ORCID Profile
0000-0003-3410-1670
Current Organisation
University of Melbourne
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In Research Link Australia (RLA), "Research Topics" refer to ANZSRC FOR and SEO codes. These topics are either sourced from ANZSRC FOR and SEO codes listed in researchers' related grants or generated by a large language model (LLM) based on their publications.
Geology | Geochronology | Surface Processes | Palaeoclimatology | Geochemistry | Archaeological Science | Igneous And Metamorphic Petrology | Archaeology | Earth Sciences Not Elsewhere Classified | Aboriginal and Torres Strait Islander Archaeology | Geochronology And Isotope Geochemistry | Sedimentology | Electromagnetism | Archaeological Science | Climatology (Incl. Palaeoclimatology) | Marine Geoscience | Ore Deposit Petrology | Isotope Geochemistry | Other Stratigraphy (Incl. Sequence Stratigraphy) | Geology Not Elsewhere Classified | Geochemistry Not Elsewhere Classified | Volcanology
Expanding Knowledge in the Earth Sciences | Earth sciences | Expanding Knowledge in History and Archaeology | Effects of Climate Change and Variability on Australia (excl. Social Impacts) | Climate Change Models | Conserving Aboriginal and Torres Strait Islander Heritage | Biological sciences | Environmental and resource evaluation not elsewhere classified | Scientific instrumentation | Climate variability | Concentrating processes of other base metal ores | Mineral Resources (excl. Energy Resources) not elsewhere classified | Expanding Knowledge in the Environmental Sciences |
Publisher: Springer Science and Business Media LLC
Date: 12-2000
Publisher: Wiley
Date: 12-2008
Publisher: Elsevier BV
Date: 2008
Publisher: Elsevier BV
Date: 09-2004
Publisher: Elsevier BV
Date: 20-05-2008
Publisher: Royal Society of Chemistry (RSC)
Date: 2012
DOI: 10.1039/C2JA10383D
Publisher: Elsevier BV
Date: 12-2020
Publisher: Royal Society of Chemistry (RSC)
Date: 2015
DOI: 10.1039/C5SC02231B
Abstract: Studying the neuroanatomy of the mouse brain using imaging mass spectrometry and chemometric analysis.
Publisher: Springer Science and Business Media LLC
Date: 06-1993
DOI: 10.1007/BF00307754
Publisher: Oxford University Press (OUP)
Date: 08-1989
Publisher: Elsevier BV
Date: 11-2016
Publisher: Elsevier BV
Date: 05-2015
Publisher: Springer Science and Business Media LLC
Date: 22-02-2021
Publisher: Elsevier BV
Date: 03-1999
Publisher: Geological Society of London
Date: 1994
Publisher: Royal Society of Chemistry (RSC)
Date: 2014
DOI: 10.1039/C4JA00008K
Abstract: This papers describes the source of systematic bias in U–Pb zircon dating by LA-ICP-MS.
Publisher: Elsevier BV
Date: 11-2009
Publisher: Geological Society of London
Date: 15-06-2023
DOI: 10.1144/JGS2022-171
Abstract: The Turkana Basin in NW Kenya and SW Ethiopia hosts remarkable fossil-rich sediments that are central to our understanding of early hominin evolution, with interbedded volcanic tuffs providing critical time markers. However, the resolution of existing Early Pleistocene–Pliocene ages is limited to c. 20–60 kyr, inhibiting the evaluation of climatic and environmental drivers of evolution. We present high-precision, single-feldspar 40 Ar/ 39 Ar age and elemental data for four stratigraphically significant tuffs. These s les exhibit variably dispersed age distributions correlated with feldspar compositional trends, interpreted to indicate the partial retention of inherited 40 Ar related to crustal ‘cold storage’ and rapid melt infiltration preceding eruption. We evaluated various statistical methods and calculated astronomically calibrated Bayesian age estimates of 1879.1 ± 0.6 ka (±2.4 ka including external errors) for the Kay Behrensmeyer Site (KBS)/H2 Tuff, 1837.4 ± 0.9 ka (±2.4 ka) for the Malbe/H4 Tuff, 1357.5 ± 1.8 ka (±2.5 ka) for the Chari/L Tuff and 1315.4 ± 1.9 ka (±2.5 ka) for the Gele Tuff. Our results permit