UvA-TREUB Symposium Advances in Tropical Research

October 18, 2019
WDG

Date: 18th of  October 2019
Location: Institute for Biodiversity & Ecosystem Dynamics, Science Park Amsterdam
Organisers: Dr. Carina Hoorn and Dr. Crystal McMichael (University of Amsterdam)

Programme

14:00-14:10 WELCOME & OPENING

  • 14:10-14:30: Characterization of phytoliths in mid-elevation Andean forests Seringe Huisman (University of Amsterdam/Treub grant awardee)
  • 14:30 –14:50: Extinction-driven changes in frugivore communities on tropical islands: worldwide and in Mauritius Julia Heinen (University of Copenhagen, Denmark)
  • 14:50 – 15:10: Are the current Amazonian fires unprecedented? Crystal N.H. McMichael (University of Amsterdam)
  • 15:10 – 15:30: On the relationship between tiger conservation and water management Jasper Griffioen, Hanne Berghuis & Ewa van Kooten (Utrecht University)

15:30-16:00: TEA

  • 16:00 – 16:45: Assembling the diverse rain forest flora of SE Asia by evaluating the fossil and molecular record in relation to plate tectonics Robert J. Morley (Palynova, and Southeast Asia Research Group, Royal Holloway University of London, UK)

17:00: DRINKS

For full details visit the Treub web site here.

Leaf wax n-alkane patterns of six tropical montane tree species show species-specific environmental response

July 22, 2019
WDG

Open access:

Teunissen van Manen, M., Jansen, B., Cuesta, F., León-Yánez, S. & Gosling, W.D. (2019) Leaf wax n-alkane patterns of six tropical montane tree species show species-specific environmental response. Ecology and Evolution. DOI: 10.1002/ece3.5458

Vegetation responses to late Holocene climate changes in an Andean forest

May 31, 2019
klaasland

Vegetation responses to late Holocene climate changes in an Andean forest
By Klaas Land (currently studying MSc Biological Sciences (Ecology & Evolution) at the University of Amsterdam.

The discussion during the APC meeting on the 19th of March was on the paper by Schiferl et al. (2018), a very recent study on the climatic shifts in the late Holocene and their effects on the South American tropics. The study had analysed a core going back about 3800 years from Lake Palotoa, which was in the Andean foothills (1370m elevation). They found that subtle changes to the fossil pollen record could be identified around the estimated periods for the Little Ice Age (LIA) and Medieval Climate Anomaly (MCA). The focus in the paper Continue Reading

Four centuries of vegetation change in the mid-elevation Andean forests of Ecuador

May 29, 2019
WDG

Huisman, S.N.*, Bush, M.B. & McMichael, C.N.H. (2019) Four centuries of vegetation change in the mid-elevation Andean forests of Ecuador. Vegetation History and Archaeobotany. DOI: 10.1007/s00334-019-00715-8

* Seringe conducted the research presented in this paper during her MSc Biological Sciences at the University of Amsterdam.

New land in the Neotropics

May 6, 2019
WDG

Cuesta, F., Llambi­, L.D., Huggel, C., Drenkhan, F., Gosling, W.D., Muriel, P., Jaramillo, R. & Tovar, C. (2019) New land in the Neotropics: a review of biotic community, ecosystem, and landscape transformations in the face of climate and glacier change. Regional Environmental Change. DOI: 10.1007/s10113-019-01499-3

Cloudy with a chance of adventure

April 8, 2019
WDG

Rachel Sales, Bryan Valencia, and Majoi de Novaes Nascimento coring a different lake. In this picture, we have just pulled a core of mud up from the bottom of the lake. Photo credit: Seringe Huisman

Rachel Sales, Bryan Valencia, and Majoi de Novaes Nascimento coring a different lake. In this picture, we have just pulled a core of mud up from the bottom of the lake. Photo credit: Seringe Huisman

Cloudy with a chance of adventure
By Rachel Sales (PhD researcher at the Institute for Global Ecology, Florida Institute of Technology)

I am sitting on the shore of Lago Condorcillo in Southern Ecuador, after a long day of travel, trying to control my shivering. At roughly 10,500 ft. above sea level, the lake is very cold, with wind that howls over the barren hills dotted with giant boulders. The lake is also almost always blanketed by thick fog and pelted by driving rain. When you’re surrounded by the thick fog punctuated by lightning bolts, it’s easy to believe that some lost civilization lurks just out of sight. Tonight we are experiencing lightning storms, which is adding to the feeling that some angry, ancient life form must live at Lago Condorcillo.

Tomorrow, I will be out in the cold and rain, balancing on an inflatable boat and fighting frostbite. Mark Bush, who is my Ph.D. advisor, Courtney Shadik, who is my lab partner and tent buddy, and I will be collecting cores of mud from the bottom of Condorcillo. We will create our rig for coring by tying two inflatable boats together, and placing a wooden platform between them. Mark, Courtney, and I will then collect our mud cores from this platform.

As I’m contemplating the hazards of camping in a lightning storm, Mark says, “Tell me everything that went wrong today.” Courtney pulls a sleeping bag closer to her. I begin to describe how Google Maps can’t seem to understand distance in the Andes, and so traveling to Lago Condorcillo took much longer than we anticipated. Courtney laughs beside me and adds, “We don’t have any matches to start a fire.” Despite our troubles, I am grinning from ear to ear, no doubt spoiling the grim mood Mark is attempting to cultivate and Lago Condorcillo is doing its best to enforce.

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Amazonia – natural wilderness or abandoned parkland?

April 5, 2019
WDG

Judith being enthusiastic on fieldwork in the Austrian Alps during her Bachelors degree

Amazonia – natural wilderness or abandoned parkland?

By Judith Kirschner (currently studying for MSc Earth Sciences: Geo-ecological Dynamics track at the University of Amsterdam)

In the 4th edition of our “Amsterdam Paleoecology Club” (APC), we discussed ‘A 6900-year history of landscape modification by humans in lowland Amazonia’ by Bush et al. (2006)1. The high-resolution record presented in this paper shows impressively that what we might perceive as native rainforest today could rather be a since a long time actively modified landscape.

The chronology from Lake Sauce (Peruvian Andes) suggests a continuously forested landscape under significant anthropogenic impact over the last 6900 years. Indicators of human activity are taken to be the varying presence of crop pollen (Zea mays) throughout the record, combined with the continuous occurrence of charcoal. Two extra-large fire events are dated at c. 6700 and between 4500-4230 cal BP, probably enhanced by the relatively drier climate of the mid-Holocene. However, it is not clear yet if human actions formed a response to climate change or were part of social and cultural changes.

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