1. Greenhouse Earth

2. The Greenhouse Era 100 Myr Ago The Cretaceous Period of the Mesozoic Era Global Sea Level – 200 m higher than today Shallow seas flooded continental interiors Cretaceous is from the Latin word creta which means chalk

3. Abundant Limestone Deposits Cretaceous Chalk Outcrop in Denmark Cretaceous Limestone Outcrop in Virginia, USA

4. Cretaceous Geography Continental flooding reduced the amount of surface land. No evidence of any permanent ice on Earth, even at the poles.

5. Fossils of Warm Adapted Animals in the Arctic: Reptiles Champsosaur Turtles

6. Fossils of Warm Adapted Animals in the Arctic: Dinosaurs

7. Fossils of Tropical Vegetation in the Arctic: Fossil leaf of a tropical breadfruit tree found in the Arctic

8. Antarctic Dinosaurs Small theropod (6 – 8 ft. tall) related to the raptors and tyrannosaurids

9. Antarctic Dinosaurs Fossil pelvis of a small (6 – 8 ft tall and 30 ft. long) sauropod compared to its giant relative shown below Brachiosaurus

10. Fossil Evidence Fossils of tropical plants and animals –North of the Arctic Circle –South of the Antarctic Circle –Indicate a much warmer Earth Tropical corals extended up to 10 degrees higher in latitude than they do at the present.

11. Cretaceous Polar Regions 20 o C to 40 o C warmer than present-day The Antarctic today is very cold because –High elevation: Lapse-rate cooling with increased elevation –High albedo of the ice which reflects insolation

12. Why Were the Poles So Warm? The simplest explanation is CO 2 levels that were up to 10 times present-day levels.

13. Ocean Heat Transport Hypothesis Today –Deep ocean is filled with cold dense water Sinks in polar regions –A small amount of intermediate depth Atlantic water Comes from sinking of salty Mediterranean Sea water that flows into the Atlantic Warmer water is denser due to high salinity it gains by strong evaporation Changes in the amount of heat transported toward polar regions by the ocean Cause changes in climate

14. Warm Saline Deep Water Filled Ocean Basins 100 Myr Ago Formed in tropics or subtropics Dense due to evaporation Sank deeper than any water near warmer poles Configuration of continents could have caused this –Large seaway near northern branch of the Hadley Cell’s descending air –Dry conditions and evaporation Warm salty bottom water could have - Contributed to poleward heat flux to warm the poles - Reduced the large temperature and density contrast between the surface and bottom ocean which would caused faster overturning and more poleward heat flow.

15. Sea Level Changes and Climate Over tectonic time scales, average sea level has risen and fallen by several hundred meters –Transgressions: Rise in sea level –Regressions:Fall in sea level Small in comparison to the >4000 m ocean depth –Can have significant effects on climate

16. Continental Margins Relatively flat –Sea Level Changes of 1:1000 (vertical to horizontal) A sea level increase of 1 meter could extend as far inland as 1 km (1000 m) –The coastline can move 100’s of km

17. Low Sea Level (Present-Day) Coastline is near the break between the continental shelf and the steeper continental slope Erosion is dominant on continental margins Sediment is carried out to the slope and into the deep ocean

18. High Sea Level Ocean floods the continental shelf to a depth of 200 m or more Sediment is deposited on the submerged shelf

19. Eustatic Sea Level Changes Eustatic refers to global or world-wide Evidence is marine sediments of the same age –Deposited on several continents –At levels well above present-day sea level.

20. Tectonic Causes of Eustatic Sea Level Changes Changes in the volume of ocean ridges Continental Collisions Construction of Volcanic Submarine Plateaus

21. 1. Changes in the Volume of Mid-Ocean Ridges High elevation from heating from below. Submarine lava flows Expansion of rocks due to extreme heat Causes surface of the ocean to rise

22. Ridges Subside with Time Initially anomalously high heat flow causes ridges to stand high above the seafloor As rock moves away from the crest –Rapid subsidence due to heat loss As rock continues to move along the ridge flanks –Rate of heat loss is more gradual After 60 Myr –All excess heat is lost –Ridge elevations are a stable depth of 5500 m (average value)

23. Ridge Depths are Constant with Age Profiles (and volumes) of past ocean ridges can be reconstructed by using a relationship observed in the modern ocean basins. –The average depth of all ridges today is 2500 m below the surface This is used as the initial depth (0 age) –Age of the crust is obtained from paleomagnetic data The ridge crest starts at 2500 depth and gradually deepens with age and increasing distance from the ridge –Rock cools and contracts Ridge Depth = 2500 m + 350 (crustal age) 1/2 (in meters) (at 0 age) (in Myr)

24. Fast Spreading Rates Ridges stand higher –Less time to cool and contract Produce a wider, high elevation (“fat”) profile Reduces the volume of ocean basins displacing water onto the continents Transgressions occur resulting in eustatic sea level changes.

