
NSF Org: |
EAR Division Of Earth Sciences |
Recipient: |
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Initial Amendment Date: | April 2, 2013 |
Latest Amendment Date: | June 1, 2017 |
Award Number: | 1253713 |
Award Instrument: | Continuing Grant |
Program Manager: |
Dena Smith-Nufio
dmsmith@nsf.gov (703)292-7431 EAR Division Of Earth Sciences GEO Directorate for Geosciences |
Start Date: | June 1, 2013 |
End Date: | May 31, 2020 (Estimated) |
Total Intended Award Amount: | $524,985.00 |
Total Awarded Amount to Date: | $604,020.00 |
Funds Obligated to Date: |
FY 2014 = $146,593.00 FY 2015 = $109,885.00 FY 2016 = $73,437.00 FY 2017 = $149,105.00 |
History of Investigator: |
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Recipient Sponsored Research Office: |
4333 BROOKLYN AVE NE SEATTLE WA US 98195-1016 (206)543-4043 |
Sponsor Congressional District: |
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Primary Place of Performance: |
24 Kincaid Hall Seattle WA US 98195-1800 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): |
EDUCATION AND HUMAN RESOURCES, Sedimentary Geo & Paleobiology |
Primary Program Source: |
01001415DB NSF RESEARCH & RELATED ACTIVIT 01001516DB NSF RESEARCH & RELATED ACTIVIT 01001617DB NSF RESEARCH & RELATED ACTIVIT 01001718DB NSF RESEARCH & RELATED ACTIVIT |
Program Reference Code(s): |
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Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.050 |
ABSTRACT
CAREER: Tracking the evolution of grasses and grasslands: using phytoliths to explore evolution-ecology links in deep time
Caroline Stromberg, University of Washington
Grasslands cover 40% of Earth's land surface today, provide habitats for over a billion animals including humans, and greatly influence global climate and the carbon and silica cycles. Understanding the history of the grassland biome is essential for disentangling its complex controls and predicting how natural grasslands and crop plants will respond to ongoing human induced climate change. In recent years, analysis of fossilized plant silica (phytoliths) has shed much needed light on evolutionary and ecological events during the establishment of grasslands. However, gaining further knowledge depends critically on refined methods for identifying specific grass lineages in the fossil record. This CAREER research has two main goals. First, the project will enhance the use of phytoliths for robust taxonomic (the naming of species) and ecological interpretations through the first comprehensive and detailed mapping of grass phytolith shapes in an evolutionary framework, coupled with mapping of other, functionally relevant traits (e.g., photosynthetic pathway) and environmental preferences. Second, project will use this "key" to fossil grass types and ecology to tackle two outstanding questions in grass evolution: (1) When and in what environments did grasses originate and diversify?; and (2) What drove the ecological expansion of grasses with C4 photosynthesis?
To address the first question, the project will study Cretaceous-Paleogene (145-23 million years ago) phytolith assemblages from Argentina to determine the evolutionary relationships between the grasses present, and use this information to determine when the lineage split occurred. Phytolith assemblage analysis and other paleobotanical evidence will help determine what early grass habitats were like. To address the second question, the project will analyze Miocene-Pliocene (23-2.6 million years ago) phytolith assemblages from Kansas to document the ecological expansion of C4 grasses in the Great Plains. The project will infer major C4 grass lineages present, and reconstruct changes in vegetation structure. Direct comparison with stable isotopic data from the section will permit testing of which factors influenced the rise to dominance of C4 grasses. The results of this research program will transform the study of ecosystem change during the last ~70 million years, specifically the assembly of grasslands, and allow evaluation of what processes control grassland evolution, in the past and in the future. It will also contribute fundamentally to archaeology, where phytoliths have long been a principal tool for tracking domestication of crop plants and land use.
