1.8 billion years of detrital zircon recycling calibrates a refractory part of Earth’s sedimentary cycle

Detrital zircon studies are providing new insights on the evolution of sedimentary basins but the role of sedimentary recycling remains largely undefined. In a broad region of northwestern North America, this contribution traces the pathway of detrital zircon sand grains from Proterozoic sandstones through Phanerozoic strata and argues for multi-stage sedimentary recycling over more than a billion years. As a test of our hypothesis, integrated palynology and detrital zircon provenance provides clear evidence for erosion of Carboniferous strata in the northern Cordillera as a sediment source for Upper Cretaceous strata. Our results help to calibrate Earth's sedimentary cycle by showing that recycling dominates sedimentary provenance for the refractory mineral zircon

Intergenerational inequity: stealing the joy and benefits of nature from our children

No abstract available.The Australia-Africa Universities Network— Partnership Research and Development Fund, a PRIME-DAAD fellowship and the Australian Research Council Linkage Grant. he article processing charge was covered by the Baden-Wuerttemberg Ministry of Science, Research and Art and the University of Freiburg through the funding programme Open Access Publishing.http://frontiersin.org/Ecology_and_Evolutiondm2022Mammal Research InstituteZoology and Entomolog