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TRANSCRIPT
ESSI Newsletter Issue one
Issue one
October 2015
Earth Surface Science Institute
SCHOOL OF EARTH AND ENVIRONMENT
ESSI Newsletter Issue 1 October 2015
INSIDE THIS ISSUE
PUBLICATIONS - Read more about
some of our top publications from
the year Page 2 & 3
RESEARCH AWARD WINNER - Dr
Caroline Peacock receives
Houtermans Award Page 4
EVENTS - Find out what we have
been up to over the year Page 4 & 5
LATEST PROJECTS - Read about
some of our new research ventures
Page 6
NEW TO THE TEAM - Meet our new
Fellows Page 7
INTRODUCING THE ESSI NEWSLETTER
Welcome to the first ESSI newsletter. This newsletter is designed to
highlight some of our work, successes, new staff, and events of the last 6
months. The last few months have seen significant change in ESSI. We
say goodbye to some of our longest serving staff; Professor Michael
Krom (retired), Professor Robert Mortimer (new Dean of the School of
Animal, Rural and Environmental Sciences at Nottingham Trent
University), and a more slowly departing Professor Liane Benning
(moving to the Helmholtz Centre Potsdam as Head of Interface-
Geochemistry). We wish them well, and in their place are pleased to
welcome Dr Alex Dunhill and Dr Ben Mills, who bring exciting new
expertise to ESSI as we continue to move onwards and upwards (meet them on
page 7 of this issue).
Professor Simon Poulton, Director of ESSI
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Mass extinction survival is more than just a numbers game: Alex Dunhill
There have been five mass extinction events in the Earth’s history, including climate change caused by volcanoes and an asteroid hit that wiped out the dinosaurs.
In general, geographically widespread animals are less likely to become extinct than animals with smaller geographic ranges, offering insurance against regional environmental catastrophes.
However, research by Dr Alex Dunhill from ESSI and Professor Matthew Wills (University of Bath’s Milner Centre for Evolution) has found this insurance is rendered useless during global mass extinction events, and that widely distributed animals are just as likely to suffer extinction as those that are less widespread.
The fossil record of terrestrial (land-living) vertebrates (including dinosaurs) from the Triassic and Jurassic periods (252-145 million years ago) were explored. It was found that although large geographic ranges do offer insurance against extinction, this insurance disappeared across a mass extinction event that occurred around 200 million years ago (at the Triassic-Jurassic boundary) associated with massive volcanic eruptions and rapid climate change which caused the demise of around 80 per cent of species on the planet.
During this catastrophic event many groups of crocodile ancestors became extinct, which paved the way for the dinosaurs to rise to dominance in the subsequent Jurassic Period.
Dunhill and Wills mapped how the geographical distribution of groups of organisms changed through the Triassic-Jurassic periods. These distribution maps were then compared with changes in biodiversity to reveal the relationship between geographic range and extinction risk.
This is the first study to analyse the relationship between geographic range and extinction in the terrestrial fossil record and the results are similar to those obtained from the marine invertebrate fossil record.
Unlocking secrets of the global carbon cycle: Caroline Peacock
Secrets of the global carbon cycle have been unlocked by scientists in a study investigating how minerals interact at the molecular scale with organic carbon in sediments. The largest reservoirs of organic carbon on Earth are found in rocks, soils and marine sediments. The
Ticinosuchus Fossil by Dr Stephan
Lautenschlager
ESSI continuously publishes ground-breaking research in leading international journals.
Below are some of our most recent key publications. You can read more about some of these papers on pages 2 and 3.
Daines S; Twitchett RJ; Little CTS (2015) Environmental controls on Jurassic marine ecosystems during global warming, Geology, 43, 263-266.
Schmalenberger A, Duran AL, Bray AW, Bridge J, Bonneville S, Benning LG, Romero-Gonzalez ME, Leake JR, Banwart SA (2015) Oxalate secretion by ectomycorrhizal Paxillus involutus is mineral-specific and controls calcium weathering from minerals. Scientific Reports, 5, 12187.
