Old Rocks
Diamond Member
Past Climates on Earth
"Hark! The faint bells of the sunken city
Peal once more their wonted evening chime!
From the deep abysses floats a ditty
Wild and wondrous, of the olden time".
- Wilhelm Mueller, "The Sunken City", translation from the German
We wish to learn:
Format for Printing
Paleoclimates Causes of change Summary
![](/proxy.php?image=http%3A%2F%2Fwww.globalchange.umich.edu%2Fglobalchange1%2Fcurrent%2Flectures%2Fkling%2Fpaleoclimate%2Fpaleo_fig01.gif&hash=c256b5f9bbe53b4be6611275ab25d301)
Figure 1. Vegetation during glaciation in North America in the last Ice Age. The geologic record indicates several ice surges, interspersed with periods of warming, called "interglacials." (Source: Oak Ridge National Laboratory)
One of the most pressing concerns for humans on Earth today is climate change, and what will happen in the future. Given that the climate is definitely warming, it is logical to ask two questions: First, have such changes happened before in the history of the Earth? And second, what is causing this change? In the next two lectures we will examine past climates (paleoclimates) and the forces that caused them to change. This information will set the stage for asking if the same forces that caused past changes are causing climate warming today, and for making predictions about what will happen in the future (upcoming lecture on climate models).
From abundant geological evidence, we know that only three hundred and fifty years ago the world was in the depths of a prolonged cold spell called the "Little Ice Age," which lingered for nearly 500 years. Twenty thousand years ago, in the middle of the last glacial period, large continental scale ice sheets covered much of North America, Northern Europe, and Northern Asia. Fifty million years ago, global temperatures were so high that there were no large ice sheets at all.
The speed at which climate can change has also recently become clear: Transitions between fundamentally different climates can occur within only decades. In order to understand these variations, we need to reconstruct them over a wide range of temporal and geographical scales. The importance of this task is underlined by the growing awareness of how profoundly human activity is affecting climate. As with so many other complex systems, the key to predicting the future lies in understanding the past
We need to ask several questions: What happened? Why did it happen? Has it happened before? Will is happen again? How do we know about it in the first place? Clickthe image to the right to explore the hypothesized changes in ice cover and vegetation.
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Paleoclimatology
Related readings:
Cultural Responses to Climate Change During the Late Holocene
University of Michigan students can access this Science On-Line article through this link.
Paleoclimatology is the study of past climates. It is a fascinating, multidisciplinary field, combining history, anthropology, archaeology, chemistry, physics, geology, atmospheric, and ocean sciences. Clues about past climate conditions are obtained from proxy indicators (a proxy is a "substitute"), which are indirect forms of evidence that can be used to infer climate. These include:
And many more methods are also being used and developed.
"Hark! The faint bells of the sunken city
Peal once more their wonted evening chime!
From the deep abysses floats a ditty
Wild and wondrous, of the olden time".
- Wilhelm Mueller, "The Sunken City", translation from the German
We wish to learn:
- What do we mean by "paleoclimate"?
- What evidence exists for ancient climate change?
- What causes the climate to change?
![](/proxy.php?image=http%3A%2F%2Fwww.globalchange.umich.edu%2Fglobalchange1%2Fcurrent%2Flectures%2Fkling%2Fpaleoclimate%2Fprint_icon.gif&hash=ed4bcd88192a6bd0e60b0fca2f0b8cae)
Paleoclimates Causes of change Summary
![](/proxy.php?image=http%3A%2F%2Fwww.globalchange.umich.edu%2Fglobalchange1%2Fcurrent%2Flectures%2Fkling%2Fpaleoclimate%2Fpaleo_fig01.gif&hash=c256b5f9bbe53b4be6611275ab25d301)
Figure 1. Vegetation during glaciation in North America in the last Ice Age. The geologic record indicates several ice surges, interspersed with periods of warming, called "interglacials." (Source: Oak Ridge National Laboratory)
One of the most pressing concerns for humans on Earth today is climate change, and what will happen in the future. Given that the climate is definitely warming, it is logical to ask two questions: First, have such changes happened before in the history of the Earth? And second, what is causing this change? In the next two lectures we will examine past climates (paleoclimates) and the forces that caused them to change. This information will set the stage for asking if the same forces that caused past changes are causing climate warming today, and for making predictions about what will happen in the future (upcoming lecture on climate models).
From abundant geological evidence, we know that only three hundred and fifty years ago the world was in the depths of a prolonged cold spell called the "Little Ice Age," which lingered for nearly 500 years. Twenty thousand years ago, in the middle of the last glacial period, large continental scale ice sheets covered much of North America, Northern Europe, and Northern Asia. Fifty million years ago, global temperatures were so high that there were no large ice sheets at all.
The speed at which climate can change has also recently become clear: Transitions between fundamentally different climates can occur within only decades. In order to understand these variations, we need to reconstruct them over a wide range of temporal and geographical scales. The importance of this task is underlined by the growing awareness of how profoundly human activity is affecting climate. As with so many other complex systems, the key to predicting the future lies in understanding the past
We need to ask several questions: What happened? Why did it happen? Has it happened before? Will is happen again? How do we know about it in the first place? Clickthe image to the right to explore the hypothesized changes in ice cover and vegetation.
[paste:font size="4"]
Paleoclimatology
Related readings:
Cultural Responses to Climate Change During the Late Holocene
University of Michigan students can access this Science On-Line article through this link.
Paleoclimatology is the study of past climates. It is a fascinating, multidisciplinary field, combining history, anthropology, archaeology, chemistry, physics, geology, atmospheric, and ocean sciences. Clues about past climate conditions are obtained from proxy indicators (a proxy is a "substitute"), which are indirect forms of evidence that can be used to infer climate. These include:
- Isotopic Geochemical Studies: The study of rock isotopic ratios, ice core bubbles, deep sea sediments, etc.
- Dendochronology: the study of tree rings
- Pollen Distribution: the study of plant types and prevalence from pollen found in sediments, ice, rocks, caves, etc.
- Lake Varves: (like dendochronology, but with lake sediments - a varve is an annual layer of mud in the sediment)
- Coral Bed Rings
- Fossils: Studies of geological settings, etc.
- Historical documents, paintings, evidence of civilizations, etc.
And many more methods are also being used and developed.