North American ecosystems have fundamentally changed over the late Pleistocene and Holocene; …
North American ecosystems have fundamentally changed over the late Pleistocene and Holocene; from a system dominated by mammoths, to bison, to domestic livestock. Given the very different body size and herd formation of these 'ecosystem engineers', it is likely that animals influence soil structure, water tables, vegetation and other animals in the ecosystems. What has been the ecological influence of the continued 'downsizing' of the largest animals in the ecosystem?
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In this exercise, students will use the Neotoma database and ArcGIS Online …
In this exercise, students will use the Neotoma database and ArcGIS Online to create a distribution map of modern collection localities of beetle taxa associated with an assemblage of fossil beetles from the Conklin Quarry site in eastern Iowa.
a data rich exercise to help students discover how organisms move in response to climate change
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Students will learn how species shift along environmental gradients (temperature, precipitation, and …
Students will learn how species shift along environmental gradients (temperature, precipitation, and vegetation) in response to climate change over the last 20,000 years, from the time of the Last Glacial Maximum through deglaciation and the Holocene. The activity involves making maps of species distribution using the Neotoma database. Students will develop skills in data analysis and interpretation over a two-to-four class arc.
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The overarching goal of this exercise is for students to explore the …
The overarching goal of this exercise is for students to explore the early anthropogenic hypothesis, which claims that early agriculture had a substantial impact on greenhouse gases and global climate thousands of years ago (Ruddiman, 2003). Students compare changes in greenhouse gas concentrations that occurred thousands of years ago to more recent changes that occurred over hundreds of years. Students also relate changes in greenhouse gas concentrations to warming. The exercise is completed over a 1.5- to 2-week period as the class covers a chapter on climate change.
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The Eemian age was the last time the Earth is believed to …
The Eemian age was the last time the Earth is believed to have been warmer than today. However, this warm period occurred with Greenhouse gas concentrations in the atmosphere that were similar to those during the pre-industrial era. Students will use a simplified climate model and with Eemian orbital conditions to try and reproduce this previous warm period. Students will then use modern orbital forcing but elevated greenhouse gas concentrations to look at the modern and future climates. Students will try and understand the differences between these two contrasting warm climates. Eemian and modern warm climates (Acrobat (PDF) 241kB Nov10 16)
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This 4-H project book includes a series of eight activities, focused on …
This 4-H project book includes a series of eight activities, focused on polar science, that youth can complete with an parent or mentor. Each activity includes a hands-on component and options for communication. The activities featured are appropriate for use outside of 4-H, for instance in science classrooms, with after school programs, or during enrichment camps. Each activity includes links to supplemental materials to extend learning.
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Students describe and interpret glacial features exposed in gravel pits and outcrops. …
Students describe and interpret glacial features exposed in gravel pits and outcrops.
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Brian Fagan is an emeritus professor of anthropology at University of California, …
Brian Fagan is an emeritus professor of anthropology at University of California, Santa Barbara who has written several books about past climate change and its effect on the course of European history. His latest book, "The Great Warming," focuses on the Medieval Warm Period (circa 10th to 14th centuries) during which the North Atlantic region experienced an unusually warm climate, and discusses historical events and trends that can be correlated with this climatic change. This assignment uses this book, along with student-retrieved newspaper articles, as the basis for a research paper that addresses the issue of global warming, its effect on past civilizations and its anticipated effect on the future of the citizens of New York City.
Based primarily on "The Great Warming", students address the following questions in a 5 page paper:
What methods and data sources do scientists use to determine climates of the past? How reliable are these various approaches? How was European climate different during the Medieval Warm Period, and how did this climate affect the lives of people in Europe? How was climate different during the Medieval Warm Period for one other region of personal interest, and how did this climate affect the lives of people who lived in that region?
Using information from "The Great Warming" and three to six articles from past issues of a major newspaper, such as the New York Times, students determine probable effects of global warming to the future populations of either their home city, or of the region for which they documented past climate change.
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The is a curriculum module from the project Data Sets and Inquiry …
The is a curriculum module from the project Data Sets and Inquiry in Geoscience Education (DIGS). The module consists of a week-long unit and two-day performance assessment in which students apply the inquiry skills to problem-based investigations of urban micro-climates. The unit and performance assessment present semi-parallel tasks but about different cities (Phoenix and Chicago).
Sudents draw conclusions about the extent to which multiple decades of temperature data about Phoenix suggest that a shift in local climate is taking place as opposed to exhibiting nothing more than natural variability. The data are from the Global Climate Historical Network (GHCN) database. GHCN is a large, multi-year, international project to measure temperature, precipitation, and air pressure from near the ground. Each monthly maximum and minimum temperature is the highest and lowest temperature reading for the month, measured in Celsius. In Phoenix and in most other places, the temperature data are collected at local airports. The performance assessment for this module requires that students apply the methods and findings from the investigation of the climate data for Phoenix to climate data for Chicago. The Chicago data shows less evidence of trends in temperature change, and this is most evident comparing the night-time minimum temperature fluctuations between the two cities. Chicago also exhibits less increase in urban development and population growth than does Phoenix. In contrast to the curriculum unit, which primarily uses constructed-response tasks to encourage student explanation and discussion, the climate assessment tasks pose explicit selected- and constructed-response questions to ensure that the items elicit the intended thinking and hence provide evidence of the targeted standards-aligned skills and understandings.