Johnson K, Purvis G, Lopez-Capel E, Peacock C, Gray N, Wagner T, März C, Bowen L, Ojeda J, Finlay N, Robertson S, Worrall F, Greenwell C (2015) Towards a mechanistic understanding of carbon stabilization in manganese oxides. Nature Communications, 6, 7628. Read more at the bottom of pg.2
Chen X, Ling HF, Vance D, Shields-Zhou GA, Zhu M, Poulton SW, Och LM, Jiang SY, Li D, Cremonese L, Archer C (2015) Rise to modern levels of ocean oxygenation coincided with the Cambrian radiation of animals., Nature Communications, 6, 8142.
Read more on pg. 3
Dunhill AM, Wills MA (2015) Geographic range did not confer resilience to extinction in terrestrial vertebrates at the end-Triassic crisis. Nature Communications , 6, 7980. Read more on pg.2
Guilbaud R, Poulton SW, Butterfield NJ, Zhu M, Shields-Zhou GA (2015) A global transition to ferruginous conditions in the early Neoproterozoic oceans, Nature Geoscience, 8, 466-468.
Gomez N, Gregoire LJ, Mitrovica JX, Payne AJ (2015) Laurentide-Cordilleran Ice Sheet saddle collapse as a contribution to meltwater pulse 1A, Geophysical Research Letters, 42, 3954-3962.
Dolan AM, Haywood AM, Hunter SJ, Tindall JC, Dowsett HJ, Hill DJ, Pickering SJ (2015) Modelling the enigmatic Late Pliocene Glacial Event - Marine Isotope Stage M2, Global and Planetary Change, 128, 47-60.
OUR KEY PUBLICATIONS
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carbon in soils and sediments is mixed with minerals, which might act to stabilise it against degradation, leading to the burial of carbon and its removal from the short-term global carbon cycle. However, the interaction between organic carbon and carbon-stabilising minerals is
poorly understood due to the complexity of natural soils and sediments, and the difficulties identifying carbon-mineral interactions at the molecular scale.
The new study has used a water treatment works as a novel controlled environment where the interactions between carbon and minerals (such as manganese oxides) can be observed. The water treatment works filter bed consisted of sands coated with the ubiquitous manganese oxide birnessite and provided an environment where the sediment mineralogy was relatively homogenous in comparison to natural marine sediments or terrestrial soils. This allowed for the interactions between manganese oxide and dissolved organic carbon to be closely monitored. Different types of spectroscopy and thermogravimetric analysis were used to determine the molecular mechanisms responsible for organic carbon uptake at the surface and at depth within the birnessite coatings. Results have shown for the first time that birnessite plays a critical role in carbon stabilisation acting to chemically adsorb organic carbon via carboxyl functional groups present in the carbon moiety and physically trap it within the birnessite layers.
Animals breathe freely for the first time 520 million-years ago: Simon Poulton
Life on Earth may have begun more than 3.5 billion-years ago, but the appearance of eukaryotic life about 2 billion-years ago and multi-cellular life about 800−600 million-years ago are both linked to oxygenation events at the Earth's surface. Following this, a burst of animal forms occurred about 540−520 million-years ago in an event known as the 'Cambrian explosion'. Although a causal link between this radiation of animals and a rise in oxygen was suggested half a century ago, redox conditions in the early Cambrian oceans, especially the deep ocean, remain controversial.
Now, a study shows that the 'Cambrian explosion' was in step with the expansion of oxygenated bottom waters in the global ocean.
The researchers utilised analyses of the redox-sensitive element molybdenum in black shales in order to investigate the extent of ocean oxygenation during the ‘Cambrian explosion’. Prof. Derek Vance, an ETH researcher who was one of the co-leaders of the study, said: “In the modern world, the deposition and isotope fractionation mechanisms of molybdenum in anoxic basins are quite different from those in the oxic open ocean."
