Associate Professor Mark Kendrick
Associate Professor

Mark Kendrick

Email: 
Phone: 
+61 7 336 53454

Background

I use geochemistry to investigate the roles of fluids and volatiles in geological processes stretching from the Earth's surface to the deep mantle. I am particularly interested in hydrothermal alteration, metasomatism/metamorphism and magmatism. The common link between these areas, and the aim of my recent research, has been to investigate the longterm exchange of volatiles between the Earth's surface and mantle reservoirs, stretching from the seafloor, through subduction zones and into the mantle. I participated in Expedition 360 of the International Ocean Discovery Program in 2016, to the slow-spreading Atlantis Bank core complex on the SW Indian Ridge, where I acted as shipboard geochemist and crossed the equator by boat for the first time. I have long standing interests in fluid inclusions as tiny recorders of past fluid activity and special interests in the halogen and noble gas groups of elements.

I moved to UQ in 2019 from the Australian National University where I was a continuing Fellow and had held an ARC Future Fellowship. Prior to that I had an ARC QEII Fellowship at the University of Melbourne (2008-2013) and postdoctoral appointments at the University of Melbourne (2004-2008) and the Geological Survey of Norway (2001-2003). I did my PhD at the University of Manchester (2001) and undergraduate studies in Geology at the University of Edinburgh (1996).

Availability

Associate Professor Mark Kendrick is:
Available for supervision

Fields of research

Earth Sciences Geochemistry Geochemistry not elsewhere classified Geochronology Geology Igneous and metamorphic petrology Isotope geochemistry Marine geoscience Resource geoscience

Qualifications

  • Bachelor of Science, University of Edinburgh
  • Doctor of Philosophy, The University of Manchester

Research impacts

Fluids enable the exchange of volatiles between the Earth's surface and mantle reservoirs, which has significant implications for the evolution of our planet, it's habitibility and climate. Hydrothermal fluids also form economically important ore deposits.

Investigating the origin of ore forming fluids can impact exploration strategies. For example, fingerprinting if ore forming fluids are related to magmatic activity or the former presence of evaporitic salt, helps delimit which areas are prospective for different metals. I wrote a chapter summarising halogen and noble gas constraints on fluid sources and acquisition of salinity in the Noble Gases as Geochemical Tracers.

My most important (and shortest) contributions to the fundamental process of global volatile (re)cycling are Kendrick et al., 2011 and Kendrick et al., 2017. I wrote a review of the behaviour of halogens in altered oceanic lithosphere in The Role of Halogens in Terrestrial and Extraterrestrial Processes.

Search Professor Mark Kendrick’s works on UQ eSpace

92 works between 1981 and 2024
All (92) Journal Article (82) Book Chapter (9) Conference Publication (1)

61 - 80 of 92 works

2012

Journal Article

Nature of alkali-carbonate fluids in the sub-continental lithospheric mantle

Giuliani, A., Kamenetsky, V. S., Phillips, D., Kendrick, M. A., Wyatt, B. A. and Goemann, K. (2012). Nature of alkali-carbonate fluids in the sub-continental lithospheric mantle. Geology, 40 (11), 967-970. doi: 10.1130/G33221.1

Nature of alkali-carbonate fluids in the sub-continental lithospheric mantle

2012

Journal Article

Halogen systematics (Cl, Br, I) in Mid-Ocean Ridge Basalts: a Macquarie Island case study

Kendrick, Mark A., Kamenetsky, Vadim S., Phillips, David and Honda, Masahiko (2012). Halogen systematics (Cl, Br, I) in Mid-Ocean Ridge Basalts: a Macquarie Island case study. Geochimica et Cosmochimica Acta, 81, 82-93. doi: 10.1016/j.gca.2011.12.004

Halogen systematics (Cl, Br, I) in Mid-Ocean Ridge Basalts: a Macquarie Island case study