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This set of investigations focuses on the use of sedimentary facies (lithologies …
This set of investigations focuses on the use of sedimentary facies (lithologies interpreted to record particular depositional environments) to interpret paleoenvironmental and paleoclimatic changes in Neogene sediment cores from the Antarctic margin. Particular attention is given to characteristics of settings close to the ice (ice-proximal) and far from the ice (ice-distal) in high-latitude settings. In Part 1, students build their knowledge of polar sediment lithologies and the corresponding facies through conceptual diagrams, geological reasoning, and use of core images and core logs (a graphical summary of the sediments). In Part 2, the core log for the entire 1285m ANDRILL 1-B core is presented. Students characterize each of the key lithostratigraphic subdivisions and use their knowledge of depositional facies to write a brief history of the Neogene climatic and environmental conditions in the Ross Sea region. In Part 3, students use their core log reading skills and facies knowledge to evaluate patterns in the Pliocene sediments from ANDRILL 1-B. They quantitatively correlate patterns in their dataset with cycles in insolation (incoming solar radiation), influenced by changes in the Earth's orbit during the Pliocene.
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This lab introduces students and other interested users to the Neotoma Paleoecology …
This lab introduces students and other interested users to the Neotoma Paleoecology Database and Neotoma Explorer. Neotoma DB is a public-access and community-supported repository of paleoecological data, mostly from the late Quaternary. These data are widely used by scientists to study species responses to past climate change.
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In this module, participants read a short scenario and answer a series …
In this module, participants read a short scenario and answer a series of questions to emulate the scientific process of making observations and hypotheses. Entitled "Gotta find a better place to fish...", the scenario details observations of biological, environmental, and ecological changes to a mountain stream over time. Participants answer questions that ask them to hypothesize why some of these changes might be occurring and how they are related. Part of the Neotoma Education Modules for Biotic Response to Climate Change.
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In this two part activity, students are introduced to the principals of …
In this two part activity, students are introduced to the principals of ecology and paleoecology and compare modern ecological relationships with prehistoric ones. In part one, students read about ecological principles such as ecological niches and competitive exclusion, and how these principles can be applied to modern and past organisms. Students answer a series of questions that ask them to apply their knowledge of ecological principles. In the second part, students are introduced to non-analogue biotas and complete a set of exercises using the Neotoma Explorer. Part of the Neotoma Education Modules for Biotic Response to Climate Change.
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In this module, students explore and analyze records of past climate. In …
In this module, students explore and analyze records of past climate. In the first part of the module, students are given background information about long-term records of Earth's climate: deep sea sediment cores and ice cores. Students are also introduced to Oxygen isotopes and how they are used as records of past climate. Students complete a set of exercises that assess their understanding of the material and ask them to analyze data about the Laurentide Ice Sheet using the Neotoma Explorer. In the second part of the module, students examine Antarctic ice core data and apply their knowledge from the beginning of the module. Part of the Neotoma Education Modules for Biotic Response to Climate Change.
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In this module, students explore biotic responses to changing climate. The module …
In this module, students explore biotic responses to changing climate. The module steps through different styles of response (i.e. stasis, adaptation, extinction) and provides examples of each from modern biota. Students are given a set of exercises where they create a hypothesis for future mammal distribution changes. Part of the Neotoma Education Modules for Biotic Response to Climate Change.
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Paleoecologists reconstruct past climates and ecosystems by comparing the habits and habitats …
Paleoecologists reconstruct past climates and ecosystems by comparing the habits and habitats preferred by living animals or ones closely related to those found as fossils. In this module, students take the first step in this process by examining modern species distributions to make observations about species habitat preferences. Given a list of species, students use the Neotoma Explorer to obtain species distribution maps and compare them to temperature and precipitation maps. A series of questions guide them through their comparison and analysis of the maps. Part of the Neotoma Education Modules for Biotic Response to Climate Change.
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Animal distributions are frequently controlled by climate extremes, especially seasonal ones. Therefore, …
Animal distributions are frequently controlled by climate extremes, especially seasonal ones. Therefore, if the climate changes from cold to warm (or vice versa) then using modern mammal distributions and modern climate conditions it is possible to make predictions about how the mammal will respond to the climate change -- whether it is past or future. In this module students use the Neotoma Paleoecological Database to test predictions, or establish hypotheses, about how certain species of mammals have responded to climate change in the past and how they might do so on the future. Part of the Neotoma Education Modules for Biotic Response to Climate Change.
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We constructed a project that outlines the students opinion on the role …
We constructed a project that outlines the students opinion on the role of government in protecting and preserving the environment. Please see that attached resource for more information.
This is a unit plan for project-based learning. Students will learn about …
This is a unit plan for project-based learning. Students will learn about paleoclimate proxies and their importance in understanding past climates. Students will focus on one region-specific aspect of paleoclimate and research it. The final outcome will be a public product of relevance to the student, school and community.
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This activity is a digital student workbook that compliments the "Recognizing Patterns …
This activity is a digital student workbook that compliments the "Recognizing Patterns in Earth's Climate History" Lesson. Students will make observations and note patterns they see in sediment cores. Students will make inferences about Earth's climate history based on their observations. This workbook is on Google Slides and can be utilized in a Learning Management System.
Provenance: Molly Ludwick, Kings Mountain Middle School Reuse: This item is offered under a Creative Commons Attribution-NonCommercial-ShareAlike license http://creativecommons.org/licenses/by-nc-sa/3.0/ You may reuse this item for non-commercial purposes as long as you provide attribution and offer any derivative works under a similar license.
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