refined age constraints for important early Homo fossils, including the cranium KNM-ER1813 ( Homo habilis ) and various Homo erectus fossils. The KBS Tuff age also provides an important calibration locus for orbital tuning of palaeoclimate proxy records, revealing the complex interplays between palaeoclimate and geological drivers of sedimentation. Supplementary material : The supplementary tables and figures include previously published ages (Table S1), s le and irradiation information (Table S2), electron probe microanalytical results for tuff glasses (Table S3, Figs S2 and S3) and feldspars (Table S4), 40 Ar/ 39 Ar analytical data (Tables S5 and S6, Fig. S4), orbital tuning model parameters (Table S7), a summary of previous and revised hominin ages (Table S8) and a worked Bayesian estimation ex le (Fig. S1) and are available at 0.6084/m9.figshare.c.6602994
Publisher: American Geophysical Union
Date: 1995
DOI: 10.1029/GM088P0175
Publisher: Geological Society of America
Date: 2007
DOI: 10.1130/G24040A.1
Publisher: Royal Society of Chemistry (RSC)
Date: 2005
DOI: 10.1039/B507647A
Publisher: Informa UK Limited
Date: 10-2007
Publisher: Oxford University Press (OUP)
Date: 2016
Publisher: Elsevier BV
Date: 10-2018
Publisher: Elsevier BV
Date: 10-2020
Publisher: Geological Society of America
Date: 2003
Publisher: Elsevier BV
Date: 07-1991
Publisher: Geological Society of America
Date: 2003
Publisher: Elsevier BV
Date: 04-1992
Publisher: Informa UK Limited
Date: 12-1991
Publisher: Informa UK Limited
Date: 04-2008
Publisher: Royal Society of Chemistry (RSC)
Date: 2020
DOI: 10.1039/C9JA00423H
Abstract: Integration of quantitative elemental distributions with structural information, allowing novel insights into how tissue development is associated with a dynamic chemical environment.
Publisher: Elsevier BV
Date: 11-2009
Publisher: Elsevier BV
Date: 05-2008
Publisher: American Geophysical Union (AGU)
Date: 08-2022
DOI: 10.1029/2021GC010324
Abstract: Despite the scientific and economic significance of kimberlites and related magmas, their origin is unclear. Here, we address this issue using whole‐rock and perovskite‐derived Sr‐Nd‐Hf isotopes for the three occurrences of kimberlite, l roites and ultramafic l rophyres (UMLs) in Finland. Mesoproterozoic olivine l roites at Lentiira‐Kuhmo and UMLs at Kuusamo have different isotopic signatures yet were emplaced contemporaneously at 1,200 Ma in response to an extensional regime linked to the Baltica‐Laurentia breakup. The low εNd (i) and εHf (i) values of the olivine l roites are consistent with an enriched subcontinental lithospheric mantle (SCLM) source while UML compositions are intermediate between those of typical kimberlites and l roites and are interpreted to reflect mixing of asthenospheric melts and ∼10%–15% of melts sourced from metasomatized SCLM. The ∼750 Ma Kuusamo kimberlites, are probably linked to the mantle plume activity that initiated Rodinia's break‐up, exhibiting homogenous isotopic compositions which mirror the prominent Geodynamic and Source Constraints for ∼1,200 Ma Olivine L roite and Ultramafic L rophyre Magmatism in Eastern Finland (PREMA)‐like signature of kimberlites globally. By contrast, ∼620–585 Ma Kaavi‐Kuopio kimberlites show limited range in εNd (i) and 87 Sr/ 86 Sr (i) but have remarkably heterogeneous εHf (i) (+6.5 to −6.3) with a temporal trend toward lower εHf (i) values. While the Kuusamo kimberlites erupted during the early stage of continental break‐up, the Kaavi‐Kuopio kimberlites were emplaced when Rodinia break‐up was completed, coeval with formation of the Central Iapetus large igneous province. Magmas forming the Kaavi‐Kupio kimberlites may have formed from an upwelling mantle source similar to PREMA modified by increasing incorporation (up to 10%) of recycled crustal material through time accounting for the trend toward lower εHf (i) in these kimberlites.
