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Professor Jonathan Aitchison
Professor

Jonathan Aitchison

Email: 
Phone: 
+61 7 336 56527

Overview

Background

Professor Jonathan C. Aitchison School of the Environment, University of Queensland

Jonathan Aitchison is a Professor in the School of the Environment (SENV) at the University of Queensland (UQ), where he leads research at the intersection of plate tectonics, paleontology, and sedimentary geology. Originally from New Zealand, he grew up on an active plate boundary, an environment that inspired his lifelong fascination with the processes that shape Earth’s dynamic crust.

Professor Aitchison earned his BSc (Hons) and MSc in geology from the University of Otago, including early fieldwork in Antarctica, before moving to Japan as a Monbusho Scholar at Niigata University. He later completed his PhD at the University of New England (Australia), where he reconstructed the tectonic evolution of the New England Orogen using radiolarian microfossils to date marine successions and constrain major tectonic events. This expertise led to his role as a micropaleontologist on Ocean Drilling Program Expedition 126, investigating intra-oceanic island arc development in the Izu–Bonin–Mariana system.

After completing a Japan Society for the Promotion of Science (JSPS) postdoctoral fellowship at Kochi University, Aitchison joined the University of Sydney in the early 1990s, before moving to the University of Hong Kong (HKU) in 1995. At HKU, he established and led the Tibet Research Group, pioneering studies of the India–Asia collision system—research he has pursued for more than three decades. He served as Head of the Department of Earth Sciences at HKU from 2003 to 2009.

In 2011, Aitchison returned to Australia as the Edgeworth David Chair of Geology and Head of the School of Geosciences at the University of Sydney. In 2015 he shifted to Brisbane to take up Headship of the School of Geography, Planning and Environmental Management at UQ. He oversaw the merger that created the School of Earth and Environmental Sciences, leading this school from 2017 to 2021.

His research continues to span multiple frontiers in Earth Science. He maintains active programs in micropaleontology and tectonics, including the evolution of Early Paleozoic radiolarians and the application of synchrotron microCT imaging to microfossils. His long-standing work on the India–Asia collision integrates field studies in northwestern and northeastern India with broader models of Himalayan–Tibetan orogenesis. He also investigates the Paleozoic tectonics of eastern Gondwana.

Recent projects highlight the breadth of his interests: a groundbreaking study of organic carbon recycling that uncovered “bio-diamonds” in ophiolites of the southwest Pacific, and a collaboration with colleagues at the University of Tokyo examining accreted cherts as potential reservoirs of rare earth elements.

Professor Aitchison’s career reflects a commitment to integrating paleontological detail with large-scale tectonic processes, offering new insights into both Earth’s past and its critical resources for the future.

Availability

Professor Jonathan Aitchison is:
Not available for supervision

Qualifications

  • Doctor of Philosophy, University of New England Australia

Research interests

  • Patkai-Bum TTF triple junction - India/Myanmar/China border region

    The deep jungles of Namdapha in far NE India conceal a geological treasure trove of information about the migratory evolution of a TTF (trench-trench-fault) triple junction where Indian, Myanmar micro- and Eurasian plates meet. The geology of this are is little studied but its understanding is fundamental to deciphering evolution of the India-Asia collision system. The project involves collaboration between colleagues from Australia, India and Myanmar.

  • India-Asia collision

    This project began in 1997 and is on-going. It involves study of the greatest tectonic collision on Earth - that between India and Asia, which is responsible for uplift of the Himalaya and Tibetan Plateau. Prior to this collision other tectonic elements within the Tethyan Ocean also collided with either India or Asia and these enigmatic events are of particular interest.

  • Arc-continent collisions

    The development of collisional systems is an integral part of plate tectonics. many collisional systems are much more complex that initially envisaged. For example the India-Asia collision was preceded one or more arc-continent collisions. Understanding these systems requires detailed and often painstaking field research using basic geological skills such as field mapping that provide the spatial basis for later laboratory based analytical work. Our group is working on tectonic reconstruction of the evolutionary history of collages such as the Tibet-Himalayan system; western and southwestern China, SE Asia, the New England and Lachlan fold belts of eastern Australia and the arc-contient collision system in New Caledonia

  • Early Paleozoic radiolarian evolution

    The origins and evolution of radiolarians from the Cambrian through to the Permian; using microCT as a tool for 3D imaging of radiolarian fossils

  • Radiolarian-bearing shales and unconventional hydrocarbon resources

    It appears that many of the exciting new unconventional hydrocarbon plays involve sedimentary facies that include radiolarian-bearing shales (e.g. Longmaxi Formation in the Silurian of the Sichuan Basin and many of the Upper Devonian to Lower Carboniferous rocks of the US mid west). I am interested in interpretation of the development of this facies as well as the influence that siliceous radiolarian skeletons have on facilitating 'frackability' of these rocks.

