carboniferous

简明释义

英[ˌkɑːbəˈnɪfərəs]美[ˌkɑːrbəˈnɪfərəs]

adj. 石炭纪的，石炭系的

n. 石炭纪，石炭层

英英释义

单词用法

同义词

反义词

例句

1.The analysis of sedimentary formation suggests the existence of groove-arc-basin system at the middle Carboniferous.

结合上述事实，通过沉积建造分析，该区在中石炭统曾存在沟弧盆体系。

2.The Liangshang Formation mudstone is the direct cap rock of the Carboniferous gas pools.

石炭系气藏的直接盖层是下二叠统梁山组泥岩层。

3.The strata are mainly Middle-Lower Carboniferous.

出露地层为中下石炭统；

4.Silurian '. 'and before the Mississippian or Carboniferous Period, and characterized by the appearance of forests and amphibians.

处于志留记之后，密西西比纪或石炭纪之前，森林和两栖类的出现是其特征。

5.The Permo Carboniferous is the main coal bearing strata in Henan Province.

石炭—二叠纪地层是河南省主要含煤地层。

6.Diagenesis had some effects to the developing of pore of carboniferous volcanic reservoir in SHIXI.

成岩作用对石西石炭系火山岩储集层孔隙的发育具有一定的影响。

7.Geologists study carboniferous 石炭纪 strata to understand the Earth's geological history.

地质学家研究石炭纪地层以了解地球的地质历史。

8.The rocks in this area are predominantly from the carboniferous 石炭纪 period, which is known for its extensive coal deposits.

这个地区的岩石主要来自石炭纪，以其丰富的煤矿储量而闻名。

9.Many fossils found in carboniferous 石炭纪 rock layers provide insights into ancient ecosystems.

在石炭纪岩层中发现的许多化石为古代生态系统提供了见解。

10.The carboniferous 石炭纪 was a time when Earth's climate was much warmer than today.

在石炭纪时期，地球的气候比今天温暖得多。

11.During the carboniferous 石炭纪, vast swampy forests thrived, leading to the formation of significant fossil fuels.

在石炭纪期间，广阔的沼泽森林繁荣生长，导致了重要化石燃料的形成。

作文

The term carboniferous refers to a significant geological period that occurred approximately 359 to 299 million years ago. This era is renowned for its vast forests of giant ferns and the formation of extensive coal deposits, which is where the name carboniferous originates, derived from Latin words meaning 'coal-bearing'. The carboniferous period is crucial in understanding the Earth's history, particularly in terms of climate change, biodiversity, and the evolution of life on our planet.During the carboniferous period, the Earth experienced a warm and humid climate that fostered the growth of lush vegetation. These dense forests played a vital role in sequestering carbon dioxide from the atmosphere, which contributed to a significant reduction in greenhouse gases. As plants died and fell into swamps, their decomposition was hindered by waterlogged conditions, leading to the accumulation of organic material. Over millions of years, this process resulted in the formation of coal, a critical energy source for humanity today.The rich biodiversity of the carboniferous period also marked a pivotal point in the evolution of terrestrial ecosystems. It was during this time that amphibians began to thrive, evolving from their fish ancestors. Additionally, the first reptiles appeared, paving the way for the dominance of reptiles in later geological periods. The carboniferous period was not only about plant life; it also saw the emergence of various invertebrates and early forms of vertebrates, showcasing an explosion of life forms that would shape future ecosystems.Geologically, the carboniferous period is divided into two main epochs: the Mississippian and the Pennsylvanian. Each epoch is characterized by distinct rock formations and fossil records. The Mississippian epoch is known for its limestone deposits, while the Pennsylvanian epoch is famous for its coal beds. These differences in sedimentation and fossilization provide valuable insights into the environmental conditions of the time.The legacy of the carboniferous period extends beyond its geological significance. The coal deposits formed during this time have been a cornerstone of industrial development, fueling the steam engines of the Industrial Revolution and continuing to provide energy today. However, the reliance on fossil fuels has raised concerns about climate change and environmental degradation. Understanding the carboniferous period helps us appreciate the delicate balance between natural processes and human activities.In conclusion, the carboniferous period is a fascinating chapter in Earth's history that highlights the interplay between climate, life, and geology. By studying this era, we gain a deeper understanding of how past events shape our present and future. The lessons learned from the carboniferous period remind us of the importance of preserving our environment and finding sustainable ways to harness natural resources. As we face contemporary challenges such as climate change, the knowledge gained from this remarkable geological period can guide our efforts towards a more sustainable future.

“碳iferous”一词指的是大约3.59亿到2.99亿年前的一个重要地质时期。这个时代以其巨型蕨类植物的广阔森林和广泛的煤炭沉积而闻名，这就是“碳iferous”这个名称的来源，源于拉丁语，意为“含煤的”。“碳iferous”时期在理解地球历史方面至关重要，特别是在气候变化、生物多样性和生命演化方面。在“碳iferous”时期，地球经历了温暖潮湿的气候，这促进了丰盛植被的生长。这些茂密的森林在从大气中封存二氧化碳方面发挥了重要作用，这有助于温室气体的显著减少。当植物死亡并掉入沼泽时，由于水淹条件的阻碍，它们的分解受到抑制，导致有机物质的积累。在数百万年的过程中，这一过程导致了煤的形成，这是人类今天的重要能源。“碳iferous”时期丰富的生物多样性也标志着陆地生态系统演化的关键点。正是在这个时期，两栖动物开始繁荣，进化自它们的鱼类祖先。此外，第一批爬行动物出现，为后来的爬行动物主导地位铺平了道路。“碳iferous”时期不仅关乎植物生命；它还见证了各种无脊椎动物和早期脊椎动物的出现，展示了将塑造未来生态系统的生命形式的爆炸性增长。在地质上，“碳iferous”时期分为两个主要纪元：密西西比纪元和宾夕法尼亚纪元。每个纪元都有其独特的岩层和化石记录。密西西比纪元以其石灰岩沉积而闻名，而宾夕法尼亚纪元则以其煤层而著称。这些沉积和化石化过程的差异为我们提供了关于当时环境条件的宝贵见解。“碳iferous”时期的遗产超越了其地质意义。在这一时期形成的煤炭沉积是工业发展的基石，为工业革命的蒸汽机提供动力，并继续为今天提供能源。然而，对化石燃料的依赖引发了对气候变化和环境退化的担忧。理解“碳iferous”时期帮助我们欣赏自然过程与人类活动之间的微妙平衡。总之，“碳iferous”时期是地球历史上一个迷人的章节，突显了气候、生命和地质之间的相互作用。通过研究这一时代，我们更深入地理解过去事件如何塑造我们的现在和未来。从“碳iferous”时期获得的教训提醒我们保护环境的重要性，以及寻找可持续利用自然资源的方法。面对气候变化等当代挑战，从这一显著的地质时期获得的知识可以指导我们朝着更可持续的未来努力。