If you’re looking for information on my research, you’ve come to the right place. Here you’ll find links to my published articles on the dynamical and chemical evolution of our planet, my CV and a little extra about me and some of my ideas about How The Earth Works.
I am a Cecil and Ida Green Postdoctoral Scholar at the Institute for Geophysics and Planetary Physics, UC San Diego. I research the dynamical and chemical evolution of our planet.
I’m a computational geophysicist who conducts research on mantle convection, volcanism and Earth’s chemical evolution. I grew up in Sydney and earned my BSc from Macquarie University and PhD from the Australian National University. Currently a Green Scholar at UCSD, I was also a Carnegie Fellow at the Carnegie Institution for Science. I was a finalist for the Schmidt Science Fellowship in 2018 and in 2017 I received the Study for Earth’s Deep Interior award for my work on mantle plumes and how they sample the deep mantle.
TD Jones, P van Keken, N Sime (2021). Burying Earth’s primitive mantle in the slab graveyard, Geochemistry, Geophysics, Geosystems, 3, (22), e2020GC009396
TD Jones, R Maguire, P van Keken, J Ritsema, P Koelemeijer (2020). Subducted Oceanic Crust as the Origin of Seismically Slow Lower-mantle Structures, Progress in Earth and Planetary Sciences, 7, (17), 2197-4284
T Mittal, N Knezek, S Arveson, C McGuire, C Williams, TD Jones, Jie Li. (2020). Precipitation of Multiple Light Elements to Power Earth’s Early Dynamo, Earth and Planetary Science Letters, 532, 116030
TD Jones, DR Davies, PA Sossi. (2019) Tungsten Isotopes in Mantle Plumes: Heads it’s Positive Tails it’s Negative, Earth and Planetary Science Letters, 506, pp.255-267
TD Jones, DR Davies, IH Campbell, GI Iaffaldano, G Yaxley, SC Kramer, CR Wilson. (2017) The concurrent emergence and causes of double-track volcanism on the Pacific plate, Nature, 545, pp.472-476
TD Jones, DR Davies, IH Campbell, CR Wilson, SC Kramer. (2016) Do mantle plumes preserve the heterogeneous structure of their deep-mantle source? Earth and Planetary Science Letters, 434, pp.10-17
You can find a complete list on google scholar
You can reach me at email@example.com or on twitter @TimGeophys
Find the podcast here Geology bites
Thanks to Oliver Strimpel and Gillian Fougler for the entertaining and educational podcast. I thought Gillian was engaging and her arguments interesting, but I take mantle plumes to be the best explanation we have for some intraplate volcanism across the globe. Still, I found her impressive, ever the skeptic.
Some of the disagreement is due to the fact that Gillian focuses on an earlier conception of plumes that has since been superseded. For instance, in Morgan’s original paper he suggested that plumes are fixed but later work showed that this need not be the case since the core-mantle boundary (CMB) is not a zero-slip surface. Instead, plumes are able to move, just at a much slower rate than plates due to the high viscosity of the lower mantle. Another is that the volcanic chain associated with a plume must emerge from large igneous provinces (LIP). But Farnetani and Samuel (2005) showed that thermochemical plumes often do not have large heads that melt to form LIPs in the first place. Aside from this, she focuses on aspects of Hawaii, rather than taking a more global perspective which would lend many more observations for an assessment of the plume hypothesis. Here is my response to the rest of her argument.
Gillian says the plume hypothesis makes 5 testable predictions (which she says is based on an email exchange with Ian Campbell 20 years ago):
(1) Initial topographic uplift with the rising plume head. (2) Volcanic track emerges from a LIP or flood basalt. (3) Tail extending to the CMB. (4) Age progressive volcanism following the motion of the overlying tectonic plate. (5) High temperatures.
Her argument is that the plume hypothesis fails all but one of the above criteria, but I don’t think this is the case. I address each point below:
(1) & (2) Gillian dismisses evidence of the first two, uplift and LIP formation, by saying that early Hawaiian volcanism has long been subducted into the mantle, taking any potential evidence of either along with it. I agree, which is why it is odd to focus on Hawaii rather than the many other locations where the evidence for LIP-volcanic track pairs remains intact. See, for example, Deccan and Reunion, North Atlantic and Iceland, Parana and Tristan da Cunha, and Karoo and Marion. See also the point in my opening paragraph regarding the work of Farnetani and Samuel (2005). Note also that there is an indication the Hawaiian plume head was accreted to the forearc of Kamchatka (Portnyaginet et al. 2008).
