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- W4387009898 abstract "The ~2,000-km-long Central Range of New Guinea is a hotspot of modern carbon sequestration due to the chemical weathering of igneous rocks with steep topography in the warm wet tropics. These high mountains formed in a collision between the Australian plate and ophiolite-bearing volcanic arc terranes, but poor resolution of the uplift and exhumation history has precluded assessments of the impact on global climate change. Here, we develop a palinspastic reconstruction of the Central Range orogen with existing surface geological constraints and seismic data to generate time–temperature paths and estimate volumes of eroded material. New (U-Th)/He thermochronology data reveal rapid uplift and regional denudation between 10 and 6 Mya. Erosion fluxes from the palinspastic reconstruction, calibrated for time with the thermochronological data, were used as input to a coupled global climate and weathering model. This model estimates 0.6 to 1.2 °C of cooling associated with the Late Miocene rise of New Guinea due to increased silicate weathering alone, and this CO 2 sink continues to the present. Our data and modeling experiments support the hypothesis that tropical arc-continent collision and the rise of New Guinea contributed to Neogene cooling due to increased silicate weathering." @default.
- W4387009898 created "2023-09-26" @default.
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- W4387009898 date "2023-09-25" @default.
- W4387009898 modified "2023-10-11" @default.
- W4387009898 title "The rise of New Guinea and the fall of Neogene global temperatures" @default.
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- W4387009898 doi "https://doi.org/10.1073/pnas.2306492120" @default.
- W4387009898 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/37748068" @default.
- W4387009898 hasPublicationYear "2023" @default.
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