Publications in collaboration with researchers from Australian National University (15)

2020

  1. Author Correction: Extraordinary human energy consumption and resultant geological impacts beginning around 1950 CE initiated the proposed Anthropocene Epoch (Communications Earth & Environment, (2020), 1, 1, (32), 10.1038/s43247-020-00029-y)

    Communications Earth and Environment

  2. Extraordinary human energy consumption and resultant geological impacts beginning around 1950 CE initiated the proposed Anthropocene Epoch

    Communications Earth and Environment, Vol. 1, Núm. 1

  3. UNDERGROUND METRO SYSTEMS A durable geological proxy of rapid urban population growth and energy consumption during the Anthropocene

    ROUTLEDGE COMPANION TO BIG HISTORY (ROUTLEDGE), pp. 434-455

2019

  1. A formal Anthropocene is compatible with but distinct from its diachronous anthropogenic counterparts: a response to W.F. Ruddiman’s ‘three flaws in defining a formal Anthropocene’

    Progress in Physical Geography, Vol. 43, Núm. 3, pp. 319-333

2018

  1. Global Boundary Stratotype Section and Point (GSSP) for the Anthropocene Series: Where and how to look for potential candidates

    Earth-Science Reviews, Vol. 178, pp. 379-429

2017

  1. Making the case for a formal Anthropocene Epoch: An analysis of ongoing critiques

    Newsletters on Stratigraphy, Vol. 50, Núm. 2, pp. 205-226

  2. Scale and diversity of the physical technosphere: A geological perspective

    Anthropocene Review, Vol. 4, Núm. 1, pp. 9-22

  3. The Working Group on the Anthropocene: Summary of evidence and interim recommendations

    Anthropocene, Vol. 19, pp. 55-60

2016

  1. The Anthropocene is functionally and stratigraphically distinct from the Holocene

    Science, Vol. 351, Núm. 6269

  2. The Anthropocene: A conspicuous stratigraphical signal of anthropogenic changes in production and consumption across the biosphere

    Earth's Future, Vol. 4, Núm. 3, pp. 34-53

  3. The geological cycle of plastics and their use as a stratigraphic indicator of the Anthropocene

    Anthropocene, Vol. 13, pp. 4-17

2015

  1. Colonization of the Americas, ‘little ice age’ climate, and bombproduced carbon: Their role in defining the anthropocene

    Anthropocene Review, Vol. 2, Núm. 2, pp. 117-127

  2. When did the Anthropocene begin? A mid-twentieth century boundary level is stratigraphically optimal

    Quaternary International, Vol. 383, pp. 196-203

2010

  1. Exhumation of high-pressure rocks in northern Gondwana during the Early Carboniferours (Coimbra-Cordoba shear zone, SW Iberian Massif): Tectonothermal analysis and U-Th-Pb SHRIMP in-situ zircon geochronology

    Gondwana Research, Vol. 17, Núm. 2-3, pp. 440-460

2009

  1. Variscan intra-orogenic extensional tectonics in the Ossa-Morena Zone (Évora-Aracena-Lora del Río metamorphic belt, SW Iberian Massif): SHRIMP zircon U-Th-Pb geochronology

    Geological Society Special Publication, Vol. 327, pp. 215-237