2012

Journal Article

New constraints on fluid sources in orogenic gold deposits, Victoria, Australia

Fu, Bin, Kendrick, Mark A., Fairmaid, Alison M., Phillips, David, Wilson, Christopher J.L. and Mernagh, Terrence P. (2012). New constraints on fluid sources in orogenic gold deposits, Victoria, Australia. Contributions to Mineralogy and Petrology, 163 (3), 427-447. doi: 10.1007/s00410-011-0678-4

New constraints on fluid sources in orogenic gold deposits, Victoria, Australia

2012

Journal Article

High precision Cl, Br and I determinations in mineral standards using the noble gas method

Kendrick, Mark A. (2012). High precision Cl, Br and I determinations in mineral standards using the noble gas method. Chemical Geology, 292-293, 116-126. doi: 10.1016/j.chemgeo.2011.11.021

High precision Cl, Br and I determinations in mineral standards using the noble gas method

2011

Journal Article

Mineral system analysis of the Mt Isa-McArthur River region, Northern Australia

Murphy, F. C., Hutton, L. J., Walshe, J. L., Cleverley, J. S., Kendrick, M. A., Mclellan, J., Rubenach, M. J., Oliver, N. H.S., Gessner, K., Bierlein, F. P., Jupp, B., Aillères, L., Laukamp, C., Roy, I. G., Miller, J. McL, Keys, D. and Nortje, G. S. (2011). Mineral system analysis of the Mt Isa-McArthur River region, Northern Australia. Australian Journal of Earth Sciences, 58 (8), 849-873. doi: 10.1080/08120099.2011.606333

Mineral system analysis of the Mt Isa-McArthur River region, Northern Australia

2011

Journal Article

Halogens and noble gases in sedimentary formation waters and Zn-Pb deposits: a case study from the Lennard Shelf, Australia

Kendrick, M. A., Phillips, D., Wallace, M. and Miller, J.McL. (2011). Halogens and noble gases in sedimentary formation waters and Zn-Pb deposits: a case study from the Lennard Shelf, Australia. Applied Geochemistry, 26 (12), 2089-2100. doi: 10.1016/j.apgeochem.2011.07.007

Halogens and noble gases in sedimentary formation waters and Zn-Pb deposits: a case study from the Lennard Shelf, Australia

2011

Journal Article

Fluid sources and the role of abiogenic-CH4 in Archean gold mineralization: constraints from noble gases and halogens

Kendrick, M. A., Honda, M., Walshe, J. and Petersen, K. (2011). Fluid sources and the role of abiogenic-CH4 in Archean gold mineralization: constraints from noble gases and halogens. Precambrian Research, 189 (3-4), 313-327. doi: 10.1016/j.precamres.2011.07.015

Fluid sources and the role of abiogenic-CH4 in Archean gold mineralization: constraints from noble gases and halogens

2011

Journal Article

The origin and evolution of mineralizing fluids in a sediment-hosted orogenic-gold deposit, Ballarat East, Southeastern Australia

Fairmaid, A. M., Kendrick, M. A., Phillips, D. and Fu, B. (2011). The origin and evolution of mineralizing fluids in a sediment-hosted orogenic-gold deposit, Ballarat East, Southeastern Australia. Economic Geology, 106 (4), 653-666. doi: 10.2113/econgeo.106.4.653

The origin and evolution of mineralizing fluids in a sediment-hosted orogenic-gold deposit, Ballarat East, Southeastern Australia

2010

Journal Article

Lower succinyl-CoA:3-ketoacid-CoA transferase (SCOT) and ATP citrate lyase in pancreatic islets of a rat model of type 2 diabetes: Knockdown of SCOT inhibits insulin release in rat insulinoma cells

Hasan, Noaman M., Longacre, Melissa J., Ahmed, Mohammed Seed, Kendrick, Mindy A., Gu, Harvest, Ostenson, Claes-Goran, Fukao, Toshiyuki and MacDonald, Michael J. (2010). Lower succinyl-CoA:3-ketoacid-CoA transferase (SCOT) and ATP citrate lyase in pancreatic islets of a rat model of type 2 diabetes: Knockdown of SCOT inhibits insulin release in rat insulinoma cells. Archives of Biochemistry and Biophysics, 499 (1-2), 62-68. doi: 10.1016/j.abb.2010.05.007