Publisher: Wiley
Date: 06-2000
Publisher: Elsevier BV
Date: 10-1994
Publisher: Royal Society of Chemistry (RSC)
Date: 2016
DOI: 10.1039/C6SC90060G
Abstract: Correction for ‘Visualising mouse neuroanatomy and function by metal distribution using laser ablation-inductively coupled plasma-mass spectrometry imaging’ by Bence Paul et al. , Chem. Sci. , 2015, 6 , 5383–5393.
Publisher: Informa UK Limited
Date: 08-2001
Publisher: Royal Society of Chemistry (RSC)
Date: 2015
DOI: 10.1039/C5SC90051D
Abstract: Correction for 'Visualising mouse neuroanatomy and function by metal distribution using laser ablation-inductively coupled plasma-mass spectrometry imaging' by Bence Paul et al. , Chem. Sci. , 2015, DOI: 10.1039/c5sc02231b.
Publisher: Wiley
Date: 16-11-2007
Publisher: Society of Economic Geologists
Date: 02-05-2013
Publisher: Springer Science and Business Media LLC
Date: 07-1989
DOI: 10.1007/BF00373722
Publisher: Elsevier BV
Date: 04-2019
Publisher: Elsevier BV
Date: 03-2020
Publisher: Elsevier BV
Date: 02-2020
Publisher: Elsevier BV
Date: 08-2007
Publisher: American Association for the Advancement of Science (AAAS)
Date: 04-03-2022
Abstract: Earth's carbon cycle is strongly influenced by subduction of sedimentary material into the mantle. The composition of the sedimentary subduction flux has changed considerably over Earth's history, but the impact of these changes on the mantle carbon cycle is unclear. Here, we show that the carbon isotopes of kimberlite magmas record a fundamental change in their deep-mantle source compositions during the Phanerozoic Eon. The
Publisher: Elsevier BV
Date: 10-2001
Publisher: Informa UK Limited
Date: 10-1999
Publisher: Elsevier BV
Date: 06-1998
Publisher: Elsevier BV
Date: 10-2020
Publisher: Elsevier BV
Date: 08-2017
Publisher: Royal Society of Chemistry (RSC)
Date: 2005
DOI: 10.1039/B412730G
Publisher: Elsevier BV
Date: 2020
Publisher: Geological Society of America
Date: 06-2012
DOI: 10.1130/G32963.1
Publisher: American Association for the Advancement of Science (AAAS)
Date: 16-02-2007
Abstract: Granitic plutonism is the principal agent of crustal differentiation, but linking granite emplacement to crust formation requires knowledge of the magmatic evolution, which is notoriously difficult to reconstruct from bulk rock compositions. We unlocked the plutonic archive through hafnium (Hf) and oxygen (O) isotope analysis of zoned zircon crystals from the classic hornblende-bearing (I-type) granites of eastern Australia. This granite type forms by the reworking of sedimentary materials by mantle-like magmas instead of by remelting ancient metamorphosed igneous rocks as widely believed. I-type magmatism thus drives the coupled growth and differentiation of continental crust.
Publisher: European Association of Geochemistry
Date: 07-2017
Publisher: Elsevier BV
Date: 05-2002
Publisher: Elsevier BV
Date: 03-2019
Publisher: Elsevier BV
Date: 03-2019
Publisher: Springer Science and Business Media LLC
Date: 25-09-2019
DOI: 10.1038/S41586-019-1574-8
Abstract: The widely accepted paradigm of Earth's geochemical evolution states that the successive extraction of melts from the mantle over the past 4.5 billion years formed the continental crust, and produced at least one complementary melt-depleted reservoir that is now recognized as the upper-mantle source of mid-ocean-ridge basalts
Publisher: Proceedings of the National Academy of Sciences
Date: 11-01-2016
Abstract: We show for the first time, to our knowledge, that pedogenic (soil) carbonate mineral accumulations can preserve continuous paleoclimate records that rival the temporal resolution of widely used archives, such as speleothems or lake sediments. Using microanalysis of oxygen, carbon, and uranium isotopes coupled with uranium series dating, we find evidence for a distinct shift in atmospheric circulation in North America’s interior from 70,000 to 55,000 years ago, a finding that highlights the influence of large continental ice sheets on atmospheric circulation. Perhaps most significantly, this work shows that pedothems, which are common in arid and semiarid regions around the world, are a rich archive of paleoclimate information for continental landscapes.