  • REE in ancient deep-sea muds

    Anomalous abundances of REE and Yttrium are know from deep-sea muds of the Pacific Ocean. This project seeks to examine inland ancient examples of similar sediments in accretionary complexes as potential REY resources.

  • Diamonds and recycled mantle

    This exciting project related to IGCP project 649 [http://www.igcp649.com] Several ophiolites within the Tibet-Himalayan-Alpine orogenic system that were once part of the extensive Tethyan ocean contain microscopic diamonds. I am interested to investigate whether this is unique to the Tethyan system or common amongst other ophiolites such as those which have collided with, and been emplaced onto, elements of the eastern margin of Gondwana. In particular ophiolitic rocks in New Caledonia, New Zealand and eastern Australia are being targeted.

  • Sedimentary response to intra-oceanic subduction within orogens: A case study of the North Qilian belt

    In collaboration with colleagues at the Institute of Geology of the Chinese Academy of Geological Sciences, Beijing I am working on an NSFC-funded project to investigate intra-oceanic subduction is ubiquitous and ongoing in modern oceanic basins, but it is rarely reported in ancient orogenic belts. At present, the identification of ancient intra-oceanic subduction processes is mostly based on the study of igneous rocks, and there has been a lack of sedimentological constraints. As a product of plate convergence, orogenic belts have recorded intra-ocean, ocean-continent subduction and continent-continent collision processes, and are natural laboratories for reshaping ancient subduction processes. The relatively complete Early Paleozoic trench-arc (basin) system outcropped in the North Qilian structural belt was formed in intra-oceanic and ocean-continental subduction, which provides an opportunity for classical research on the sedimentary response to intra-oceanic subduction. This project takes the Cambrian-Ordovician sedimentary basin in North Qilian as the research object, systematically studies the basin filling sequence, sedimentary facies and depositional environment, composition and source area of the filling, and focuses on petrology, clastic mineral structure and age "fingerprint" Combined with regional magmatic, metamorphic, and paleontological data, comprehensively analyze basin types and the evolution of the original Tethys Ocean, reconstruct the history of intraoceanic subduction and sedimentary responses, eliminate the blind spots in the study of intraoceanic subduction sedimentary records in orogenic belts, and try to establish a general The adaptive identification system of paleo-oceanic subduction geological records can make up for the defect that modern oceanic subduction zone studies cannot reveal the complete depositional process of basins, and provide new ideas and methods for the identification of intra-oceanic subduction of orogenic paleo-oceanic basins.

Research impacts

Professor Aitchison's research interests include the evolution of the the India-Asia collision system. This involves the Himalaya and Tibet-Qinghai Plateau and surrounding regions over a variety of time scales. He has a strong interest in tectonics and collision zones especially those involving intra-oceanic island arcs and ophiolites, subduction initiation, continental collision; the Yarlung Tsangpo, Indus, Bangong-Nujiang and Shyok suture zones, as well as the the role of tecotnics in the climatic evolution of Tibet. Recent fieldwork has concentrated in NW India in Ladakh as well as NE India in Arunachal Pradesh and Nagaland and Manipur. He has also been working on the northern margin of the Tibetan Plateau in the Qinling and Qilian regions. He also investigates the evolution of life on Earth, biogeography and extremophile organisms, radiolarian paleoecology and biostratigraphy, the tectonic evolution of East Asia and the tectonic evolution of eastern Australia through the Phanerozoic and island biogeography and the complex interplay between Darwinian biological evolution, and eustatic and subsidence driven sea-level change especially in the Galapagos. Recent paleobiogeographic work has involved Christmas Island and the Wallace Line.

The main projects he has been working on are as lead CI on an ARC DP funded investigation of "Early Paleozoic radiolarian evolution". This DP is now completed by the research continues and involves examination of incredibly well preserved radiolarian faunas using microCT (and from November 2022) synchrotron technology.

Jonathan is also working on another ARC DP funded project entitled "Diamonds in ophiolite: Recycling deep mantle into supra-subduction zones" examining ophiolitic rocks in New Caledonia, New Zealand and New England. These rocks include diamonds that carry and organic isotopic signature and are unique to supra-subduction zone ophiolites.

