AGU 2016

I will be at AGU for the whole week.  On Monday afternoon I will presenting work we have been doing combining new Fe-XANES observations and thermodynamic models of mantle melting to understand solid Earth redox.  On Wednesday afternoon Paula Antoshechkina will be presenting our preliminary model incorporating carbonate melting into the pMELTS thermodynamic framework.  See you in San Francisco!

The solid Earth’s involvement in oxygen cycling: Observations and theory

Authors: Oliver Shorttle, Edward Stolper, Paula Antoshechkina, Paul Asimow, Eleanor Jennings, Glenn Gaetani, David Graham, Margaret Hartley, Helen Williams, Maryjo Brounce, Saemundur Halldorsson

Session: V13B Magmatic and Tectonic Influences on Elemental Cycling and Earth’s Climate and Oxidation State Posters

When/where: Monday 12th December, 13:40 – 18:00 in Moscone South – poster hall

We have undertaken a targeted study of basalts erupted along the South East Indian Ridge to test the relative controls of mantle temperature and chemical heterogeneity on Fe3+/ΣFe.  Among this suite of basalts there is short length scale heterogeneity and a long wavelength transition to cooler mantle.  Despite these factors, the Fe3+/ΣFe and the oxidation state of erupted basalts is remarkably uniform.  This result suggests that basalt  fO2 is being buffered during mantle melt extraction.

Silicate and Carbonatite Melts in the Mantle: Adding CO2to the pMELTS Thermodynamic Model of Silicate Phase Equilibria

Authors: Paula Antoshechkina, Oliver Shorttle

Session: V33C Deep Carbon: From the Mantle to the Surface and Back Again III Posters

When/where: Wednesday 14th December, 13:40 – 18:00 in Moscone South – poster hall

The transport of carbon in the mantle via carbonated melting of peridotite is critical for the solid Earth volatile cycle, yet most models of mantle melting only consider the thermodynamics of silicate melting and treat carbon as a trace species.  To address this issue and form a self-consistent thermodynamic description of carbonated peridotite melting we have expanded and updated the CO2-fluid database constructed by Ghiorso and Gualda (2012, 2015) to include more recent high pressure experiments.  In the initial stages of calibrating the model a key question we will answer is whether a Na2CO3 liquid component is required in addition to CaCO3.

AGU 2015

I will be at AGU for the whole week: on Thursday speaking about work we have been doing combining geochemical and geophysical indicators of mantle potential temperature to understand what drives melting anomalies on Earth; followed by a talk on Friday presenting some early results investigating the thermodynamics of melt transport and the chemical signals this produces in basalts. On Wednesday Simon Matthews has a poster with new Al-olivine thermometry data from Iceland and neat modelling results showing how petrological estimates of crystallisation temperature can be used to estimate mantle potential temperature – the essence: mantle lithology matters!

Lithology and temperature: How key mantle variables control rift volcanism

Authors: Oliver Shorttle, Mark Hoggard, Simon Matthews, John Maclennan

Session: T44C: Tectonic, Magmatic, and Geodynamic Studies of Extensional Processes: Applications in Iceland and the Nubia-Somalia-Arabia Plate System II

When/where: Thursday 17th December, 16:15 in Moscone South 304

Here we pick apart the various roles of mantle potential temperature and source composition in generating melting anomalies on Earth.  Taking Iceland as a case study, we show how crustal production rates (a proxy for melt flux) and estimates of the enriched-lithology’s melt supply to the crust can be used to constrain the source composition.  Knowing the source composition we can then make more accurate estimates of the thermal structure of the melting region, and so invert petrological estimates of crystallisation temperature into mantle potential temperature. Irrespective of Iceland’s source composition, the mantle must represent a thermal anomaly of at least 100ºC.

We extend our analysis to rifting globally by using a compilation of continental margin crustal thickness estimates. By making reasonable assumptions about mantle source composition, these crustal thickness estimates track the post break-up thermal evolution of the mantle. These observations allow us to evaluate the hypothesis that even away from plumes continental insulation drives up mantle potential temperature prior to rifting. However, the crustal thickness records provide little evidence for a long term increase of mantle temperature due to continental insulation: either it decays rapidly following break-up, or was not generated during the pre-break-up lifetime of the continent.

Geochemical constraints on magma formation and transport processes

Authors: Oliver Shorttle, Paula Antoshechkina, Paul Asimow, Rajdeep Dasgupta, John Rudge

Session: DI51C: Melt and Liquids in Earth and Planetary Interiors II

When/where: Friday 18th December, 08:30 in Moscone South 303

The key question motivating this work is what proportion of geochemical diversity in basalts can be attributed to the melt transport history a given melt has experienced? The implications of this question are broad, as it leads to us questioning the origin of geochemical differences observed between ocean islands and mid-ocean ridges, or as a function of spreading rate and mantle potential temperature: Are these various tectonic regimes driving different styles and rates of melt transport that map into geochemical differences?

