Bertola, L.D., Jongbloed, H., van, d.G., de Knijff, P., Yamaguchi, N., Hooghiemstra, H., Bauer, H., Henschel, P., White, P.A., Driscoll, C.A., Tende, T., Ottosson, U., Saidu, Y., Vrieling, K. & de Iongh, H.H. (2016) Phylogeographic Patterns in Africa and High Resolution Delineation of Genetic Clades in the Lion (Panthera leo). Scientific Reports 6, 30807. DOI: 10.1038/srep30807

Rull, V. The ‘Anthropocene’: A requiem for the Geologic Time Scale? Quaternary Geochronology. DOI: 10.1016/j.quageo.2016.08.006

Xu, H., Lan, J., Sheng, E., Liu, Y., Liu, B., Yu, K., Ye, Y., Cheng, P., Qiang, X., Lu, F. & Wang, X. (2016) Tropical/Subtropical Peatland Development and Global CH4 during the Last Glaciation. Scientific Reports 6, 30431. DOI: 10.1038/srep30431

Shanahan, T.M., Hughen, K.A., McKay, N.P., Overpeck, J.T., Scholz, C.A., Gosling, W.D., Miller, C.S., Peck, J.A., King, J.W. & Heil, C.W. (2016) CO2 and fire influence tropical ecosystem stability in response to climate change. Scientific Reports 6, 29587. DOI: 10.1038/srep29587

In the news

Ancient ‘massacre’ unearthed near Lake Turkana, Kenya, by Anon. BBC News: Africa

Bronze Age houses uncovered in Cambridgeshire are Britain’s ‘Pompeii’ , by Anon. BBC News: Cambridgeshire

Scientists weigh in on ‘giraffe relative’ fossil by Helen Briggs. BBC News: Science & Environment

Sex with Neanderthals may be the cause of modern allergies, studies suggest by Doug Bolton. Independent: Science

Scientific articles

Patterson, R.T., Huckerby, G., Kelly, T.J., Swindles, G.T. & Nasser, N.A. (2015) Hydroecology of Amazonian lacustrine Arcellinida (testate amoebae): A case study from Lake Quistococha, Peru. European Journal of Protistology 51, 460-469. DOI: 10.1016/j.ejop.2015.06.009

Pitulko, V.V., Tikhonov, A.N., Pavlova, E.Y., Nikolskiy, P.A., Kuper, K.E. & Polozov, R.N. (2016) Early human presence in the Arctic: Evidence from 45,000-year-old mammoth remains. Science 351, 260-263. DOI: 10.1126/science.aad0554

Moseley, G.E., Edwards, R.L., Wendt, K.A., Cheng, H., Dublyansky, Y., Lu, Y., Boch, R. & Spotl, C. (2016) Reconciliation of the Devils Hole climate record with orbital forcing. Science 351, 165-168. DOI: 10.1126/science.aad4132

 

Brown, J.H. (2014) Why are there so many species in the tropics? Journal of Biogeography 41, 8-22. DOI:  10.1111/jbi.12228

Matamoro-Vidal, A., Prieu, C., Furness, C.A., Albert, B. & Gouyon, P. (2016) Evolutionary stasis in pollen morphogenesis due to natural selection. New Phytologist 209, 376-394. DOI: 10.1111/nph.13578

McMichael, C., Piperno, D., Neves, E., Bush, M., Almeida, F. & Mongelo, G. (2015) Phytolith assemblages along a gradient of ancient human disturbance in western Amazonia. Frontiers in Ecology and Evolution 3, 141. DOI: 10.3389/fevo.2015.00141

ter Steege, H. et al. (2015) Estimating the global conservation status of more than 15,000 Amazonian tree species. Science Advances 1. DOI: 10.1126/sciadv.1500936

 

Palaeoecology at UvA and Twente 2015: Teaching and Learning

September 21, 2015
cmcmicha

By Crystal McMichael

The month-long palaeoecology module at UvA is coming to an end. We have had two weeks of lectures and microscope work, an introduction to quantitative palaeoecology, and we just finished a week of fieldwork in Twente, which is in the easternmost part of the Netherlands.

