Late Carboniferous

简明释义

晚石炭世;

英英释义

例句

1.The fossils found in this region date back to the Late Carboniferous 晚石炭纪, indicating a rich ecosystem.

该地区发现的化石可以追溯到晚石炭纪晚石炭纪，表明这里曾有丰富的生态系统。

2.The climate during the Late Carboniferous 晚石炭纪 was characterized by high humidity and extensive swampy areas.

在晚石炭纪晚石炭纪期间，气候特征是高湿度和广泛的沼泽地区。

3.The Late Carboniferous 晚石炭纪 is known for the formation of massive coal seams.

晚石炭纪晚石炭纪以形成大规模煤层而著称。

4.Many of the plants we see today evolved from species that thrived in the Late Carboniferous 晚石炭纪 forests.

我们今天看到的许多植物都是从在晚石炭纪晚石炭纪森林中繁盛的物种演变而来的。

5.Geologists have identified several coal deposits from the Late Carboniferous 晚石炭纪 period.

地质学家已经识别出几个来自晚石炭纪晚石炭纪时期的煤矿床。

作文

The geological period known as the Late Carboniferous is a crucial chapter in Earth's history, spanning from approximately 318 to 299 million years ago. During this time, the planet underwent significant changes that shaped its biodiversity and geological features. The Late Carboniferous is characterized by the formation of extensive coal deposits, which are remnants of lush, tropical forests that thrived in the warm and humid climate of the time. These forests were primarily composed of gigantic ferns, horsetails, and seed plants, creating a rich ecosystem that supported a wide variety of life.One of the most notable aspects of the Late Carboniferous is the dramatic increase in terrestrial plant life. This period saw the rise of large-scale forests that not only contributed to the oxygen levels in the atmosphere but also played a vital role in the carbon cycle. As these plants died and accumulated, they eventually transformed into coal, which we still rely on as a significant energy source today. The vast coal beds formed during this period are among the largest and most economically important in the world.In addition to the flourishing plant life, the Late Carboniferous was also marked by diverse animal life. Amphibians became more prominent, and early reptiles began to emerge, adapting to the changing environments. The evolution of these creatures laid the groundwork for future terrestrial vertebrates. Fossil records from the Late Carboniferous indicate a variety of insects, including some of the largest known species, showcasing the rich biodiversity of the era.Geologically, the Late Carboniferous was a time of significant tectonic activity. The supercontinent Pangaea began to form, resulting in the collision of landmasses and the creation of mountain ranges. This tectonic movement influenced ocean currents and climate patterns, further shaping the environment in which both plants and animals thrived. The climatic conditions during the Late Carboniferous were conducive to the development of extensive swampy areas, which later contributed to the formation of coal deposits.As we study the Late Carboniferous, we gain valuable insights into the Earth's past and the evolutionary processes that have led to the current biodiversity we see today. Understanding this period helps scientists predict how ecosystems might respond to contemporary environmental changes. The legacy of the Late Carboniferous continues to impact us, not only through the fossil fuels we extract but also through the lessons learned about ecological balance and sustainability.In conclusion, the Late Carboniferous represents a pivotal moment in Earth's geological and biological history. From its lush forests and diverse animal life to the significant geological transformations that occurred, this period has left an indelible mark on our planet. Studying the Late Carboniferous allows us to appreciate the complexity of life and the interconnectedness of various environmental factors, reminding us of the importance of preserving our natural world for future generations.

被称为晚石炭纪的地质时期是地球历史中的一个重要章节，约从3.18亿年前到2.99亿年前。在此期间，地球经历了重大变化，塑造了其生物多样性和地质特征。晚石炭纪的特点是形成了广泛的煤矿，这些煤矿是当时繁茂热带森林的遗迹，这些森林在温暖潮湿的气候中蓬勃发展。这些森林主要由巨型蕨类植物、马尾草和种子植物组成，创造了一个丰富的生态系统，支持着各种生命。晚石炭纪最显著的方面之一是陆地植物生命的戏剧性增加。这个时期见证了大规模森林的兴起，这些森林不仅有助于提高大气中的氧气水平，还在碳循环中发挥了重要作用。随着这些植物的死亡和积累，它们最终转化为煤炭，而我们今天仍然依赖这种重要的能源来源。这个时期形成的广阔煤层是世界上最大和最经济重要的煤层之一。除了繁荣的植物生命，晚石炭纪还以动物生命的多样性而闻名。两栖动物变得更加突出，早期爬行动物开始出现，适应不断变化的环境。这些生物的进化为未来的陆生脊椎动物奠定了基础。来自晚石炭纪的化石记录显示出多种昆虫，包括一些已知的最大物种，展示了这个时代的丰富生物多样性。在地质上，晚石炭纪是一个重大构造活动的时期。超级大陆潘吉亚开始形成，导致陆地块的碰撞和山脉的形成。这种构造运动影响了海洋洋流和气候模式，进一步塑造了植物和动物繁盛的环境。在晚石炭纪期间的气候条件有利于广泛沼泽地区的发展，这些地区后来又促进了煤矿的形成。随着我们对晚石炭纪的研究，我们获得了对地球过去及其演化过程的宝贵见解，这些过程导致了今天我们所看到的生物多样性。理解这一时期有助于科学家预测生态系统如何应对当代环境变化。晚石炭纪的遗产继续影响着我们，不仅通过我们提取的化石燃料，也通过我们对生态平衡和可持续性的重要性的认识。总之，晚石炭纪代表了地球地质和生物历史中的一个关键时刻。从其繁茂的森林和多样的动物生命到发生的重大地质变革，这一时期在我们的星球上留下了不可磨灭的印记。研究晚石炭纪使我们能够欣赏生命的复杂性和各种环境因素的相互联系，提醒我们保护自然世界的重要性，以造福未来的世代。