To answer these questions we performed some simple calculations of focussed melt flow to quantify the geochemical diversity generated just from varying the amount of melt focusing.  We observe a significant response in terms of the major and trace element chemistry of basalts, suggesting that some portion of local geochemical variability could be mapping in the diverse transport history melts have experienced through the mantle.

The Temperature of the Icelandic Mantle Plume from Aluminium-in-Olivine Thermometry

Authors: Simon Matthews, Oliver Shorttle, John Maclennan

Session: DI31B: Melt and Liquids in Earth and Planetary Interiors

When/where: Wednesday 16th December, 08:00 in Moscone South – Poster Hall

Petrological estimates of mantle potential temperature are a key observation underpinning our models of mantle geodynamics. However, the process of going from the direct observable, a crystallisation temperature, back into a mantle potential temperature is not straight forward. A crystallisation temperature at the very list gives a minimum bound on the mantle temperature, but depending on the thermal history of the magma that crystal grew from, and the magma’s origin within the melting region, that temperature could be 100ºC less than the temperature of initial mantle melting.  To recover the mantle temperature before melting requires a model for the thermal evolution of the mantle during decompression and partial melting.

Here we combine a multi-lithology model of mantle melting with new Al-olivine thermometer estimates for the crystallisation temperature of forsteritic Icelandic olivines. By using geochemical and geophysical constraints on melt production we are able to arrive at a valid range of potential temperatures for the Icelandic mantle that are consistent with available observations.  Combining constraints in this way enables us to propagate uncertainty through relevant model parameters and analytical uncertainty on the crystallisation temperature, to obtain rigorously defined uncertainties. All viable model solutions show the Icelandic mantle to be significantly hotter than typical mid-ocean ridge mantle.


AGU 2014

Come and find me or any of my collaborators at AGU this year to discuss our latest results.  Margaret Hartley and I have some great new XANES data collected at Diamond Light Source probing fO2 in enriched mantle domains and tracking its evolution during magmatic processes. I have an invited talk in V038: The Geochemical Diversity of the Mantle Inferred from Hotspots: Five Decades of Debate, where I will present evidence for the ubiquity of concurrent mixing and crystallisation in destroying the primary chemical diversity leaving the mantle at mid-ocean ridges. With Mark Hoggard’s fantastic record of dynamic support in the world’s ocean basins, we have begun to reconstruct spatio-temporal variability in mantle potential temperature over the last 100Ma.

Controls on OIB and MORB Geochemical Variabilty

Authors: Oliver Shorttle & John Maclennan

Concurrent mixing and crystallisation is visible on a local scale looking at melt inclusion and whole rock suites. Here we show that this basic magmatic process extends not only off of Iceland onto the adjacent Reykjanes Ridge, but by spatial statistical analysis can be seen to be present in global MORB datasets. Homogenisation of primary mantle chemical diversity is therefore a ubiquitous phenomenon occurring in magmatic systems. Understanding how this operates is going to be key for reconstructing mantle compositional diversity.

Authors: Oliver Shorttle & Yves Moussallam, Margaret E Hartley, Marie Edmonds, John Maclennan and Bramley J Murton

Recent evidence from Cottrell and Kelley (2013) has indicated that the mantle heterogeneity sampled by MORB and typically identified from studying radiogenic isotope tracers, may also be associated with redox heterogeneity in the mantle. This compelling observation has major implications for the flux of redox sensitive elements throughout the Earth system, for mantle dynamics, and for the melting process itself. In this work we have characterised the changes in mantle fO2 that occur towards the Iceland plume using a suite of basalt samples.

Authors: Margaret E Hartley, Oliver Shorttle, John Maclennan, Yves Moussallam and Marie Edmonds

Melt inclusions record the primary diversity of melts leaving the mantle in terms of their trace and isotopic compositions, and there is the potential for melt inclusions to also record redox heterogeneity of the source.  However, post entrapment processes such as diffusion and crystallisation may compromise the melt inclusion record, resetting melt inclusion fO2 during shallow level processes. To investigate the potential of the melt inclusion archive in terms of fO2 we have studied a suite of melt inclusions from the AD 1783 Laki eruption, Iceland.

A History of Global Mantle Potential Temperatures from Oceanic Crustal Thicknesses

Authors: Mark Hoggard, Nicholas J White and Oliver Shorttle

We know from geophysical observations of gravity anomalies and petrological measurements on primitive basalts that mantle potential temperature is likely to vary by several hundred degrees in the modern Earth.  A record of potential temperature variation in the past is preserved in the crustal thickness of old seafloor, which will be thicker if high potential temperatures during its formation increased melt production. Here, we use Mark’s extensive compilation of reflection and wide-angle seismic profiles to constrain crustal thicknesses throughout the oceanic realm. These observations when combined with a mantle melting model allow us to back out a unique record of spatio-temporal syn- and post-rift variations in mantle temperature.