
NSF Org: |
EAR Division Of Earth Sciences |
Recipient: |
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Initial Amendment Date: | December 22, 2015 |
Latest Amendment Date: | December 22, 2015 |
Award Number: | 1551429 |
Award Instrument: | Standard Grant |
Program Manager: |
Dena Smith-Nufio
dmsmith@nsf.gov (703)292-7431 EAR Division Of Earth Sciences GEO Directorate for Geosciences |
Start Date: | January 1, 2016 |
End Date: | December 31, 2016 (Estimated) |
Total Intended Award Amount: | $48,822.00 |
Total Awarded Amount to Date: | $48,822.00 |
Funds Obligated to Date: |
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History of Investigator: |
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Recipient Sponsored Research Office: |
2221 UNIVERSITY AVE SE STE 100 MINNEAPOLIS MN US 55414-3074 (612)624-5599 |
Sponsor Congressional District: |
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Primary Place of Performance: |
500 Pillsbury Drive SE Minneapolis MN US 55455-0233 |
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): |
GLOBAL CHANGE, Sedimentary Geo & Paleobiology |
Primary Program Source: |
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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
Non-Technical Abstract
Understanding mechanisms that caused rapid global climate changes in the past is a key problem in paleoclimate research, and is critical for evaluating impacts of ongoing and future climate change. In particular, the role of the tropics in climate shifts remains poorly understood. This grant will provide funding to the University of Minnesota at two campuses: Duluth and Twin Cities, in order to recover a drill core from Lake Chalco, on the southern outskirts of Mexico City. These lake sediments have the potential to provide a half-million year record of North American climate. The core from Lake Chalco is directly relevant to one of the most densely populated urban centers on our planet, Mexico City, home to ~20 million people. The project includes plans to increase public scientific literacy and engagement, building on existing programs in Mexico (museums and mobile classrooms) and Minnesota ("Flyover Country" mobile app), and to organize workshops for local K-12 teachers. A robust plan for evaluation of Broader Impacts is included. This project will contribute to the training of the next generation of geoscientists through the inclusion of students and postdoctoral researchers in the drilling project. This project will foster ties among scientific communities in the U.S., Europe and Mexico, both during drilling and continuing scientific investigations of the Chalco Basin. While the focus of this proposal is recovery of an environmental record, other groups have interest in utilizing the core or the boreholes for a range of studies including volcanic history and hazards, seismic monitoring and earthquake hazard modeling, as well as hydrological monitoring and teaching tools. No funding is provided for these related projects in the current grant.
Technical Abstract
This grant provides funding to recover a drill core from a >350m lacustrine sedimentary sequence contained in the Lake Chalco basin on the southern outskirts of Mexico City in the Basin of Mexico. These sediments have the potential to provide a >500,000 year record of North American climate. This will be a unique climate archive that could develop into the "type sequence" for paleoclimate studies in North America. Chalco is well suited for reconstruction and investigatation of interannual through orbital-scale variations in the North American Monsoon (NAM) and hydrologic variations of the neotropics. Ongoing work indicates that the system records environmental responses to both Milankovitch- and millennial-scale climate forcing. In order to evaluate the relative role of low latitudes in initiating and propagating abrupt global climate changes, information regarding the geographical distribution, patterns and timing of abrupt changes in the tropics is still needed, particularly records to help define the nature of variability in the Intertropical Convergence Zone (ITCZ). Precipitation over the Chalco Basin is determined by the position of the ITCZ and the strength of the NAM. Long-term (orbital) variations in the position of the ITCZ follow insolation. However, Holocene paleoclimatic records show an antiphase pattern in precipitation intensity between the tropical core of the NAM and its northern margins in response to ocean forcing (e.g. Atlantic Meridional Overturn, AMO, and Pacific Decadal Oscillation, PDO). A record from the Chalco basin can be compared with existing long term records to the North and to the South to determine if this antiphase relationship to AMO and PDO forcing existed in earlier interglacials.
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.
This NSF grant to the University of Minnesota provided partial funding for a large project to collect drill core samples from the Mexico City basin. This basin, with a population of 21 million people, has held a lake for hundreds of thousands of years. Over time, sediment layers are deposited in lakes, and each of the sediment layers contains information about the conditions around the lake at the time it was deposited. By collecting core samples, the layers can be analyzed to understand how climate, hydrology, ecosystems, volcanoes, and earthquakes in the region have changed throughout the lifespan of the lake. These analyses provide important evidence to understand these natural processes. The information collected also allows us to better predict and prepare for changes in these processes, and the chance of destructive earthquakes, volcanic eruptions, floods, droughts, and other hazards in the future, all of which are known to be important problems in this region.
The specific activities this NSF grant supported include:
- Shipping materials, tools, and supplies to the site for drilling.
- Travel and other costs for supervisory staff from the drilling facility at the University of Minnesota to be on-site during drilling, to manage the drilling operation, drill core sample handling, logging, and documentation, and other on-site activities.
- Travel and other costs for drilling facility outreach staff to work with University of Mexico researchers on public outreach campaigns, to communicate information about the project to local communities and schools. Two of the posters created for this purpose are included with this report.
- Shipping materials, tools, and core samples (more than 3,500 feet / 1,068 meters) from the drill site to the University of Minnesota drilling facility’s specialized lab for core scanning, logging, and analysis.
- Lab activities at the University of Minnesota drilling facility lab.
Project scientists visited the unique facility at the University of Minnesota as a team twice, each for 10 days at a time. Working 12 hours each day, they analyzed the core samples on specialized lab instruments, and split the core samples open to look at the layers of sediment. They described, interpreted, and photographed the core samples, extracted nearly 5,000 small pieces of sediment out of the layers, and shipped those pieces to their own labs for slower, detailed analyses on other types of instruments to generate additional data. This work on their own lab instruments is still underway at the time of this writing, and will require years of work.
During drilling, the outreach team created two educational posters explaining the goals of the project, the scale of time that scientists hope to be able to gain insight on with the cores, and the methods used to extract cores. These posters were displayed at the drill site for interested passersby and used at several outreach events.
The outreach team ran two major events at local schools. The first, at Escuela Secundaria Técnica no. 43 in Mixquic, 4 km from the drilling site, a GLOBE school, included a presentation and hands-on activity involving core samples taken from Lake Chalco. Myrbo introduced the activity with a presentation about how and why scientists take core samples. The cores were examined by the students with guidance from local teachers, Sandy García León, and Myrbo/Loeffler. Students analyzed the samples and made observations using hand lenses provided by the team.
The second outreach event held with local schoolchildren was located at the historic Estación Sismológica Central, now a UNAM outreach facility, where Myrbo, Loeffler, and UNAM faculty led a mock coring activity, where students constructed their own coring devices and extracted core samples from fake (gelatin) lake sediments, and then analyzed these cores. Instructions for setting up and running this coring activity, along with basic supplies needed for it, were provided to local educators, who report that they have continued to use the activity successfully and frequently since the project first introduced them to it.
A custom digital field trip guide was created and is available in the Flyover Country mobile app as well as via an open application programming interface (api.flyover.umn.edu/guide). This guide not only provides information about the scientific goals and motivations of the project, it also acts as a geologic guide to the Mexico City region by exposing interactive geologic maps, locations of archeological sites, highlighting human/environment impacts like subsidence due to groundwater pumping, and providing information about the many volcanoes that surround the city. This guide can be saved for the user’s devices for offline use in the Flyover Country app. Users are notified that the field guide is available whenever they use the app in the Mexico City area, or by looking at the list of field guides available in the application.
Last Modified: 03/31/2017
Modified by: Anders J Noren
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