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Earth System History GEOL 1020 [15] Announcements More about global geochemical cycles September 30, 2013.

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Presentation on theme: "Earth System History GEOL 1020 [15] Announcements More about global geochemical cycles September 30, 2013."— Presentation transcript:

1 Earth System History GEOL 1020 [15] Announcements More about global geochemical cycles September 30, 2013

2 About plants and carbon fixation….

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4 The photosynthesis-respiration cycle in plants. THIS DIFFERENCE IN BEHAVIOR OF THE BOND STRENGTHS, CAN BE TRACED USING CARBON ISOTOPES!! KNOW THIS BIOLOGICAL SYSTEMS PREFER THE LIGHT ISOTOPE OF CARBON ( 12 C) OVER THE HEAVY ISOTOPE ( 13 C).

5 What is the relationship between burial of plant debris and atmospheric chemistry? The CO 2 and O 2 system CO 2 DOWN  O 2 UP CO 2 UP  O 2 DOWN

6 Respiration “BURNS” organic matter back to CO 2

7 And consumes Oxygen in the process…

8 OXIDATION CO2 formation Rapid burial of organic matter cuts it off from oxygen, therefore no feedback to CO 2 !! KNOW THIS:

9 13 C / 12 C ratio in atmosphere is steady here. 13 C / 12 C ratio in atmosphere is increasing here!

10 PREFERS CARBON-12 Carbon-12 enriched Organic matter gets Buried. Carbon-12 gets Depleted in atmosphere Case Study: Increased plant growth and/or increased carbon burial Oxygen starts to build up.

11 What is the relationship between burial of plant debris and atmospheric chemistry? The CO 2 and O 2 system CO 2 DOWN  O 2 UP CO 2 UP  O 2 DOWN

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13 Time (samples from bottom to top) Amount of CO 2 in atmosphere Case Study: Decreased plant growth and/or decreased carbon burial TEMPERATURE?? IS IT GETTING HOTTER OR COLDER WITH TIME? A. COLDER B. HOTTER

14 time CO 2 in atmosphere Case Study: Decreased plant growth and/or decreased carbon burial TEMPERATURE!! IS IT GETTING HOTTER OR COLDER OUTSIDE? A. COLDER B. HOTTER BECAUSE CO2 IS A GREENHOUSE GAS, IT TRAPS WARMTH AND WARMS THE AIR

15 time OXYGEN LEVELS? time 13 C/ 12 C In atmosphere & sediments Case Study: Decreased plant growth and/or decreased carbon burial OXYGEN LEVELS? A. B. C.

16 time OXYGEN LEVELS? time 13 C/ 12 C In atmosphere & sediments Case Study: Decreased plant growth and/or decreased carbon burial OXYGEN LEVELS? C.

17 OXIDATION CO2 formation Returns Carbon-12 to atmosphere Rapid burial of organic matter cuts it off from oxygen, therefore no feedback to CO 2 !! KNOW THIS:

18 13 C / 12 C ratio in atmosphere is steady here. 13 C / 12 C ratio in atmosphere is increasing here!

19 Mid-Cretaceous

20 RECALL: if CO 2 goes down, O 2 goes up if O 2 goes down, CO 2 goes up More organic carbon burial = left-over HEAVY carbon in atmospheric CO 2. With increasing burial of organic matter, or increasing FLUX (input) into sedimentary reservoir, CO 2 level goes DOWN

21 13 C / 12 C ratio in atmosphere is steady. 13 C / 12 C ratio in atmosphere is increasing! 13 C/ 12 C ratio changes over time COLD WARM

22 In the marine system, the same relationship between increased burial of organic matter in INCREASE in the stable carbon isotope ratio ( 13 C/ 12 C) holds!

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