As the majority of Earth’s energy is received at the tropics the region has huge potential to trigger and/or amplify climate change. Elucidating the role of the tropics in global climate change is essential to constraining future climate trajectories. In particular, new understandings are needed on the relationship between climate change in tropical and extra-tropical regions, and the role of ‘tropical’ forcing in causing ice ages, and abrupt climate variability. There is now compelling evidence for major shifts in tropical temperature and precipitation during the Holocene and particularly over the last few millennia, and this has challenged the prevailing view of tropical climate stability during this time. However, the timing, magnitude and expression of these climate perturbations are highly variable, especially across South America.
Lake sediments are widely accessible natural archives of environmental change in the Andes and they have the potential to provide insights into both long- (millennial) and short-term (decadal) changes in climate. In the tropical Andes, palaeolimnological records have provided evidence of changes in the El NiÃ±o Southern Oscillation (ENSO), palaeohydrology and South American monsoon; demonstrating that climate is highly dynamic and modulated by both Pacific and Atlantic Oceans.
PhD project will target a formerly glaciated region in northern Peru at ~5Â°S. The student will generate multi-proxy lake sediment records to track ENSO variability over the last 12,000 years, and to provide evidence of palaeohydological changes since deglaciation. As fundamental questions remain about climate variability in the tropical Andes, especially synoptic-scale mechanisms that cause changes in hydroclimate, the studentship will develop answers and insights into the following questions:
1. What is the timing and frequency of ENSO-driven shifts during the late Holocene?
2. What is the magnitude of centennial and millennial-scale climate events since the deglacial?
3. What are the spatio-temporal linkages between ENSO, equatorial Pacific sea surface temperatures and North Atlantic climate variability?
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Laguna Shimbe, northern Peru (Photo: Andrew Henderson)
There will be two field expeditions to the northern Peru. The key objective of the first field season will be to target specific lakes and identify appropriate locations for coring, as well as undertaking limnological investigations e.g. temperature, conductivity, nutrients, stable isotopes. A joint geophysical survey (bathymetry, seismic sub-bottom profiling, ground penetrating radar) will be undertaken on lakes and wetlands at the site. These data will be acquired and processed in collaboration with a current PhD student who is investigating glacial geomorphology of the region. Results will help identify sediment packages within the lake, and suitable coring locations.
Short cores will be collected during the first field season to establish suitable proxies in the lakes over the last 2000 years. In the second field season, longer cores stretching back through the Holocene will be taken and integrated with previous short cores. Lake sediment analysis will focus on documenting fluxes in clastic and organic material using well-established sedimentological and geochemical techniques (total carbon, organic and inorganic carbon, biogenic silica, magnetic susceptibility, grain size, XRD, scanning Î¼-XRF, colour reflectance, stable isotopes). Chronology for the cores will be established using radiometric dating (210Pb/137Cs) and radiocarbon (14C).
1. Review of existing lake sediment records from the Andes.
2. Training needs analysis.
3. Planning and organisation of field expedition 1.
4. Field expedition – Season 1 (Jan 2021).
5. Multi-proxy analysis of existing and newly collected short sediment cores.
6. Establish 210Pb/137Cs-based chronology.
7. Processing and analysis of geophysical data.
1. Interpretation and synthesis of data from short cores to reconstruct environmental change in northern Peru over the last 2000 years.
2. Planning and organisation of field expedition 2.
3. Field expedition – Season 2 (Jan 2022).
4. Multi-proxy analysis of long sediment cores.
5. Establish preliminary radiocarbon age model.
1. Refine radiocarbon chronology.
2. Complete outstanding multi-proxy analysis.
3. Interpretation and synthesis of data from long cores to reconstruct environmental change in northern Peru since deglaciation.
4. Present results at a significant international conference.
5. Begin write-up of thesis.
1. Finish and submit thesis
2. Write papers based on results
The student will be trained in a broad range of palaeolimnological and geophysical techniques. The student will receive bespoke training in field skills e.g. limnology and sediment coring, and laboratory skills in working with lake sediments e.g. core description, inorganic geochemistry, sedimentology, and chronology. In-house training will be provided in geophysical data acquisition and processing, gaining skills in software packages such as ReflexW and Opendtect. They will also have the chance to attend NERC-recognised short courses on stable isotope analysis, radiocarbon dating and Bayesian chronological analysis, and statistics for geoscientists.
References & further reading
Baker PA, Fritz SC. (2015) Nature and causes of Quaternary climate variation of tropical South America. Quaternary Science Reviews 124: 31-47.
Bird BW, Abbott MB, Rodbell DT, Vuille M. (2011) Holocene tropical South American hydroclimate revealed from a decadally resolved lake sediment ï¤18O record. Earth and Planetary Science Letters 310: 192-202.
Moy CM, Seltzer GO, Rodbell DT, Anderson DM. (2002) Variability of El NiÃ±o/Southern Oscillation activity at millennial timescales during the Holocene epoch. Nature 420: 162-165.
Rodbell DT, Smith JA, Mark BG. (2009) Glaciation in the Andes during the late glacial and Holocene. Quaternary Science Reviews 28: 2165-2212.
Rodbell DT, Seltzer GO, Mark BG, Smith JA, Abbott MA. (2008) Clastic sediment flux to tropical Andean lakes: records of glaciation and soil erosion. Quaternary Science Reviews 27: 1612-1626.
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