(3) On evidence for plume tails extending to the CMB, Gillian states that different models result in different conclusions drawn about precisely where the tails are and that therefore there is no “repeatability.” First, many seismic studies do not image plume tails because they lack the resolution required, this was rigorously quantified by Maguire et al. (2018). But some studies do. For example, French and Romanowicz (2015) detected 11 plume tails extending to the CMB using a technique that retains more information from the seismic signal than previous techniques. As for repeatability, that concept applies to making the same measurement under the same experimental conditions. But different models contain different data, make different assumptions, and use different model parameters. Holding these constant, analagous to an experimental setting, you find repeatability.
(4) Gillian says that around 45 million years ago, while the Pacific plate continued to move, volcanism stopped and so too did the age progression of the eruptions. I agree, but come to a different conclusion: volcanism generated by plumes is intermittent, not constant in space and time. Most things in nature are like this. For something to be unchanged there is usually an additional force at work maintaining it. More importantly, when volcanism is actually occurring, it is age progressive, though there will be minor discrepancies as the magmatic plumbing system that transmits melt from mantle to surface is not a well oiled machine.
(5) Gillian agrees the lavas are hot, but that’s only 1 mark out of 5 by her scoring.
So each of the criteria has been tested and met. Yet I doubt these points will convince because Gillian has an additional, philosophical objection to accepting the plume hypothesis as true: that it is superfluous, an ad-hoc addition to an existing theory - plate theory - that already explains the observations as well as, if not better than, mantle plumes. From this perspective, intraplate volcanism is just one more implication of Earth’s tectonically mobile surface.
But this argument contains a misconception. For mantle plumes are also the manifestation of a more general theory, that of mantle convection. It asserts that on geological time-scales the mantle behaves like a viscous fluid that transfers heat through its interior by convection. Accepting this, along with our best estimates of Earth’s physical properties and pressure-temperature conditions, plumes are predicted to arise from a thermal boundary layer at the base of the mantle.
Thus, an account of mantle plumes does not require bolting one theory onto another any more than describing falling objects on the Earth requires a theory of terrestrial-gravity apart from the general theory of relativity; they are merely specific consequences that can be deduced from deeper, more general explanations.
To be sure, we could be wrong about Earth’s physical properties and the conditions it is under. In principle, they need not be conducive to plume formation. If that were the case, we would also need to rethink our account of two fundamental constraints on our planet’s interior: plate motions and surface heat flow, for those too demand a vigorously convecting mantle that is conducive to plume formation. But that is a very different kind of argument to the one proposed. It is one about what we can measure and to what accuracy, as opposed to which theoretical redundancies should be cut by Occam’s razor.
Some final questions for Gillian: Where we see clear signs of rifting, spreading ridges form, not near-point sources of heat. Why? And those ridges must be accommodated for along subduction zones. How do you get rifting at multiple intraplate locations without forming compressional counter-parts between them (which look like mountains on the continents)? Finally, how does the plate model explain the high heat flux and topographic swelling around hotspots, the latter of which is typically used to calculate the buoyancy flux of mantle plumes?
Farnetani, C. G., and Samuel, H. (2005), Beyond the thermal plume paradigm, Geophys. Res. Lett., 32, L07311, doi:10.1029/2005GL022360.
Portnyagin, M., Savelyev, D., Hoernle, K., Hauff, F., Garbe-Schonberg, D., Geology 36, 903–906 (2008)
Maguire, R., Ritsema, J., Bonnin, M., van Keken P. E., & Goes, S. (2018). Evaluating the resolution of deep mantle plumes in teleseismic traveltime tomography. Journal of Geophysical Research: Solid Earth, 123, 384– 400. https://doi.org/10.1002/2017JB014730
French, S., Romanowicz, B. Broad plumes rooted at the base of the Earth’s mantle beneath major hotspots. Nature 525, 95–99 (2015). https://doi.org/10.1038/nature14876