Prof. Hong-Fei Ling, a researcher based at NJU who was another co-leader of the study, said: "We analysed molybdenum concentrations and isotopic compositions in sediments deposited between 660 and 520 million-years ago on the Yangtze platform, and also compiled published molybdenum data from about 3.5 billion-years ago to the early Cambrian. Using mass balance models, global marine redox conditions can be quantitatively inferred from these molybdenum records."
"We found that a rise of molybdenum concentrations and molybdenum isotope values in marine sediments coincides with the increasing diversity and ecological importance of both animals and planktonic algae in early
Cambrian," said Prof. Maoyan Zhu at NIGPAS. "All of these life forms peaked around 520 million years ago, which according to our data is when the oxygenation level of the ocean reached modern levels for the first time in Earth history."
Prof. Simon Poulton of UoL, said: "Although surface waters may have been partially oxygenated before the 'Great Oxidation Event', which happened 2.4−2.2 billion-years ago, the deeper ocean remained largely devoid of oxygen until much later in Earth history, but until now we have not known when modern oxygenation levels were first achieved.”
"Although the exact causal links and feedback mechanisms between ocean oxygen levels and eukaryotic evolution are still not clearly understood, this coincidence between the rise of ocean oxygenation level and the Cambrian radiation of animals strongly implies a close relationship," added Prof. Graham Shields-Zhou at UCL. "In the Precambrian ocean, besides suffocation through lack of oxygen, anoxia may have also caused metal nutrient deficiencies and the frequent invasion of toxic H2S-rich waters into the major habitats of animals − the shallow oceans. The key features of the Cambrian explosion, such as large size, active locomotion (including carnivory and bicturbation)may have been restricted until the rise to modern levels of ocean oxygenation."
Scanning electron micrograph
showing intact birnessite
coating on sand grains
Haikouella, the earliest fish-like
chordate from the Lower Cam-
brian Maotianshan shales of
Chengjiang County in Yunnan
Province, China. Credit: Maoyan
Zhu, Nanjing Institute of Geolo-
gy and Palaeontology (NIGPAS)
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Goldschmidt Conference The Earth Surface Science Institute was well represented at the 25
th annual Goldschmidt Conference held in
Prague from 16th – 21
st August.
ESSI researches were showcasing their science though talks and poster presentations during the week-long
conference. Dr Caroline Peacock, Dr Ruza Ivanovic and Dr Andy Bray all have invited talks and Professor Liane
Benning was invited to attend as a keynote speaker giving a talk on ‘Nanoscale Processes and X-Rays in
Geoscience Research’
Research Award Winner Dr Caroline Peacock awarded the European Association of Geochemistry 2015 Houtermans Award
This award is bestowed annually to a scientist no more than 35 years of age or within 6 years of their PhD ‘for a
single exceptional contribution to geochemistry, published as a single paper or a series of papers on a single topic’.
Caroline has been recognised for a series of papers investigating the biogeochemical reactivity and cycling of trace-
metals in terrestrial and marine environments. Her work has been among the first to characterise and quantify the
molecular-level processes occurring at mineral-water interfaces that control the partitioning of trace-metals between
soils and freshwaters, and marine sediments and seawater. These processes ultimately control the abundance and
distribution of both bio-essential metals and toxic contaminant metals in modern and ancient environments, and are
therefore crucial to understanding metal cycling on both a local and global scale. Caroline uses a combination of
laboratory experiments, advanced synchrotron-based spectroscopic techniques and geochemical modelling to
probe the mineral-water interface, and shed new light on the complex behaviour of trace-metals in our environment.
Caroline received her award during the Goldschmidt conference and as part of the honour gave a prize winners
lecture entitled ‘Reactivity and Cycling of Trace-metals in Marine Sediments’ whilst in Prague.
EVENTS There is always a lot going on in ESSI
from weekly research lunches to
hosting conferences.
Palaeontological
Association - 58th Annual
Meeting
This year’s meeting was organised
by Cris Little, Fiona Gill and
colleagues from ESSI. A symposium
was held on 16th December, followed
by the Annual Address and an
evening reception in the Parkinson
Building of the University.
