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Integrated records of environmental change and evolution challenge the Cambrian Explosion
Abstract The 'Cambrian Explosion'describes the rapid increase in animal diversity and
abundance, as manifest in the fossil record, between~ 540 and 520 million years ago (Ma) …
abundance, as manifest in the fossil record, between~ 540 and 520 million years ago (Ma) …
Coordinated biotic and abiotic change during the Great Ordovician Biodiversification Event: Darriwilian assembly of early Paleozoic building blocks
Abstract The Ordovician Period records an extraordinary biodiversity increase known as the
Great Ordovician Biodiversification Event (GOBE), which coincided with a series of …
Great Ordovician Biodiversification Event (GOBE), which coincided with a series of …
A high-resolution record of early Paleozoic climate
The spatial coverage and temporal resolution of the Early Paleozoic paleoclimate record are
limited, primarily due to the paucity of well-preserved skeletal material commonly used for …
limited, primarily due to the paucity of well-preserved skeletal material commonly used for …
Marine anoxia and delayed Earth system recovery after the end-Permian extinction
Delayed Earth system recovery following the end-Permian mass extinction is often attributed
to severe ocean anoxia. However, the extent and duration of Early Triassic anoxia remains …
to severe ocean anoxia. However, the extent and duration of Early Triassic anoxia remains …
Co-evolution of oceans, climate, and the biosphere during the 'Ordovician Revolution': a review
The Ordovician Period (~ 485-444 Ma) was an interval of major, causally interconnected 15
changes in the Earth's biotic, climatic, and environmental systems. The diversity of marine …
changes in the Earth's biotic, climatic, and environmental systems. The diversity of marine …
Oxygenation as a driver of the Great Ordovician Biodiversification Event
The largest radiation of Phanerozoic marine animal life quadrupled genus-level diversity
towards the end of the Ordovician Period about 450 million years ago. A leading hypothesis …
towards the end of the Ordovician Period about 450 million years ago. A leading hypothesis …
Global marine redox evolution from the late Neoproterozoic to the early Paleozoic constrained by the integration of Mo and U isotope records
The emergence and diversification of early animals is commonly thought to have coincided
with atmosphere and ocean oxygenation across the terminal Neoproterozoic and early …
with atmosphere and ocean oxygenation across the terminal Neoproterozoic and early …
The rise of animals in a changing environment: global ecological innovation in the late Ediacaran
The evolutionary trajectory of early complex life on Earth is interpreted largely from the
fossils of the Precambrian soft-bodied Ediacara Biota, which appeared and evolved during a …
fossils of the Precambrian soft-bodied Ediacara Biota, which appeared and evolved during a …
Quantifying ecospace utilization and ecosystem engineering during the early Phanerozoic—The role of bioturbation and bioerosion
The Cambrian explosion (CE) and the great Ordovician biodiversification event (GOBE) are
the two most important radiations in Paleozoic oceans. We quantify the role of bioturbation …
the two most important radiations in Paleozoic oceans. We quantify the role of bioturbation …
Synchronizing rock clocks in the late Cambrian
The Cambrian is the most poorly dated period of the past 541 million years. This hampers
analysis of profound environmental and biological changes that took place during this …
analysis of profound environmental and biological changes that took place during this …