地球の「失われた」10億年:大不整合と初期の地殻変動を結びつける研究(Earth’s “Missing” Billion Years: Study Links the Great Unconformity to Early Tectonics)

2026-03-11 コロンビア大学

コロンビア大学の研究は、地球史における「失われた10億年」と呼ばれる大不整合の形成原因を初期プレートテクトニクスに結び付けた。大不整合は、広範囲で地層が欠落している現象で、その起源は長年議論されてきた。本研究では地質データと年代解析を統合し、約10億年前に大陸衝突や山脈形成が進行し、侵食が大規模に進んだ結果、地層が削剥されたと結論づけた。これにより、初期のプレート運動が地表環境や地殻進化に大きな影響を与えたことが示され、地球の進化史理解に重要な知見を提供する。

<関連情報>

大不整合の原因は、「スノーボールアース」と呼ばれる氷河作用ではなく、地殻変動である Tectonism rather than “snowball Earth” glaciation is responsible for the Great Unconformity

Rong-Ruo Zhan , Liang Duan , Massimiliano Zattin, +8 , and Xingliang Zhang
Proceedins of the National Academy of Sciences  Published:February 23, 2026
DOI:https://doi.org/10.1073/pnas.2523891123

地球の「失われた」10億年:大不整合と初期の地殻変動を結びつける研究(Earth’s “Missing” Billion Years: Study Links the Great Unconformity to Early Tectonics)

Significance

The Great Unconformity (GUn) is arguably the most iconic but enigmatic gap in Earth’s stratigraphic record. Among puzzling features requiring explanation is evidence for many kilometers of exhumation and a hiatus of hundreds of millions to billions of years in continental interiors. Existing models call for either a glacial or a plate tectonic origin in the Neoproterozoic. We provide evidence that erosion below the unconformity was protracted in North China, and that the most pronounced erosion at a global scale occurred during the late Paleoproterozoic and was driven by tectonics associated with supercontinent cycle of Columbia.

Abstract

The Great Unconformity (GUn)—a widely recognized discontinuity and associated gap in the rock record between Precambrian and Cambrian rocks—represents a globally important interval of continental exposure and erosion that is notable also for the first appearance of all major animal phyla on Earth. However, its origin remains the subject of vigorous debate. Here, we present field relationships, and zircon and monazite U–Pb, biotite and muscovite Rb–Sr, and zircon (U–Th)/He thermochronology data for Precambrian crystalline basement rocks from North China to constrain the exhumation history below the unconformity. Dates from multichronometers and thermal history inversions show that the most substantial cooling of continental basement took place from ~2,100 to 1,600 Ma. Comparison with thermal history data from Laurentia, Baltica, and Amazonia suggests that protracted plate tectonics broadly modulated by supercontinent cycles, and not “snowball Earth” glaciation, is responsible for crustal exhumation below the unconformity. The most pronounced erosion evident in both the thermochronologic record and geochemical indicators of continental weathering is shown to correspond with development of Earth’s first true supercontinent (Columbia), rather than with either the Cambrian explosion or the emergence of modern plate tectonics.

1703地質
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