The topic for the Annual Symposium
was 'The photosynthesis revolution:
how plants and photosynthetic micro-
organisms have bioengineered the
planet'.
Keynote Speakers included Professor
Simon Poulton (University of Leeds),
Dr Bettina Schirrmeister (University of
Bristol), Professor Charles Wellman
(University of Sheffield), Dr Nick
Butterfield (University of Cambridge),
Professor Dianne Edwards (Cardiff
University), Professor David Beerling
(University of Sheffield), Professor
Margaret Collinson (Royal Holloway),
and Dr James Riding (British
Geological Survey).
The Annual Address was given by
ESSI member Professor Alan
Haywood .
ESSI Day Each year the institute hosts a
science day, a broad topic is chosen
to interest as many researchers as
possible from across our two
research groups. Speakers are
invited from the institute and around
the UK and Europe to talk about work
related to our chosen topic. The
events are a great opportunity for the
institute members to showcase their
science in a relaxed environment and
to network both across the Institute
and with our visitors.
This year the event was organised by
Caroline Peacock and the theme was
‘Mineral & Organics’. Our visitors
included James Byrne (University of
Tubingen), Martin Palmer (University
of Southampton), Christian Bjerrum
(University of Copenhagen) and
Richard Sanders (NOCS) as well as
talks from ESSI members, Andy Bray,
Liane Benning, Cris Little & Lauren
Gregoire. The day was rounded off
with PhD poster presentations, drinks
reception and dinner. We are now
looking forward to our next ESSI day
in the coming months which will be
themed around ‘all things ice’.
Rock Map Over the past year the School of
Earth and Environment have had
Leverhulme Artist in Residence, Sue
Lawty working across the institutes to
create works of art to represent the
The completed map (Credit T. Aze)
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School’s research. In April ESSI researcher Fiona Gill
and Sue collaborated to build a geological map of
Yorkshire from Yorkshire beach pebbles. First of all the
pebbles needed to be collected, this involved a great day
out at Filey for a team of ESSI volunteers armed with
buckets and rewarded with fish and chips. Once all the
pebbles were collected the rock map was built, with
institute members all volunteering a little bit of time
throughout the day to help with the construction. A BBQ
was held for all the volunteers to celebrate the
completion. Geoscience Seminars Series This year we teamed up with the Institute of Applied
Geosciences (IAG) to put together a fantastic seminar
series which ran throughout the year. The speakers were
arranged by ESSI member Andy Bray and Marco Patacci
from IAG. They did an excellent job of attracting
fascinating speakers from all over the world. Seminars
are followed by a social event giving an opportunity for
institute members to discuss the content on the seminars
with each other and the speaker.
The Kromference This July saw ESSI say goodbye to one of their longest
serving members as Professor Mike Krom took his
retirement. In honour of Mike’s
career at the School of Earth &
Environment ESSI hosted a two
day conference on Nutrient
Cycling on the Modern and
Ancient Earth. A fantastic line
up of speakers were arranged
with Keynote and invited talks
from Robert Aller (Stony Brook
University), Ellery Ingall
(Georgia Tech), Tim Jickells
(University of East Anglia),
Rachel Mills (University of
Southampton), Thanos Nenes
(Georgia Tech), Robert
Raiswell (University of
Leeds), Caroline Slomp
(University of Utrecht),
Clare Woulds (University
of Leeds), Philippe Van
Cappellen (University of
Waterloo, Canada) and
Aubrey Zerkle (St
Andrews University).
The event began with an
icebreaker on the Sunday
evening in the School’s
foyer, delegates were given
the opportunity to meet and
mingle over food and drinks
before the conference
programme began the
following morning. Monday
saw the first two thematic
sessions take place,
Macronutrients in the
Modern Environment chaired
by Audrey Zerkle and Andy
Bray and Redox and
Mineral Controls on
Nutrient Cycling chaired by Romain Guilbaud and PhD
student Jenny Thompson. This was followed by a drinks
reception and poster session where an excellent array of
work was displayed and discussed.
