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Showing 1–7 of 7 results

Advanced filters: Author: Yebo Liu Clear advanced filters

Orbital forcing of ice sheets during snowball Earth

Reconciling the Snowball Earth hypothesis with sedimentological cyclicity has been a persistent challenge. A new cyclostratigraphic climate record for a Cryogenian banded iron formation in Australia provides evidence for orbital forcing of ice sheet advance and retreat cycles during Snowball Earth.

Ross N. Mitchell
Thomas M. Gernon
Xiaofang He
ResearchOpen Access07 Jul 2021
Nature Communications

Volume: 12, P: 1-9
Emplacement of the Argyle diamond deposit into an ancient rift zone triggered by supercontinent breakup

The Argyle deposit erupted 1.3 billion years ago into an ancient rift at the edge of a craton. Argyle coincided with supercontinent breakup, highlighting the link between diamond emplacement, former rifts and continental breakup.

Hugo K. H. Olierook
Denis Fougerouse
Michael T. D. Wingate
ResearchOpen Access19 Sept 2023
Nature Communications

Volume: 14, P: 1-10
A Palaeoproterozoic tectono-magmatic lull as a potential trigger for the supercontinent cycle

Earth experienced a lull in magmatic and tectonic activity about 2.3 billion years ago, followed by a flare-up of magmatism, according to a compilation of existing geologic data. These events might mark the transition to the supercontinent cycle.

Christopher J. Spencer
J. Brendan Murphy
Ross N. Mitchell
Reviews29 Jan 2018
Nature Geoscience

Volume: 11, P: 97-101
Linc00423 as a tumor suppressor in retroperitoneal liposarcoma via activing MAPK signaling pathway through destabilizing of NFATC3

Yong Zhang
Hanxing Tong
Yuhong Zhou
ResearchOpen Access03 Jun 2019
Cell Death & Disease

Volume: 10, P: 1-13
First Precambrian palaeomagnetic data from the Mawson Craton (East Antarctica) and tectonic implications

Yebo Liu
Zheng-Xiang Li
Martin Hand
ResearchOpen Access06 Nov 2018
Scientific Reports

Volume: 8, P: 1-12
The supercontinent cycle

Repeated amalgamation and dispersal of continents over Earth history is known as the supercontinent cycle; however, the geodynamic processes driving this cyclicity remain debated. This Review synthesizes observations, plate reconstructions and geodynamic models of supercontinent, and older Archaean supercraton, cycles.

Ross N. Mitchell
Nan Zhang
Zheng-Xiang Li
Reviews20 Apr 2021
Nature Reviews Earth & Environment

Volume: 2, P: 358-374
Weak orogenic lithosphere guides the pattern of plume-triggered supercontinent break-up

The location of orogenic belts has a strong influence on the rifting of supercontinents after mantle plumes trigger the initial break-up and contribute to lithospheric weakening, according to numerical simulations of the break-up of Pangea.

Zhuo Dang
Nan Zhang
Yebo Liu
ResearchOpen Access19 Nov 2020
Communications Earth & Environment

Volume: 1, P: 1-11