アケア上層地殻のマフィックからフェルシックへの移行は,プレート構造の始まりを示しています
Ming Tang1, Kang Chen2, Roberta L Rudnick3
1Department of Geology, University of Maryland, College Park, MD 20742, USA. Corresponding author.
まとめ
古代のエオンは,初期の大陸の殻がマフィックからフェルシックに進化した. この変化は地殻の質量の増加によって示され,約30億年前の地球板構造の始まりを示唆しています.
科学分野:
- 地質学
- 地化学
- 初期の地球科学
背景:
- 古代エオン (4.02.5億年前) は,初期の大陸の地殻形成と生命の出現に決定的であった.
- 大陸地殻の初期構成は,その後の地質学的プロセスにより,ほとんど理解されていません.
- 初期の地殻の進化を理解することは 地球の初期の歴史を解読する鍵です
研究 の 目的:
- 古代大陸の上層層のMgO組成を再構築する.
- 初期の大陸地殻の構成の変化のタイミングを 決定する.
- 地殻の進化と プレート構造の発生の関係を調べる
主な方法:
- 古代土着の堆積岩におけるNi/CoとCr/Zn比の分析
- 古代の岩石と岩石の分析
- 大陸地殻上部のMgO組成の地球化学的追跡
主要な成果:
- 古代大陸の上層層は,マフィックからフェルシックの大量組成に進化した. それは30億年から25億年前.
- この期間中に上部大陸の質量が5倍に増加した.
- 砂岩の追加が地殻の質量増加に大きく貢献した.
結論:
- 古代の地殻の組成の進化は,マグマの過程における重要な変化を示しています.
- 地殻の質量の大幅な増加は,地殻生成率の向上を示唆しています.
- この発見は地球板構造が 約30億年前に始まったという仮説を裏付けています
関連する概念動画
Conditions on Early Earth
2.9K
2.9K
Conditions on Early Earth
103.2K
Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
103.2K
The Fossil Record
28.4K
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...
28.4K
The Colonization of Land
38.6K
Changes in the environment of the early Earth drove the evolution of organisms. As prokaryotic organisms in the oceans began to photosynthesize, they produced oxygen. Eventually, oxygen saturated the oceans and entered the air, resulting in an increase in atmospheric oxygen concentration, known as the oxygen revolution approximately 2.3 billion years ago. Therefore, organisms that could use oxygen for cellular respiration had an advantage. More than 1.5 years ago, eukaryotic cells and...
38.6K
Overview of Archaea
1.6K
Archaea, named after the Archaean eon, represent a unique domain of life, distinct from bacteria and eukaryotes, with remarkable traits. Their cellular and molecular features, ecological adaptability, and industrial relevance highlight their importance in understanding life processes and leveraging biotechnology.Cellular and Molecular CharacteristicsA defining feature of archaea is their unique membrane composition. Archaeal membranes contain ether-linked isoprenoid lipids, which confer...
1.6K
Formation of the Platelet Plug
10.6K
The platelet phase, the second stage of hemostasis, commences around 15-20 seconds after an injury. It follows and overlaps with the vascular phase, during which blood vessels constrict to minimize blood loss.
As the injured blood vessel contracts, endothelial cells undergo contraction, revealing collagen fibers in the basement membrane and underlying connective tissue. Furthermore, the plasma membrane of endothelial cells becomes adhesive, preparing the site for platelet adhesion. Platelets...
As the injured blood vessel contracts, endothelial cells undergo contraction, revealing collagen fibers in the basement membrane and underlying connective tissue. Furthermore, the plasma membrane of endothelial cells becomes adhesive, preparing the site for platelet adhesion. Platelets...
10.6K