Lower succinyl-CoA:3-ketoacid-CoA transferase (SCOT) and ATP citrate lyase in pancreatic islets of a rat model of type 2 diabetes: Knockdown of SCOT inhibits insulin release in rat insulinoma cells

2010

Book Chapter

Sources of ore fluid components in IOCG deposits

Williams, Patrick J., Kendrick, Mark A. and Xavier, Roberto Perez (2010). Sources of ore fluid components in IOCG deposits. Hydrothermal iron oxide copper-gold and related deposits: a global perspective - advances in the understanding of IOCG deposits. (pp. 107-116) edited by T. M. Porter. Linden Park, SA Australia: PGC Publishing.

Sources of ore fluid components in IOCG deposits

2009

Journal Article

New constraints on the release of noble gases during in vacuo crushing and application to scapolite Br-Cl-I and 40Ar/39Ar age determinations

Kendrick, M. A. and Phillips, D. (2009). New constraints on the release of noble gases during in vacuo crushing and application to scapolite Br-Cl-I and 40Ar/39Ar age determinations. Geochimica et Cosmochimica Acta, 73 (19), 5673-5692. doi: 10.1016/j.gca.2009.06.032

New constraints on the release of noble gases during in vacuo crushing and application to scapolite Br-Cl-I and 40Ar/39Ar age determinations

2009

Conference Publication

Noble gas and halogen evidence for the origin of mineralising fluids in orogenic gold deposits: An example from the Ballarat East Deposit, Australia

Fairmaid, A. M., Kendrick, M. A. and Phillips, D. (2009). Noble gas and halogen evidence for the origin of mineralising fluids in orogenic gold deposits: An example from the Ballarat East Deposit, Australia. 19th Annual VM Goldschmidt Conference, Davos Switzerland, Jun 21, 2009. OXFORD: PERGAMON-ELSEVIER SCIENCE LTD.

Noble gas and halogen evidence for the origin of mineralising fluids in orogenic gold deposits: An example from the Ballarat East Deposit, Australia

2009

Journal Article

Decreased levels of metabolic enzymes in pancreatic islets of patients with type 2 diabetes

MacDonald, M. J., Longacre, M. J., Langberg, E. -C., Tibell, A., Kendrick, M. A., Fukao, T. and Ostenson, C. -G. (2009). Decreased levels of metabolic enzymes in pancreatic islets of patients with type 2 diabetes. Diabetologia, 52 (6), 1087-1091. doi: 10.1007/s00125-009-1319-6

Decreased levels of metabolic enzymes in pancreatic islets of patients with type 2 diabetes

2009

Journal Article

Discussion of 'the Paleozoic metamorphic history of the Central Orogenic Belt of China from 40Ar/39Ar geochronology of eclogite garnet fluid inclusions by Qiu Hua-Ning and Wijbrans J.R.'

Kendrick, M. A. and Phillips, D. (2009). Discussion of 'the Paleozoic metamorphic history of the Central Orogenic Belt of China from 40Ar/39Ar geochronology of eclogite garnet fluid inclusions by Qiu Hua-Ning and Wijbrans J.R.'. Earth and Planetary Science Letters, 279 (3-4), 392-394. doi: 10.1016/j.epsl.2008.12.047

Discussion of 'the Paleozoic metamorphic history of the Central Orogenic Belt of China from 40Ar/39Ar geochronology of eclogite garnet fluid inclusions by Qiu Hua-Ning and Wijbrans J.R.'

