Man

Giselle Andrea Astorga

Postdoctoral fellow

Universidad Austral de Chile

Valdivia, Chile

Líneas de Investigación


Taphonomy of southern hemisphere plants. Vegetation reconstructions based on plant macrofossils from lake sediments Modern/fossil leaf cuticles and veins to reconstruct forest structure, and refine pollen-based vegetatation reconstructions

Educación

  •  Plant Science/Palaeobotany, School of Plant Science. Australia, 2016
  •  Biological Sciences (Hons.), Instituto de Geociencias. Chile, 2008

Experiencia Académica

  •   Instructor: First year Botany (KPA100) laboratory Part Time

    UNIVERSITY OF TASMANIA

    Science, Engineering and Technology

    Hobart, Tasmania, Australia

    2011 - 2013

  •   Guest Lecturer Other

    UNIVERSIDAD AUSTRAL DE CHILE

    Ciencias

    Valdivia, Chile

    2015 - A la fecha

  •   Profesor adjunto (ad honorem) Other

    UNIVERSIDAD DE CHILE

    Ciencias

    Valdivia, Chile

    2016 - A la fecha


 

Article (2)

Towards understanding the fossil record better: Insights from recently deposited plant macrofossils in a sclerophyll-dominated subalpine environment

Jordan, Gregory J.; Brodribb, Timothy

Article
Review of Palaeobotany and Palynology  (2016)

Fossil leaves from the last interglacial in Central-Southern Chile: Inferences regarding the vegetation and paleoclimate

astorga, g; Pino M.

Article ISI SCOPUS
Geologica Acta  (2011)

BookSection (1)

Semillas de lleuque en el Sitio Pilauco

Pino, Mario A.

BookSection
 (2008)

ConferencePaper (1)

Postglacial assembly of subalpine plant communities: Tabula rasa or nunatak model?

Jordan, G.; Brodribb, T.

ConferencePaper The Last glacial and post-glacial history of the vegetation from montane regions in the Southern Hemis- phere has been mainly studied from pollen evidence, and most of these studies reveal wide-spread tree- less conditions during these periods. However, it is widely recognised that pollen studies can be relatively uninformative in treeless situations, or determining the past position of treeline and glacial refugia. Plant macrofossil can assist these vegetation studies and provide direct evidence of the presence of a taxon in the paleovegetation mainly because their limited taphonomic transport, and ner taxonomic resolution (Birks, 2001; Jackson and Booth, 2007).
 (2014)

ConferencePoster (2)

Climatic influence in the distribution of non-biting midges (Diptera: Chironomidae) in the Araucanian region, south-central Chile

Martel-Cel, A.

ConferencePoster
 (2017)

How well are subalpine leaves, flowers and fruits represented as fossils?

Jordan, Gregory

ConferencePoster
 (2011)

1
Mario Pino

Director

Instituto de Ciencias de la Tierra

Universidad Austral de Chile

VALDIVIA, Chile

6
Giselle Astorga

Postdoctoral fellow

Instituto Ciencias de la Tierra

Universidad Austral de Chile

Valdivia, Chile