Diana Paola Ochoa L.
Diana Ochoa
Address
ochoad@si.edu
dochoa1709@yahoo.com
Research Interests
My research interests are principally related with palynology (pollen and spores), paleoclimatology and paleoecology, applied to understanding the biodiversity and dynamic of the tropical ecosystems and to biostratigraphy.
Current Research
My current research is focused in understanding the biodiversity changes in neotropical floras during the Paleocene-Eocene Thermal Maximum. For this purpose I’m using palynological samples from NW Venezuela. So far, we had found a surprising increasing in diversity trough this warming period.
Something about PALEOCENE-EOCENE THERMAL MAXIMUM (PETM) EVENT:
It is a geologically brief episode of global warming associated with the Paleocene – Eocene boundary (55.8 million years ago). The PETM is characterized by a globally warming, about 5°C for tropical areas and 8°C for mid and high latitudes. In the geological record this warming period has been associated with a worldwide negative carbon isotope excursion (CIE).
Because the PETM was a natural event that occurred in a brief period of time (100 to 250 kyr), it is an excellent analogue to the modern warming. For this, understanding the causes and consequences of this brief period will give some insight on the behavior and response of the marine and terrestrial biota.
The biotic response on land and in the oceans was heterogeneous in nature and severity, including radiations, extinctions and migrations (Sluijs, 07). For example, there is evidence of an increase in diversity on dinocysts and planktonic foraminifera (Kelly et al. 1998, Crouch and Brinkhuis 2005) but a large extinction rate in benthic foraminifera (Thomas 1998, 2003). Also, a change in mammalian composition is related to it, with the prosimians first occurrence (Gingerich 2006).
However, in terms of flora this event has been studied in high and mid latitudes (Harrington et al. 2004, Wing et al. 2005). However, the response of the terrestrial plants is still unknown, Because of that we had been working in samples from tropical areas (Northern part of South America) trying to understand the behavior and answer of the plant community to this warming.
Education and Degrees
B.S., Geology, Industrial University of Santander, Bucaramanga-Colombia, (2007).
Grants and Fellowships
- American Association of Stratigraphic Palynologist, INC.
Traveling award to attend 12th International Palynological Congress and 8th International Organization of Palaeobotany Conference in Bonn, Germany
July 2008 - American Association of Stratigraphic Palynologist, INC.
Traveling award to attend 40th Annual Meeting in Panama, Panama
September 2007 - Smithsonian Tropical Research Institute - STRI.
Internship Period: April 2007 to December 2008.
Project: Biodiversity changes in Neotropical Floras during Paleocene-Eocene Thermal Boundary - Corporación Geológica ARES
Grants for Undergraduate Projects developed in Geology.
Grant Name: Promoción de Jóvenes Investigadores, Bogotá Abril 2007.
Published Abstracts of Papers Presented at Professional Meetings
- Ochoa, D.P., Contreras, L., Jaramillo, C. Rapid diversification of the tropical rain forest during the PETM in North of South, Oral Presentation, 12th International Palynological Congress and 8th International Organization of Palaeobotany Conference in Bonn, Germany (August, 2008)
- Contreras, L.C., Ochoa-Lozano, D.P., Jaramillo, C.a., Mora, G., Floristic Changes In The Neotropics at The Paleocene/Eocene Thermal Maximum, Abstract for Poster, 40th Meeting AASP in Panama, Panama (October, 2007)
- Ochoa-Lozano, D.P, Torres-Torres, V., and Hoorn, C., 2007. Palinology of deposits from Agua Negra section and geological implications for the NW Amazon Basin. Abstract for Poster, 40th Meeting AASP (October, 2007).
- Ochoa-Lozano, D.P, Torres-Torres, V., and Hoorn, C., 2007. Palinología de los depósitos de la sección Agua Negra e implicaciones en la geología del NW de la Cuenca Amazónica. Abstract for Poster, I Simposio Venezolano de Paleontología y Bioestratigrafía (May, 2007).