2008

Journal Article

New constraints on regional brecciation in the Wernecke Mountains, Canada, from He, Ne, Ar, Kr, Xe, Cl, Br and I in fluid inclusions

Kendrick, M. A., Honda, M., Gillen, D., Baker, T. and Phillips, D. (2008). New constraints on regional brecciation in the Wernecke Mountains, Canada, from He, Ne, Ar, Kr, Xe, Cl, Br and I in fluid inclusions. Chemical Geology, 255 (1-2), 33-46. doi: 10.1016/j.chemgeo.2008.05.021

New constraints on regional brecciation in the Wernecke Mountains, Canada, from He, Ne, Ar, Kr, Xe, Cl, Br and I in fluid inclusions

2008

Journal Article

Metamorphic fluid origins in the Osborne Fe oxide - Cu - Au deposit, Australia: Evidence from noble gases and halogens

Fisher, L. A. and Kendrick, M. A. (2008). Metamorphic fluid origins in the Osborne Fe oxide - Cu - Au deposit, Australia: Evidence from noble gases and halogens. Mineralium Deposita, 43 (5), 483-497. doi: 10.1007/s00126-008-0178-2

Metamorphic fluid origins in the Osborne Fe oxide - Cu - Au deposit, Australia: Evidence from noble gases and halogens

2008

Journal Article

Noble gas and halogen constraints on regionally extensive mid-crustal Na-Ca metasomatism, the Proterozoic Eastern Mount Isa Block, Australia

Kendrick, M. A., Baker, T., Fu, B., Phillips, D. and Williams, P. J. (2008). Noble gas and halogen constraints on regionally extensive mid-crustal Na-Ca metasomatism, the Proterozoic Eastern Mount Isa Block, Australia. Precambrian Research, 163 (1-2), 131-150. doi: 10.1016/j.precamres.2007.08.015

Noble gas and halogen constraints on regionally extensive mid-crustal Na-Ca metasomatism, the Proterozoic Eastern Mount Isa Block, Australia

2007

Journal Article

Comment on 'Paleozoic ages and excess 40Ar in garnets from the Bixiling eclogite in Dabieshan, China: New insights from 40Ar/39Ar dating by stepwise crushing by Hua-Ning Qiu and J.R. Wijbrans'

Kendrick, M. A. (2007). Comment on 'Paleozoic ages and excess 40Ar in garnets from the Bixiling eclogite in Dabieshan, China: New insights from 40Ar/39Ar dating by stepwise crushing by Hua-Ning Qiu and J.R. Wijbrans'. Geochimica et Cosmochimica Acta, 71 (24), 6040-6045. doi: 10.1016/j.gca.2007.01.029

Comment on 'Paleozoic ages and excess 40Ar in garnets from the Bixiling eclogite in Dabieshan, China: New insights from 40Ar/39Ar dating by stepwise crushing by Hua-Ning Qiu and J.R. Wijbrans'

2007

Journal Article

Mid-crustal fluid mixing in a Proterozoic Fe oxide-Cu-Au deposit, Ernest Henry, Australia: Evidence from Ar, Kr, Xe, Cl, Br, and I

Kendrick, M. A., Mark, G. and Phillips, D. (2007). Mid-crustal fluid mixing in a Proterozoic Fe oxide-Cu-Au deposit, Ernest Henry, Australia: Evidence from Ar, Kr, Xe, Cl, Br, and I. Earth and Planetary Science Letters, 256 (3-4), 328-343. doi: 10.1016/j.epsl.2006.12.032

Mid-crustal fluid mixing in a Proterozoic Fe oxide-Cu-Au deposit, Ernest Henry, Australia: Evidence from Ar, Kr, Xe, Cl, Br, and I

2006

Journal Article

Noble gas and halogen constraints on mineralizing fluids of metamorphic versus surficial origin: Mt Isa, Australia

Kendrick, M. A., Duncan, R. and Phillips, D. (2006). Noble gas and halogen constraints on mineralizing fluids of metamorphic versus surficial origin: Mt Isa, Australia. Chemical Geology, 235 (3-4), 325-351. doi: 10.1016/j.chemgeo.2006.08.002

Noble gas and halogen constraints on mineralizing fluids of metamorphic versus surficial origin: Mt Isa, Australia