In the evening we held a banquet at the Park Plaza in the
city centre giving
everyone a chance
to unwind after the
day’s events.
During the dinner
some of Mike’s
colleagues spoke
about their
experiences of
working with him
over the years
and a prize for best poster was awarded to Jenny
Thompson for her poster titled ‘Iron and phosphorus
cycling in the ferruginous Lake La Cruz’
Day two of the programme had two further thematic
sessions, Micronutrients in the Modern Environment
chaired by Stefan Lalonde and Aleksandra Mloszeski and
Nutrient Dynamics Through Earth History chaired by
Sasann Henkel and PhD student Kathy Doyle. Following
the final session Prof Krom took the stage for his plenary
session ‘Musings of an itinerant phosphorus geochemist’
where he spoke about his experiences in research over
the years and offered words of advice to those continuing
in the field.
The event was a great
success and enjoyed by all
those who attended
especially Mike. ESSI would
like to wish Mike the best of
luck with his future
endeavours, although we are
sure it will not be long before
we see him again in the
School.
Student registration was
kindly sponsored by the
EAG
Professor Mike Krom
Delegates enjoying the
Icebreaker
PhD Student Kathy Doyle
discussing her research
during the poster session
The conference banquet, Park Plaza
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NEW RESEARCH PROJECTS
Black and Bloom: Understanding melting of
the Greenland Ice Sheet
As part of NERC’s latest round of large grants ESSI’s
Liane G. Benning and Jim McQuaid from ICAS are
joining forces to work on the Black and Bloom project.
With over £500,000 coming to Leeds, the £2.4m project
is being led by Professor Martyn Tranter from the
University of Bristol and includes scientists from the
Universities of Sheffield and Aberystwyth and also
international collaborators from Denmark, the US and
Canada. The Greenland Ice Sheet (GrIS) adds ~1 mm/yr
to sea level, it is said to be the largest driver of sea level
rise. Earlier this year, a House of Lords report highlighted
“momentous” change in Arctic and identified the critical
role of UK
science in
furthering our
understanding
of the
processes
impacting the
polar regions.
The main aim
of Black and
Bloom is to
investigate the
causes of
accelerated
melting of the Greenland ice sheet. Traditionally, it has
been thought that the long range transport of soot from
wildfires in Canada and Siberia, as well as desert dust
cause arctic ice sheets to darken. These darker surfaces
absorb more sunlight, and this may be causing the ice to
melt more quickly. However the story is much more
complicated with coloured algal blooms on snow and ice
now being thought to be important.
“We are really excited about this new project. It not just
follows on from our previous work on the effect of
coloured algal blooms on snow and ice but for the first
time we will be able to span scale by cross-correlating
observations from the small scale of a microbe, a dust or
a soot particle all the way to large scale satellite data and
better understand and model the accelerated rates of
melting observed in Greenland and predict how much
sea level rise will occur in the future” said Liane.
The Black and Bloom team are already making plans for
the first field season on the ice sheet in early summer
2016. As part of the measurement campaign, the Leeds
team will be collecting a whole suite of samples of algae
across their seasonal growth cycle but also making
measurements of mineral dust and black carbon to
quantify the respective contributions to albedo. Together
with Jim – who will be on his first terrestrial bound
Greenland Field trip (he is more often found on board the
UK’s research aircraft) – we will deploy instruments to
continuously monitor atmospheric aerosols, which
contribute to the surface darkening as well as providing
potential nutrients for the algae. Alongside this, filter
The Greenland ice sheet; far from a
pristine white snowscape (Photo credit:
Chris Bellas, University of Bristol)
Green and red algae which darken the surface
CONFERENCE SUCESSES FOR OUR STUDENTS
Congratulations to ESSI students who won awards for their presentations at conferences over the summer
Rhian Rees-Owen won the poster prize at the Past Earth Networks conference in Crewe. The title of Rhian’s poster
was 'Constraints on the hydrological cycle in Antarctica during the Neogene'.
