Corals are unique in the suite of proposed Anthropocene Global Boundary Stratotype Section and Point (GSSP) archives, as living organisms that produce aragonite exoskeletons preserved geological record contain highly accurate precise (<±1 year) internal chronologies. The GSSP candidate site North Flinders Reef Coral Sea (Australia) is an offshore oceanic reef, therefore less vulnerable to lo...

INTegration of Ice-core, MArine and TErrestrial records (INTIMATE) is a core project of the INQUA Palaeoclimate Commission, the primary goal of which is to synchronise records of the Last Glacial–Interglacial Transition (LGIT). Through a series of international workshops, INTIMATE has encouraged direct collaboration between scientists with interests and expertise in a wide range of palaeoenviro...

The Middle–Late Triassic climates have attracted the attention of paleontological and geological scientists for Carnian pluvial event in early Late Triassic. is well-documented pelagic epi-continental marine deposits Tethys, Gondwana, Laurasia. However, inland terrestrial are less frequently depicted, with high-resolution palynological biostratigraphy constraints. In this study, we report recor...

The Cretaceous/Paleogene (K/Pg) boundary is marked by one of the largest mass extinctions in Earth’s history, with geological evidence for this event being expressed hundreds locations worldwide. An extensively studied section located near El Kef, northwestern Tunisia, characterized classic iridium-rich K/Pg layer, abundant and well-preserved microfossils, apparently continuous sedimentation th...

Abstract The Chiba composite section (CbCS) in the Kokumoto Formation, Kazusa Group, central Japan is a thick and continuous marine succession that straddles Lower–Middle Pleistocene boundary well-recognized Matuyama–Brunhes paleomagnetic polarity boundary. Although recent studies extensively investigated CbCS, its chemostratigraphy, particularly around boundary, poorly understood. Therefore, t...