Students working in the field (photo: M. Groot)

Students working in the field (photo: M. Groot)

Will Gosling and I tried something new for the field excursion this year. We split the class into eight groups, and gave each group a set of pollen and phytolith samples from an ‘unknown location’. Unknown in this context means being from one of the eight primary sites that we would visit during the field excursion. The students were required to perform vegetation surveys and characterize soils at each of the primary sites that we visited. The goal of each group was to figure out which location their set of ‘unknown’ samples came from. Basically, we had them doing forensic palynology, with idea that they could then better visualize the different vegetation assemblages seen in the palaeoecological records.
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Tropical Botany in Belize: Part 2 – Las Cuevas

April 1, 2015
nicholasloughlin

Tropical Botany in Belize

By Nick Loughlin

Las Cueavs Forest Reseach Station (Photograph by Anna Turbelin)

Figure 1: Las Cueavs Forest Reseach Station (Photograph by Anna Turbelin)

As mentioned in my last post I have recently returned from a 2 week field course in tropical botany run by the Royal Botanic Garden Edinburgh (RBGE) in conjunction with their MSc course on the ‘Biodiversity and Taxonomy of Plants’. The field course allowed for 10 NERC funded PhD students in relevant fields to accompany the MSc students out to Belize to learn a host of valuable skills in tropical botany and ecology.

To find out what we did read on…

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INQUA 2015: Climate change in the tropical South Pacific during the Late Quaternary

October 27, 2014
WDG

 

inqua-JPPosted on behalf of Prof. David Sear (University of Southampton)

The next INQUA Congress will be held in Nagoya (Japan) on July 27 – August 2, 2015

This is a call for contributions to session P05 on ‘Climate change in the tropical South Pacific during the Late Quaternary’.

The session abstract is as follows:
Establishing well dated, quantitative, highly resolved palaeoclimate data for the major climate systems of the tropical south Pacific has become a research priority owing to the paucity of instrumental data from this critical region of the Earth. Whilst the quantity of proxy climate data for this region is increasing rapidly, compared to records from the Northern Hemisphere there is a surprising paucity especially when considering the importance of this region to global climate. Such information is vital for fully understanding inter-hemispheric climate linkages, global energy fluxes and the long-term evolution of natural climate variability such as the El Nino-Southern Oscillation. The dearth of pre-industrial climate records from this region contributes to large uncertainties associated with future climate change impacts far beyond the south Pacific. This session aims to bring together researchers working on Late Quaternary ocean/climate proxies with those whose research lies in modelling ocean-climate processes and dynamics in the tropical south pacific region, and their implications for global climate.

We hope this session will be of interest to you. If you plan to contribute to this session, please submit your abstract before December 20, 2014 click here.

We hope to see you at INQUA 2015.

Best Wishes,

David Sear, Julian Sachs, Kim Cobb, John Chiang, Peter Langdon – session conveners.

Professor David Sear
Geography & Environment
University of Southampton

PDRA: Past environmental and climate change in West Africa

March 29, 2013
WDG

Full time Post-Doctoral Research Associate, Temporary contract for 36 months, £27,854 – £36,298
Department of Environment, Earth & Ecosystems, Faculty of Science, The Open University

Closing date : 25/04/2013

The PDRA project will descover more about past vegetation and climate change in Lake Bosumtwi (Ghana)

The PDRA project will descover more about past vegetation and climate change in Lake Bosumtwi (Ghana)

We are seeking a PDRA to study past climate and vegetation change in tropical West Africa as part of the NERC-funded “500,000 years of solar irradiance, climate and vegetation changes” project. You will join a multidisciplinary collaborative research team and will work with an international network of project partners. The project will utilise cutting-edge organic geochemical techniques to generate the longest continuous record of fossil pollen chemistry change. The study will build upon previous research into the sediments recovered from Lake Bosumtwi (Ghana). The data generated will shed new light on the role of climate in driving vegetation change in the tropics.