Steffi Lutz won the Student Oral Presentation Award at the 6th Polar and Alpine Microbiology Meeting in České
Budějovice for her talk "Biogeography and functionality of microbial glacial surface communities across the Arctic”.
Maggie Georgieva won the student poster award at the 14th Deep-Sea Biology Symposium for her poster
'Mineralization of polychaete worm tubes at hydrothermal vents: implications for a 430 million-year-old hydrothermal
vent community',
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MEET OUR NEW FELLOWS
Alex Dunhill
Alex joined our team in August 2014 from the University of
Bath. He started his research here with a Royal Commission
for the Exhibition of 1851 Fellowship; however we are
delighted to announce that
he has since been
awarded a Leverhulme
Early Career Fellowship,
meaning that he is now on
a tenure-track position at
Leeds. Alex graduated
from Sheffield and gained
his PhD from the University
of Bristol. His research
focuses on biogeography
of extinction and the accuracy of biodiversity data obtained
from the fossil record.
Ben Mills
ESSI are excited to welcome our new University Academic
Fellow, Dr Ben Mills to the team this September.
Ben is joining us from a
Postdoctoral research
position in marine
biogeochemical
modelling at the
University of Bristol. His
research focuses on the
evolution of Earth’s
environment, particularly
the mechanisms
controlling the rise of
atmospheric oxygen from
trace levels on the early
Earth, to ~21% of the
atmosphere at the present day. This is an active and exciting
field that crosses many disciplinary boundaries, and aims to
answer questions relating to climate stability and planetary
habitability.
Ben has joined us through the University’s 250 Great Minds
scheme which seeks to recruit 250 exceptional University
Academic Fellows by 2017. Last year 76 outstanding
individuals were appointed across the University of which Ben
is one. This is a tenure track position which, upon successful
completion of a structured five year development programme,
will lead Ben to a permanent position as an Associate
Professor.
samples will be collected for analysis back in Leeds
using a range of techniques including mass
spectrometry and electron microscopy to quantify
the composition of these particles.
Funding towards drilling at Mochras B
The International Continental Scientific Drilling
Programme (ICDP) has set aside $1.5 million in
funding towards drilling at Mochras B, an Early
Jurassic succession of sediments on the north
Wales coast. A team from ESSI led by Rob Newton
and including Cris Little, Simon Poulton and Paul
Wignall has been actively involved with putting this
proposal together. The project as a whole is being
led by Steve Hesselbo from the University of
Exeter. Additional co investigators include scientists
from Oxford University and the British Geological
Survey. The funding from ICDP will be received on
the basis that the UK team can arrange funding for
the remaining drilling costs and scientific
investigations. The team are working towards a
large grant proposal which will be submitted to
NERC in November.
The Past Earth Network
The EPSRC has provided 3 years funding to
develop the Past Earth Network (PEN). This
network will use palaeoclimates as a basis for
testing our understanding of mechanisms of climate
change. They will promote a thorough assessment
of uncertainty in climate models and a quantification
of the uncertainty around palaeo data by bringing
together statisticians, climate scientists and
geologists.
The idea behind this initiative is to support the
creation of new collaborations and link the
disciplines of mathematics and environmental
science .
This network is being led by ESSI member Alan
Haywood and Jochen Voss from the School of
Mathematics.
The Past Earth Network held its opening
conference in January this year. The conference
saw over 80 members of the network come together
to begin discussions and set up working groups for
their four themes, Quantification of error and
uncertainty of data, Quantification of uncertainty in
complex models, Methodologies which enable
robust model-data comparison and Forecasting and
future climate projections.
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School of Earth and Environment
Institute Director, Professor Simon Poulton
School of Earth & Environment
Leeds, LS2 9JT, UK
www.see.leeds.ac.uk/research/essi/
Twitter @ESSILeeds
Newsletter compiled by Claire McLoughlin