43
GEOG5426 Stable isotopes

Class 10, Stable isotopes

Embed Size (px)

Citation preview

Page 1: Class 10, Stable isotopes

GEOG5426 Stable isotopes

Page 2: Class 10, Stable isotopes

November 24

Brief (15-minute) summaries of project topics.

(1) What are the most important features of the modern climate in your region?

(2) What proxies are available in your region, over the time interval specified? How are they related to climate? and

(3) How different were past climates from modern conditions? Why is that important?

Page 3: Class 10, Stable isotopes

S TA B L E I S O T O P E S I N P A L E O C L I M AT O L O G Y

Page 4: Class 10, Stable isotopes

Isotopes are elements with the same number of protons but varying numbers of neutrons.

Page 5: Class 10, Stable isotopes

Stable isotopes are either not radioactive or decay so slowly that their half-lives cannot be measured.

Page 6: Class 10, Stable isotopes

Stable isotopes have the same chemical properties but don’t have the same atomic mass.

Page 7: Class 10, Stable isotopes

O16 O18

Page 8: Class 10, Stable isotopes

Stable isotopes of oxygen

O1699.76%

O180.2%

O170.04%

Page 9: Class 10, Stable isotopes

Photograph: David SifrySMOW standard mean ocean water

Page 10: Class 10, Stable isotopes

Evaporation Condensation

Page 11: Class 10, Stable isotopes

Fractionation

Page 12: Class 10, Stable isotopes

H2O18

H2O18H2O18

H2O18

H2O18

H2O16H2O16

H2O16

H2O16

H2O16

Page 13: Class 10, Stable isotopes

H2O18

H2O18H2O18

H2O18

H2O18

H2O16H2O16

H2O16

H2O16

H2O16

H2O16

H2O16

H2O16

Page 14: Class 10, Stable isotopes
Page 15: Class 10, Stable isotopes

more O18“enriched”

Page 16: Class 10, Stable isotopes

more O18“enriched”

Page 17: Class 10, Stable isotopes

less O18“depleted”

more O18“enriched”

Page 18: Class 10, Stable isotopes
Page 19: Class 10, Stable isotopes
Page 20: Class 10, Stable isotopes

more O18

“enriched”

Page 21: Class 10, Stable isotopes

more O18

“enriched”

less O18“depleted”

Page 22: Class 10, Stable isotopes
Page 23: Class 10, Stable isotopes

“heavy”

Page 24: Class 10, Stable isotopes

“heavy”

“light”

Page 25: Class 10, Stable isotopes

O18

O16

Page 26: Class 10, Stable isotopes

O18

O16

small

Page 27: Class 10, Stable isotopes

O18

O16

small

BIG

Page 28: Class 10, Stable isotopes

O18

O16SMOW

O18

O16sample

Page 29: Class 10, Stable isotopes

“more positive” δO18 = “heavy” = “enriched”for example, ocean water

Page 30: Class 10, Stable isotopes

“more negative” δO18 = “light” = “depleted”for example, glacial ice

Page 31: Class 10, Stable isotopes

Source: Jouzel et al., Journal of Geophysical Research, 1994

Page 32: Class 10, Stable isotopes

Source: Jouzel et al., Journal of Geophysical Research, 1994

“light”

“heavy”

Page 33: Class 10, Stable isotopes
Page 34: Class 10, Stable isotopes
Page 35: Class 10, Stable isotopes

paleothermometer

Page 36: Class 10, Stable isotopes

Source: Bowen and Revenaugh, Water Resources Research, 2003δO18 in precipitation

Page 37: Class 10, Stable isotopes

Source: Bowen and Wilkinson, Geology, 2002

δO18 in precipitation

Page 38: Class 10, Stable isotopes

The “amount effect”: The greater the amount of rainfall, the lower the δO18 of the rainfall.

(i.e., more negative)

Page 39: Class 10, Stable isotopes

O18

O18 O18

O18O16

O16O16

O16O16

Page 40: Class 10, Stable isotopes

O18

O18 O18

O18O16

O16O16

O16O16

O16

O16

“more negative” δO18 = “light” = “depleted”

Page 41: Class 10, Stable isotopes

O18

O18 O18

O18O16 O16

O16

O16

O16

Page 42: Class 10, Stable isotopes

O18

O18 O18O18O16

O16

O16

O16

“more positive” δO18 = “heavy” = “enriched”

Page 43: Class 10, Stable isotopes

Source: Shanahan et al., Science, 2009

less O18

more negative“depleted”

more O18

more positive“enriched”