new diseases. Large populations are more likely to survive pressures such as these, as such populations are more likely to harbor individuals that have genetic variants that are adaptive under new stresses. Small populations are much less likely to...
What is Evolutionary History?02:35

What is Evolutionary History?

Scientists record evolutionary history by analyzing fossil, morphological, and genetic data. The fossil record documents the history of life on Earth and provides evidence for evolution. However, both fossil and living organisms offer evidence that outlines Earth’s evolutionary history.
The Fossil Record02:56

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...

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Holocene Refugium of Shrubby Birch Betula humilis Schrank and Avens Dryas sp. in Kazakh Uplands.

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Find of Eggs of the Trematode Echinochasmus sp. (Trematoda, Echinochasmidae) in the Late Holocene of Northwestern Siberia.

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Find of Eggs of the Nematode Dioctophyme renale (Goeze, 1782) (Nematoda, Dioctophymidae) from the Late Holocene of Northwestern Siberia.

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相关实验视频

Updated: May 11, 2026

A Noninvasive Hair Sampling Technique to Obtain High Quality DNA from Elusive Small Mammals
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A Noninvasive Hair Sampling Technique to Obtain High Quality DNA from Elusive Small Mammals

Published on: March 13, 2011

在巨型鹿和羊毛猛象中,普世到全新世的灭绝动态.

A J Stuart1, P A Kosintsev, T F G Higham

  • 1Department of Biology, University College London, London WC1E 6BT, UK. Tony@megafauna.freeserve.co.uk

Nature
|October 8, 2004
PubMed
概括

大鹿 (爱尔兰鹿) 在西伯利亚生存到7700年前,挑战了以前的灭绝时间表. 它们的生存和分布变化受到全新纪气候和植被变化的影响,而不仅仅是普莱斯托纪事件.

科学领域:

  • 古生物学的古生物学
  • 四分学科学 四分学科学
  • 古生态学 古生态学

背景情况:

  • 晚期普莱斯托时代巨型动物的灭绝通常归因于人类的过度杀戮或气候变化.
  • 以前的研究表明,欧亚大陆的巨型动物在普世/全新世纪的边界消失了.
  • 最近的发现表明,一些物种的存活时间比以前想象的要晚.

研究的目的:

  • 为了准确地确定巨鹿 (爱尔兰鹿) 的灭绝时间表.
  • 通过检查地理和时间数据,测试有关巨型动物灭绝原因的假设.
  • 了解影响大动物生存和分布变化的生态因素.

主要方法:

  • 放射性碳测年法测定西伯利亚西部巨鹿的遗骸.
  • 对大动物群的地理分布和时间数据的分析.
  • 灭绝模式与气候和植被变化的比较.

主要成果:

  • 巨鹿在西伯利亚西部生存到大约6,900放射性碳年之前 (7,700年前).
  • 这种生存日期比以前接受的时间晚了三千多年.
  • 巨鹿和毛猛都经历了由于气候/植被变化的显著分布变化.

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Protocol for Assessing the Relative Effects of Environment and Genetics on Antler and Body Growth for a Long-lived Cervid
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Protocol for Assessing the Relative Effects of Environment and Genetics on Antler and Body Growth for a Long-lived Cervid

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A Noninvasive Hair Sampling Technique to Obtain High Quality DNA from Elusive Small Mammals

Published on: March 13, 2011

Protocol for Assessing the Relative Effects of Environment and Genetics on Antler and Body Growth for a Long-lived Cervid
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Protocol for Assessing the Relative Effects of Environment and Genetics on Antler and Body Growth for a Long-lived Cervid

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Using Archival Japanese Paper and Thermoplastic Resins to Prepare Fossils for Storage, Display, Transport, and Radiography
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结论:

  • 巨鹿的灭绝很可能发生在全新纪,而不是新纪.
  • 这种物种的灭绝原因必须在Holocene环境背景下考虑.
  • 不同的生态适应影响了巨型鹿和毛猛对环境变化的独特反应.