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1
Intro
2
OVERVIEW
3
STUDY AREA
4
LATE CRETACEOUS DRUMHELLER
5
THE HORSESHOE CANYON FORMATION
6
UNIT 1
7
UNIT 3
8
UNIT 5
9
METHODOLOGIES
10
MODERN SOILS
11
ANCIENT SOILS
12
IN THE FIELD
13
OBSTACLES TO FIELD WORK
14
WHY STUDY PALEOSOLS?
15
SOILS AS PALEOENVIRONMENTAL INDICATORS
16
PETROGRAPHIC STUDY
17
GEOCHEMISTRY
18
PALEOSOLS OF THE HORSESHOE CANYON FM.
19
POORLY-DRAINED PALEOSOLS
20
WELL-DRAINED PALEOSOLS
21
MODERATELY DRAINED PALEOSOLS
22
UNIT 2
23
SUBTROPICAL FOREST
24
UNIT 4
25
THE FAUNAL TURNOVER
26
FAUNAL ASSEMBLAGE
27
NEW DISCOVERIES
28
CONCLUSIONS (1/3)
29
CONCLUSION (2/3)
30
ACKNOWLEDGEMENTS
Description:
Explore the paleoenvironments of the Horseshoe Canyon Formation in this 49-minute lecture from the Royal Tyrrell Museum Speaker Series. Delve into the Late Cretaceous period around Drumheller, Alberta, as Annie Quinney from the University of Calgary presents her research. Learn about various methodologies used in paleoenvironmental reconstruction, including the study of modern and ancient soils, field work techniques, and petrographic and geochemical analyses. Discover the different types of paleosols found in the Horseshoe Canyon Formation and their significance as environmental indicators. Examine the subtropical forest ecosystem of Unit 2 and the faunal turnover observed in Unit 4. Gain insights into new discoveries and their implications for understanding this ancient ecosystem. Originally presented in 2012, this talk offers a comprehensive look at the paleoenvironmental history of this important geological formation.

Reconstructing the Paleoenvironments of the Horseshoe Canyon Formation

Royal Tyrrell Museum of Palaeontology
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