Past funding

  • 2022
    Evaluation of seafloor-carbonation feedback on atmospheric CO2
    Australian National University
    Open grant
  • 2022
    The halogen composition of subducting oceanic sediments
    Australian National University
    Open grant
  • 2021 - 2022
    Tracking the growth and evolution of the ocean crust using cryptic crystal archives (ANZIC IODP Legacy Analytical Funding, AILAF grant)
    Australian National University
    Open grant
  • 2020 - 2021
    The timing of ocean floor carbonation and global CO2 cycling
    Australian National University
    Open grant
  • 2019 - 2024
    Mantle evolution and the origin of Earth's atmosphere
    ARC Discovery Projects
    Open grant

Availability

Associate Professor Mark Kendrick is:
Available for supervision

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Available projects

  • Geochemistry of SW Pacific Backarc Basins

    Tungsten or boron isotopes in backarc basin basalts, will provide information about the nature of mantle components underlying SW Pacific backarc basins. Previous work suggests these include depleted mantle wedge, subducted components (fluids and melts) and primitive mantle components with high 3He/4He ratios that probably formed early in Earth's history and are expected to have tungsten isotope anomalies. This project is in partnership with Monash University.

  • The volatile content of eclogites and the nature of eclogitic fluid inclusions

    A historical assumption was that volatiles, including noble gases, are almost entirely lost from subducting slabs during metamorphism. However, few studies have quantified the volatile content of eclogite facies lithologies, which is an essential step towards constraining the actual subduction budget. The current project will involve collection of samples from an eclogite terrane such as New Caledonia and characterisation of samples representing dehydrated oceanic crust and metasediments. The aims are to assess the extent to which noble gases and halogens are retained in eclogitic rocks during metamorphism and the degree to which they exchange between adjacent lithologies, which is of additional interest because crustally-derived 'excess 40Ar' is an obstacle to geochronological studies. The project will use a variety of techniques including petrography, fluid inclusion microthermometry, LA-ICPMS and novel 40Ar-39Ar methodologies to measure halogens and noble gases with great precision.

  • Alteration of the oceanic lithosphere: insights from halogens

    The nature of fluids responsible for alteration of the oceanic crust (seawater versus magmatic) and the volatile content of the oceanic crust that is subducted into the mantle exert critical controls on the recycling of elements from the Earth's surface to the mantle. This study will use cutting edge techniques to investigate all four halogens (F, Cl, Br and I) in altered ocean crust recovered by seafloor drilling. This is important because halogens are the dominant ligands that enable metal transport in hydrothermal solution and bromine and iodine are essential elements for life, but there abundances in oceanic crust are poorly known. A combination of in situ and bulk analyses will be used to link the behaviour of halogens to other trace elements and fluid chemistry, and to provide new information about hydrothermal mineralisation and geochemical cycling of elements in the oceanic crust.

  • The timing and duration of seafloor alteration

    Alteration of the oceanic crust controls the composition of seawater and the slab that is subducted into the mantle. It was traditionally assumed that most alteration occurs close to the spreading axis; however, low temperature alteration could influence oceanic crust intermitently throughout its life cycle. This project will characterise alteration in drill cores recovered from the W Pacific and W Atlantic using a range of techniques including SEM and electron microprobe and then investigate the timing of the alteration processes via newly developed U-Pb carbonate dating as well as U-Pb titanite and 40Ar-39Ar geochronology.

  • How salty was the Solar Nebular?

    The relative abundances of different elements in the Bulk Earth provide important clues about how the Earth condensed and accreted in the early solar system (e.g. birth of planets). Most previous studies have suggested halogens are depleted on Earth compared to other elements of similar volatility, implying early loss of halogens by erosion of halogen-rich crustal materials (e.g. collisional erosion) from the young Earth of partitioning into the core. However, this view was challenged by a recent suggestion that halogens have a much lower abundance in the solar system than previously estimated. This study will further explore the findings of Clay et al. by detailed petrographic examination and analysis of halogens in world class examples of major chondritic meteorite types. Electron microprobe and SHRIMP will be used for in situ F and Cl measurements and bulk analyses of Cl, Br and I will be obtained by the noble gas method, which provides uniquely high precision for Br and I measurement and is only possible in a couple of laboratories globally.

Supervision history

Current supervision

Enquiries

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