MODULE 3.2 Flashcards
study of the Earth’s climate before instrumental records were available.
Paleoclimate
The past ______________ years is far more stable than the previous ______________ years.
10,000; 400,000
warmest temperature of Planet Earth
Paleocene-Eocene Thermal Maximum (PETM)
coldest temperature of the Planet Earth
Last Glacial Maximum (LGM)
sits between the warmest and coldest temperature of the Earth
Younger Dryas
The 19th century is then characterized by_____________
rapid warming
Before the 19th century, the temperature was caused by _______________, proven by ________________.
natural variability; paleoclimate archives
During the 19th century, rapid warming is caused by ________________ and _________________.
human activities; instrumental records
These are what paleoclimate scientists use to study past climates, otherwise known as geologic archives. Examples include ice cores, tree rings, sediments, corals, cave deposits, and more.
Paleoclimate archives
physical, chemical, and biological materials preserved within paleoclimate archives that can be analyzed and correlated with climate or environmental parameters in the modern world
Paleoclimate proxies
These are examples of physical proxies
sediment composition, sediment texture, color, density, and magnetic properties
These are examples of chemical proxies
stable isotopes, elemental analyses, biomarkers, and Biogenic Silica
These are examples of biological proxies
charcoal and micro/macrofossils like Pollen, Foraminifera, Ostradoces, Diatoms, Dinocysts, and other Algae, Corals, and Mollusks
Direct measurements from instrumental and historical records have time limitations, specifically spanning ______________ and _______________ years respectively.
100, 1000
Historical records are often ____________________
qualitative and incomplete
____________________ allows scientists to reconstruct a more reliable, consistent story, and longer climate history.
Comparing multiple proxy sources against each other
This paleoclimate archive collects data from oxygen and carbon isotope from bottom dwelling deep sea foraminfera and reveals what climate looked like 70 million years ago.
Deep sea record
Most of the trends from the data are controlled by __________________ and reflect sudden input of _________________ from deep inside the Earth.
tectonic activity; hydrothermal fluids
Global temperatures reached a maximum at about ________________, after which cooling began.
55 million years ago
This cooling resulted from three main events:
- collision of India with Asia
- reduction in seafloor spreading rates
- rise of Andean Mountain
The first half of the Cenozoic likely saw _______________ polar regions.
ice-free
major drivers of climate on the scale of millions of years of change
Plate tectonics
Discuss the implications of fast seafloor spreading
Rapid CO2 input —> Warm greenhouse climate —> Increased chemical weathering —> Increased CO2 removal —> Reduced warming
Discuss the implications of slow seafloor spreading
Slow CO2 input —> Cold greenhouse climate —> Decreased chemical weathering —> Decreased CO2 removal —> Reduced cooling