The integrated themes explored in this research program--evolution, ecology, and environmental change--will be incorporated into formal and informal education at the middle-school- to graduate-school-level and public outreach. This educational component will be accomplished through (1) inquiry-based labs and activities in my undergraduate courses at University of Washington, (2) research mentoring of one postdoctoral researcher, one graduate student, and at least 7 undergraduates in the lab and field, (3) design of new exhibits at the Burke Museum demonstrating evolution research in action, and (4) an after-school program aiming to engage middle-school girls, which remain minorities in STEM, in evolution-ecology science. The joint research and educational activities proposed here aim to inspire a greater appreciation for the processes that shaped and continue to shape our world, and more broadly, a better understanding of the practice of science and critical thinking in students of all ages.
PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH
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PROJECT OUTCOMES REPORT
Disclaimer
This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.
My research focuses on elucidating the evolutionary history of one of the most important groups of plants alive today, grasses (family Poaceae). Grass-dominated ecosystems now occupy 40% of Earth’s land surface, but likely only emerged in the last ~30 million years, reshaping ecosystems across all continents. To shed light on this remarkable ecological transformation, I use a lesser known type of plant fossil, namely fossilized plant silica (“phytoliths”). Phytoliths form inside and around cells in living plants and can be preserved in the soil after plant tissues decay. Much has been learned, through phytolith studies, about when and where grasses and grasslands first emerge. However, many crucial questions remain that cannot be answered using current ways of interpreting which type of grass each fossil phytolith represents. These methods suffer from being subjective and inexact, resulting in interpretations of how grasses evolved and the composition of ancient grass communities that are at best vague and at worst erroneous.
In this CAREER project, postdoc Tim Gallaher and I, and a large and diverse group of primarily undergraduate students worked to significantly enhance the ability of phytoliths to reconstruct grass lineages and ecology through time. We did so by studying in detail the three-dimensional (3D) shape (and size) of grass phytoliths. Specifically, we designed a protocol for imaging phytoliths from nearly 200 species of species within Poaceae in 3D and converting the images to 3D phytolith models. The shape and size of these 3D models could then be measured and compared (using a method called 3D geometric morphometrics), allowing us to study how the shape and size of grass phytoliths have evolved within the grass family (Poaceae). More importantly, this method makes it possible to compare unknown fossil grass phytoliths to our database and determine with good precision which group of grasses that produced it.
Using this new identification “tool”, we can now answer questions about where and when grasses evolved and diversified, what the earliest grass communities looked like, and study differences in grassland evolution on different continents. For this grant, we have focused on understanding the ecology of some of the earliest grasses that lived ~60 million years ago in Argentina, South America. This work is still underway but preliminary data indicate that they lived in the forest understory or forest margins. We are also studying grasses that were present as Great Plains of North America and Turkey transformed from forests to grass-dominated habitats.
This grant also funded investigation into if the high levels of silica (in the form of phytoliths) deposited in the leaves of living grasses evolved as an adaptation to deterring grazers that emerged as grasslands spread. We found that high silica concentrations most likely did not evolve to deter herbivory on grasses, but instead that high silica levels occur in response to climatic conditions where the grasses grow.
This grant also funded several education and outreach efforts through both UW Biology and the Burke Museum of Natural History and Culture. First, I redesigned my upper-level paleobotany and paleoecology class (Greening of the Earth) to include evidence-based learning and hands-on activities, such as a quarter-long research project on fossils that the students themselves collected on a local field trip to a fossil site. Second, my graduate students and I worked with Burke Museum Education staff to design a free afterschool STEM program for middle-school girls (“Girls in Science”). In this program, 16 girls from diverse backgrounds meet women researchers (faculty, graduate students) once a month during the academic year to do hands-on STEM research activities. This program, which has gradually expanded and changed to reach more students and become more inclusive and diverse, is a success as indicated by front-and-back evaluation. Finally, well over 30 undergraduate students and six graduate students have received research training on this grant, with several students presenting their research at conferences, contributing to manuscripts, and participating in research-related outreach events through the Burke Museum.
Last Modified: 11/20/2020
Modified by: Caroline Stromberg
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