Publisher: Springer Science and Business Media LLC
Date: 06-06-2000
Publisher: Elsevier BV
Date: 12-1989
Publisher: Elsevier BV
Date: 10-2011
Publisher: Springer Science and Business Media LLC
Date: 04-05-2018
Publisher: Elsevier BV
Date: 02-2010
Publisher: Elsevier BV
Date: 03-2002
Publisher: Wiley
Date: 23-05-2014
Publisher: Wiley
Date: 16-11-2007
Publisher: Mineralogical Association of Canada
Date: 12-2007
Publisher: Elsevier BV
Date: 11-2009
Publisher: Elsevier BV
Date: 02-2010
Publisher: Elsevier BV
Date: 11-1997
Publisher: Geological Society of America
Date: 1998
Publisher: American Geophysical Union (AGU)
Date: 09-2011
DOI: 10.1029/2011GC003683
Publisher: American Geophysical Union (AGU)
Date: 03-2010
DOI: 10.1029/2009GC002618
Publisher: Wiley
Date: 12-2010
Publisher: Elsevier BV
Date: 02-2002
Publisher: Elsevier BV
Date: 10-2007
Publisher: Elsevier BV
Date: 10-1997
Publisher: Informa UK Limited
Date: 04-2005
Publisher: American Association for the Advancement of Science (AAAS)
Date: 07-02-2020
Abstract: Radiocarbon-dated mud wasp nests provide a terminal Pleistocene age estimate for an Australian Aboriginal rock art style.
Publisher: Royal Society of Chemistry (RSC)
Date: 2011
DOI: 10.1039/C1JA10172B
Publisher: Oxford University Press (OUP)
Date: 2018
Publisher: Geological Society of London
Date: 1992
Publisher: Elsevier BV
Date: 12-2019
Publisher: Elsevier BV
Date: 05-2009
Publisher: Elsevier BV
Date: 04-2011
Location: United Kingdom of Great Britain and Northern Ireland
Start Date: 2014
End Date: 2015
Funder: Australian Research Council
View Funded ActivityStart Date: 2013
End Date: 2016
Funder: Australian Research Council
View Funded ActivityStart Date: 2008
End Date: 2012
Funder: Australian Research Council
View Funded ActivityStart Date: 2005
End Date: 2013
Funder: Australian Research Council
View Funded ActivityStart Date: 2018
End Date: 2020
Funder: Australian Research Council
View Funded ActivityStart Date: 2006
End Date: 2006
Funder: Australian Research Council
View Funded ActivityStart Date: 2018
End Date: 2021
Funder: Australian Research Council
View Funded ActivityStart Date: 2009
End Date: 2009
Funder: Australian Research Council
View Funded ActivityStart Date: 2006
End Date: 2008
Funder: Hermon Slade Foundation
View Funded ActivityStart Date: 03-2008
End Date: 09-2013
Amount: $6,000,000.00
Funder: Australian Research Council
View Funded ActivityStart Date: 07-2005
End Date: 06-2014
Amount: $24,450,000.00
Funder: Australian Research Council
View Funded ActivityStart Date: 07-2018
End Date: 06-2023
Amount: $414,204.00
Funder: Australian Research Council
View Funded ActivityStart Date: 03-2021
End Date: 02-2026
Amount: $1,337,900.00
Funder: Australian Research Council
View Funded ActivityStart Date: 06-2014
End Date: 09-2017
Amount: $480,000.00
Funder: Australian Research Council
View Funded ActivityStart Date: 2006
End Date: 12-2007
Amount: $186,000.00
Funder: Australian Research Council
View Funded ActivityStart Date: 2009
End Date: 06-2010
Amount: $950,000.00
Funder: Australian Research Council
View Funded ActivityStart Date: 04-2018
End Date: 04-2024
Amount: $880,000.00
Funder: Australian Research Council
View Funded ActivityStart Date: 2014
End Date: 12-2016
Amount: $3,600,000.00
Funder: Australian Research Council
View Funded Activity