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Showing 1–11 of 11 results
Advanced filters: Author: Pincelli M. Hull Clear advanced filters
  • The fossil record provides a nuanced view of ecosystem collapse over intervals of mass extinction, with abundant, biomineralizing and widespread species preferentially preserved; here the authors collate evidence for ‘mass rarity’ during these intervals, and suggest that the increasing rarity of modern species, rather than their outright extinction, may be a better metric for comparing the current biodiversity crisis to the ‘Big Five’ mass extinctions in the Earth’s history.

    • Pincelli M. Hull
    • Simon A. F. Darroch
    • Douglas H. Erwin
    Reviews
    Nature
    Volume: 528, P: 345-351
  • Two competing models have been suggested to explain the recovery of ecosystems from mass extinctions. An analysis of the recovery of marine pelagic communities from the Cretaceous–Palaeogene mass extinction supports a model of contingent recovery, rather than one based on trophic structure.

    • Pincelli M. Hull
    • Richard D. Norris
    • Jonathan D. Schueth
    Research
    Nature Geoscience
    Volume: 4, P: 856-860
  • New proxy data for ocean pH and an ocean–atmosphere model show that a radically different ocean circulation led to decoupling of ocean productivity and upwelling in the equatorial Pacific Ocean 3–6 million years ago.

    • Madison G. Shankle
    • Natalie J. Burls
    • Pincelli M. Hull
    Research
    Nature
    Volume: 598, P: 457-461
  • Molecular analyses of modern and fossil skeletal samples reveal that elevated metabolic rates consistent with endothermy evolved independently in mammals and plesiosaurs, and ornithodirans: Exceptional metabolic rates are ancestral to dinosaurs and pterosaurs and were acquired before energetically costly adaptations, such as flight.

    • Jasmina Wiemann
    • Iris Menéndez
    • Derek E. G. Briggs
    Research
    Nature
    Volume: 606, P: 522-526
  • The Cretaceous/Palaeogene mass extinction caused ecosystem upheaval. Fish abundance data from the Tethys Sea and the Pacific Ocean indicate heterogeneity in the extinction and recovery, with greater resilience in the Pacific.

    • Elizabeth C. Sibert
    • Pincelli M. Hull
    • Richard D. Norris
    Research
    Nature Geoscience
    Volume: 7, P: 667-670
  • The Pliocene shows that a warmer world can support both expanded and contracted marine Oxygen Minimum Zones. While oxygen distributions were overall like today, there was less low-oxygen water in the North Pacific and more in the North Atlantic

    • Catherine V. Davis
    • Elizabeth C. Sibert
    • Pincelli M. Hull
    ResearchOpen Access
    Nature Communications
    Volume: 14, P: 1-11
  • Single-foraminifera measurements of the PETM carbon isotope excursion from Maud Rise have been interpreted as indicating geologically instantaneous carbon release. Here, the authors explain these records using an Earth system model and a sediment-mixing model and extract the likely PETM onset duration.

    • Sandra Kirtland Turner
    • Pincelli M. Hull
    • Andy Ridgwell
    ResearchOpen Access
    Nature Communications
    Volume: 8, P: 1-10
  • The effects of biological similarity on geochemical signals recorded in planktonic foraminiferal tests used in paleo-reconstructions remains unclear. Here, the authors embed species-specific vital effect offsets in evolutionary models and show how shared evolutionary history shapes δ13C, but not δ18O values.

    • Kirsty M. Edgar
    • Pincelli M. Hull
    • Thomas H. G. Ezard
    ResearchOpen Access
    Nature Communications
    Volume: 8, P: 1-9