Works

Search Professor Jonathan Aitchison’s works on UQ eSpace

286 works between 1983 and 2025

281 - 286 of 286 works

1988

Journal Article

Lithofacies and origin of the buckeye formation: Late paleozoic glacial and glaciomarine sediments, Ohio range, transantarctic mountains, Antarctica

Aitchison, J. C., Bradshaw, M. A. and Newman, J. (1988). Lithofacies and origin of the buckeye formation: Late paleozoic glacial and glaciomarine sediments, Ohio range, transantarctic mountains, Antarctica. Palaeogeography, Palaeoclimatology, Palaeoecology, 64 (1-2), 93-104. doi: 10.1016/0031-0182(88)90145-9

Lithofacies and origin of the buckeye formation: Late paleozoic glacial and glaciomarine sediments, Ohio range, transantarctic mountains, Antarctica

1988

Journal Article

Late Paleozoic radiolarian ages from the Gywdir terrane, New England orogen, eastern Australia

Aitchison, J. C. (1988). Late Paleozoic radiolarian ages from the Gywdir terrane, New England orogen, eastern Australia. Geology, 16 (9), 793-795. doi: 10.1130/0091-7613(1988)0162.3.CO;2

Late Paleozoic radiolarian ages from the Gywdir terrane, New England orogen, eastern Australia

1985

Journal Article

New zealand journal of geology and geophysics

Aitchison, J. C. (1985). New zealand journal of geology and geophysics. New Zealand Journal of Geology and Geophysics, 28 (4). doi: 10.1080/00288306.1985.10428488

New zealand journal of geology and geophysics

1985

Journal Article

Pillow lava and conglomerate in metamorphosed torlesse terrane rocks of haast schist group, landsborough valley, southern alps, new zealand

Aitchison, J. C. (1985). Pillow lava and conglomerate in metamorphosed torlesse terrane rocks of haast schist group, landsborough valley, southern alps, new zealand. New Zealand Journal of Geology and Geophysics, 28 (4), 751-754. doi: 10.1080/00288306.1985.10422545

Pillow lava and conglomerate in metamorphosed torlesse terrane rocks of haast schist group, landsborough valley, southern alps, new zealand

1985

Journal Article

Hot springs along the alpine fault, cascade river valley, south westland, new zealand

Aitchison, J. C. (1985). Hot springs along the alpine fault, cascade river valley, south westland, new zealand. New Zealand Journal of Geology and Geophysics, 28 (4), 755-756. doi: 10.1080/00288306.1985.10422546

Hot springs along the alpine fault, cascade river valley, south westland, new zealand

1983

Journal Article

Appendix: Geological setting of the Livingstone fossil insect

Aitchison, Jonathan C, Campbell, Hamish J, Campbell, J.D. and Raine, J. I (1983). Appendix: Geological setting of the Livingstone fossil insect. Journal of the Royal Society of New Zealand, 13 (3), 103-105. doi: 10.1080/03036758.1983.10415323

Appendix: Geological setting of the Livingstone fossil insect

Funding

Current funding

  • 2019 - 2025
    Diamonds in ophiolite: Recycling deep mantle into supra-subduction zones
    ARC Discovery Projects
    Open grant
  • 2017 - 2026
    Collaborative Research in Aquatic Toxicology
    Queensland Government Department of Science, Information Technology and Innovation
    Open grant
  • 2011 - 2025
    The Robert Day Postdoctoral Fellowship in Palaeontology and Stratigraphy
    Research Donation Generic
    Open grant

Past funding

  • 2021 - 2022
    Analysis of rare diamonds from ancient oceanic lithosphere using synchrotron-FTIR microspectroscopy
    Australian Nuclear Science and Technology Organisation
    Open grant
  • 2018 - 2019
    Continuous flow isotope ratio mass spectrometer (CF-IRMS) and ancillary preparation systems for carbon, nitrogen and sulfur isotope microanalysis for archaeology, biology, earth and environmental scie
    UQ Major Equipment and Infrastructure
    Open grant
  • 2017 - 2018
    Centre for Geoanalytical Mass Spectrometry (CGMS) - Achieving excellence in isotope geochemistry and geochronology
    UQ Research Facilities Infrastructure Grants
    Open grant
  • 2017 - 2019
    Resolving questions about continental convergence using the double and triple dating method
    Universities Australia - Germany Joint Research Co-operation Scheme
    Open grant
  • 2016
    Next-generation multi-collector inductively-coupled plasma mass spectrometer (MC-ICP-MS) with laser-ablation capability for in situ high-throughput and high resolution isotope dating and characterizat
    UQ Major Research Facility Fund
    Open grant
  • 2015 - 2020
    Early Palaeozoic radiolarian evolution
    ARC Discovery Projects
    Open grant

Supervision

Availability

Professor Jonathan Aitchison is:
Not available for supervision

Supervision history

Current supervision

  • Doctor Philosophy

    Diamonds in Ophiolites: recycling deep mantle into supra-subduction zones

    Principal Advisor

    Other advisors: Dr Renjie Zhou

Completed supervision

Media

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