Gary Twinn, our new associate postdoctoral researcher at the LGC, recently completed his PhD at Birkbeck College London. His research focuses on (U-Th)/He thermochronometry, particularly its application in understanding the formation of topographical features. Additionally, Gary is keenly interested in streamlining analytical processes through automation techniques, aiming to reduce toil in analytic research as well as minimising human errors. |
London Geochronology Centre
Gary Twinn joins the LGC
Prof. Yang Li from Peking University joins the LGC
Dr Yang Li is an associate professor in Economic Geology and Geochemistry at Peking University.
His research mainly focuses on the timing and rates of geological process, with a specific emphasis on ore formation, mass extinction and life innovation. Rooted in field geology and driven by research innovations, he develops cutting edge analytical tools to tackle the problems in earth and planetary sciences.
We are glad to have him as an honorary associate professor at the London Geochronology Centre, University College London. He is working closely with Prof. Pieter Vermeesch and others from the LGC.
Further information about Prof. Yang Li can be found from his website at PKU.
Detrital geochronology points to early glaciation of West Antarctica.
Zircon U-Pb data acquired at the LGC, and statistical methods developed
by us, demonstrated that the extent of the West Antarctic Ice Sheet
(WAIS) was larger than previously thought during colder periods in the
Miocene. This means it contributed a lot more to sea-level rise events
millions of years ago than previously thought. This insight will help researchers
more accurately predict the future of the WAIS as the world warms.
The work was carried out by an international team of geoscientists led by Imperial College Prof. Tina van de Flierdt and including LGC scientists Prof. Andy Carter and Prof. Pieter Vermeesch.
Marschalek, J. W., Zurli, L., Talarico, F., van de Flierdt, T., Vermeesch, P., Carter, A., ... & McKay, R. M. (2021). A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude. Nature, 600(7889), 450-455.
How to quantify U-Pb discordance?
In a new Geochronology paper, Vermeesch (2021) shows that the current practice of filtering discordant U–Pb data based on the relative difference between the 206Pb/238U and 207Pb/206Pb ages is just one of several possible approaches to the problem and demonstrably not the best one. An alternative approach is to define discordance in terms of isotopic composition, as a log ratio distance between the measurement and the concordia line. Application to real data indicates that this reduces the positive bias of filtered age spectra. Vermeesch, P., 2021. On the treatment of discordant detrital zircon U-Pb data, Geochronology, 3, 247-257, 2021. |
Tim Band joins the group
Sir David Attenborough visits the lab
On Tuesday April 17, we had the great pleasure of giving a lab tour to Sir David Attenborough, who was the guest of honour at the Kathleen Lonsdale Building reopening ceremony. After a brief introduction to U-Pb, U-Th-He and K-Ar geochronology, our esteemed guest asked the pertinent question as to whether these chronometers could be cross-calibrated. Interestingly, improving such cross calibrations turns out to be one of our top priorities for the coming years! Further information about Sir David's visit to the Department can be found here. |
IsoplotR released to the world
![]() | IsoplotR is a free and open-source substitute for Kenneth Ludwig's popular Isoplot add-in to Microsoft Excel. The program is written in R and includes functions for U-Pb, Pb-Pb, 40Ar/39Ar, Rb-Sr, Sm-Nd, Lu-Hf, Re-Os, U-Th-He, fission track and U-series disequilibrium dating. IsoplotR can be run in three different modes: online, offline and from the command line. Its underlying principles are described in a paper that has been accepted for publication in: Vermeesch, P., 2018, IsoplotR: a free and open toolbox for geochronology. Geoscience Frontiers, doi: 10.1016/j.gsf.2018.04.001. |
Geologists discover 60 million-year-old meteorite impact
Drake, S.M., Beard, A.D.,
Jones, A.P., Brown, D.J., Fortes, D., Millar, I.A., Carter, A., Baca, J. B., Downes, H. (2017) Discovery of a
meteoritic ejecta layer containing unmelted impactor fragments at the base of
Paleocene lavas, Isle of Skye, Scotland. Geology,
https://doi.org/10.1130/G39452.1
High throughput geochronology by automated phase mapping and LAICPMS
The first step in most geochronological studies is to extract dateable minerals from the host rock, which is time consuming, removes textural context, and increases the chance for sample cross-contamination. A collaborative research effort between the LGC and Rocktype Ltd. has developed a new method to rapidly perform in-situ analyses by coupling a fast Scanning Electron Microscope (SEM) with Energy Dispersive X-ray Spectrometer (EDS) to a Laser Ablation Inductively Coupled Plasma Mass Spectrometer (LAICPMS) instrument.
Vermeesch, P., Rittner, M., Petrou, E., Omma, J., Mattinson, C. and Garzanti, E., 2017, High throughput petrochronology and sedimentary provenance analysis by automated phase mapping and LAICPMS, Geochemistry, Geophysics, Geosystems (doi: 10.1002/2017GC007109)
Vermeesch, P., Rittner, M., Petrou, E., Omma, J., Mattinson, C. and Garzanti, E., 2017, High throughput petrochronology and sedimentary provenance analysis by automated phase mapping and LAICPMS, Geochemistry, Geophysics, Geosystems (doi: 10.1002/2017GC007109)
Widespread Antarctic glaciation during the Late Eocene