You will already hold a PhD, or be near to completing your PhD, in a relevant scientific discipline with a background in the Earth or Environmental sciences. You must have substantial experience of organic geochemistry or tropical palynology, with well-developed self-management skills and the ability to prioritise effectively.

The PDRA will work with an associated PhD student looking at modern pollen-vegetation relationships in the same region.

The PDRA will work with an associated PhD student looking at modern pollen-vegetation relationships in the same region.

Co-Investigators:
Dr Barry Lomax (University of Nottingham)
Dr Wesley Fraser (Oxford Brookes University)

Project partners:
Prof . Yadvinder Malhi (University of Oxford)
Prof. Mark Sephton (Imperial College London)
Dr Tim Shanahan (University of Texas, Austin)
Dr Stephen Abu-Bredu (Forestry Research Institute of Ghana)

For further particulars click here.
For information on how to apply click here visit The Open University jobs web site.

Associated PhD project.

The PDRA will be part of an international team; partners based at University of Nottingham, Oxford Brooks University, Imperial College London, Oxford University, University of Texas at Austin and the Forestry Research Institute of Ghana

The PDRA will be part of an international team; partners based at University of Nottingham, Oxford Brooks University, Imperial College London, Oxford University, University of Texas at Austin and the Forestry Research Institute of Ghana

Funded PhD studentship: Tropical vegetation, environment and climate

March 21, 2013
WDG

William Gosling

William Gosling pollen trapping in west Africa. A studentship on the new grant will investigate modern pollen-vegeation relationships

Fully funded NERC PhD studentship tied to 500,000 years of solar irradiance, climate and vegetation changes project.
To start October 2013 now avaliable with the Palaeoenvironmental Change Research Group.

Title: Tropical vegetation, environment and climate: The present is the key to the past

Supervisors:
William D. Gosling (The Open University),
Wesley Fraser (Oxford Brookes University),
Barry Lomax (University of Nottingham),
Mark Sephton (Imperial College London) &
Yadvinder Malhi (University of Oxford)

  • Investigate the dynamics of modern tropical forest and savannah ecosystems
  • Training in micro fossil and organic geochemical analysis
  • Develop a comprehensive understanding of modern pollen-vegetation relationships
  • Field work in Ghana, in conjunction with Forestry Research Institute of Ghana
Making pollen traps on field work in Ghana

Making pollen traps on field work in Ghana

Understanding how vegetation responded to past climate change requires the development of well constrained relationships between living floras, environment and climate. This project will help constrain the great uncertainty which exists as to how tropical ecosystems are represented in the fossil record by examining the relationship between modern vegetation and the pollen it produces. The project will analyse modern pollen rain using a combination of traditional microscopic analysis [1] and cutting edge geochemical techniques [2]. We anticipate that the findings will provide new insight into past vegetation and climatic change.

For further information on the project and how to apply see the full advert: NERC PhD advert. Prior to applying please check eligibility for NERC funding by clicking here.

Closing date: 25th April, interviews will be held at The Open University during May.

To find out more about the department, research environment and student life at The Open Univerity visit the Department of Environment, Earth & Ecosystems, the Centre for Earth, Planetry, Space & Astronomical Research (CEPSAR) and OU RocSoc web pages.

Work as part of a larger research team in the UK and abroad.

Work as part of a larger research team in the UK and abroad.

References:

[1] Gosling, W.D., et al., Differentiation between Neotropical rainforest, dry forest, and savannah ecosystems by their modern pollen spectra and implications for the fossil pollen record. Review of Palaeobotany and Palynology, 2009. 153(1-2): p. 70-85.
[2] Lomax, B.H., et al., Plant spore walls as a record of long-term changes in Ultraviolet-B radiation. Nature Geoscience, 2008. 1(9): p. 592-596.

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