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

Tim Band is a Senior Research Software engineer who will work on the NERC-funded "Beyond Isoplot" project (Standard Grant #NE/T001518/1). This project aims to create a 'software revolution' in geochronology, by building an internally consistent ecosystem of computer programs to account for inter-sample error correlations. The proposed software will modify existing data reduction platforms and create entirely new ones. It will implement a data exchange format to combine datasets from multiple chronometers together whilst keeping track of the correlated uncertainties between them. Before taking on this post, Tim's experience involved numerous programming languages, including C++, Java, Python, JavaScript, TypeScript, C#, Ruby, Go, Haskell and a few others. He has worked on PlayStation games, the Symbian mobile phone operating system, loads of command-line tools, some desktop apps in various frameworks, and back end code with databases like Postgres and MySQL. We are lucky to have such an experienced programmer among us to help improve geochronological data processing at the LGC and beyond.

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

 

The LGC were part of a team of geologists who discovered the first recorded occurrence of vanadium-rich osbornite on Earth, from two sites on Skye, northwest Scotland, which are interpreted as part of a meteoritic ejecta layer. Vanadium-rich osbornite has only previously been reported in space dust from NASA missions, but on Skye it has been identified as an unmelted phase.

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)

Widespread Antarctic glaciation during the Late Eocene

A provenance study of late Eocene marine sedimentary rocks drilled on the southeastern margin of the South Orkney microcontinent in Antarctica (Ocean Drilling Program Leg 113 Site 696) provides the first evidence for a continuity of widespread glacier calving along the coastline of the southern Weddell Sea embayment at least 2.5million yrs before the prominent oxygen isotope event at 34–33.5 Ma that is considered to mark the onset of widespread glaciation of the Antarctic continent.

Carter, A., Riley, T.R., Hillenbrand, C-D, Rittner, M. (2017), Widespread Antarctic glaciation during the Late Eocene, Earth and Planetary Science Letters. 458, 49-57. doi.org/10.1016/j.epsl.2016.10.045.

Matt Fox joins the LGC

Matthew Fox joins the LGC as a NERC Independent Research Fellow. Matthew's work focuses on using thermochronometric data to study a range of earth surface processes from large scale geodynamics to the incision of canyons. Matthew integrates diverse datasets and fieldwork with both inverse and forward numerical models. More information about Matthew's work can be found here here.