25. Slow Spreading Rates More time for crustal rocks to cool and contract A narrower (“thin”) profile results –Ocean basins are deeper –Less water is displaced Regressions occur resulting in eustatic seal level change

26. Sea Level During the Cretaceous Period Average spreading rates were at least 50% faster than today Evidence of marine transgressions Ocean basins had a lower capacity Sea level was 200 to 300 m higher than today

27. 2. Collisions of Continents Continents “float” on the denser asthenosphere –Lower density granitic bedrock

28. Collision Thickens the Crust A high plateau is formed –Faulting shears off slivers of rock and stacks them on top of each other A subsurface low-density root forms down to 60 or 70 km The crust is double its normal 30 km thickness –Net area of continental crust is lost –Increases the area of the ocean basins Sea level falls

29. India is Colliding with southern Asia The only continental collision within the last 100 Myr First made contact 55 Myr ago Still in progress –Increased area of the ocean by 2 million km 2 –Sea level is about 40m lower than 100 Myr ago when no collisions were occurring

30. 3. Construction of Volcanic Plateaus in the Ocean A large region of 110 to 80 Myr old plateaus is buried beneath a thin layer of marine sediment in the tropical Pacific Ocean Initially high above the nearby seafloor –Heat from volcanic origin Today they are cooler and at lower levels 80 Myr ago they likely displaced more sea water –Sea level was probably 40 m high than today

31. Climate Factors and Sea Level Water Stored in Ice Sheets Thermal Contraction of Seawater

32. Glacial Ice Huge amounts of water stored on land –Sea Level is lower during ice ages Water returns to the sea during interglacial periods –During the last ice age sea level was about 300 m lower than today

33. Sea Level Today... Antarctica’s Ice –Holds enough water to raise sea level 66 meters Greenland’s Ice –Holds enough water to raise sea level 6 m If all the ice on these continents melted, there would be a eustatic sea level increase of 72 meters

34. Thermal Contraction of Seawater Warmer water expands –Oceans 80 to 100 Myr ago would have occupied more space than the cooler ocean water today Cooling of the oceans –Low latitude ocean has cooled slightly in the last 100 Myr –High Latitude Ocean surface and the deep ocean have cooled by 10 o C to 15 o C –Sea level has dropped 7 meters

35. Summary of Sea Level Change Factors When all factors are combined, a sea level decrease of 300 to 440 m is estimated Rates of sediment deposition indicates sea level should only be 100 to 300 m lower This discrepancy (“mismatch”) can be explained by uncertainties in –Past spreading rates –Volcanic plateaus –Sedimentation rates –Other factors

36. Sea Level Change and Climate Changes

37. Higher Sea Levels Flooding of –Continental margins –Interior seaways Continental extremes of climate would be moderated (water heats up and cools slower than land) –Milder, more maritime winters –Cooler summers

38. Falling Sea Level More land is exposed Seasonally climate variations are more extreme

39. Glaciation Summer melting is a major control on the amount of glacial ice on Earth –Cooler summers result in less melting Causes greater climate cooling and glaciation – (a higher albedo) As a result, with higher sea level the moderating effect of water on climate should cause cooler summers with more glaciation –There should be less glaciation with today’s lower sea level

40. Glaciation Mismatch The record of the last 100 Myr shows just the opposite trend. –High sea levels of 100 Myr ago should have aided glaciation, but none occurred –Low sea levels of today should oppose glaciation, but we have ice sheets This mismatch indicates that we should assume that sea level change does NOT control long-term climate change.

41. Asteroid Impacts

42. Frequency of Earth Impacts Inverse relationship between size and frequency of impacts –Largest (>10 km): 50 to 100 Myr frequency Great environmental impacts (e.g., “extinction events”) –Smaller objects impact much more frequently

43. 10 km Diameter Meteorite Impacted 65 Myr Ago Impacted at 20 km per second (72,000 km/hr or 44,712 mi/hr) Created an immense shock wave that traveled outward at the same speed. Seismic waves equivalent to an earthquake 100 to 1000 times stronger than the strongest recorded earthquakes.

44. Chixulub Impact 1 second before impact5 seconds after impact 60 seconds after impact 1000 years after impact

45. A Global Extinction Event Many paleontologists believe that this was a major cause of the non-avian dinosaur extinction. But, not only the dinosaurs suffered extinction. 70% of the living species and 40% of genera became extinct

46. Planktonic Foraminifera Extinction of all but one of 25 species

47. Ammonite Cephalopds All became extinct

48. Evidence of the Impact: Iridium Anomaly World-wide distribution of clay containing the element iridium –Ir is rare in crustal rocks –It is found in much higher concentrations in some meteorites Ocean sediments with a layer of enriched Ir

49. Closeup view of the boundary clay in the Raton Basin, New Mexico Boundary Clay

50. Centered on the Yucatán Peninsula of Mexico 180-km diameter structure Lies beneath layers of sedimentary rock Appears to be the right age Chixulub Meteorite Impact Crater

51. Evidence for an Impact Crater

52. Impact Crater Structure Barringer (“Meteor”) Crater, AZLunar Impact Crater

53. Density Measurements of Rocks Patterns of low density pulverized rock High density rock Consistent with an impact crater

54. Shocked Quartz No, shocked quartz isn't a pyschologically-distressed rock. It is actually a structurally-altered form of quartz that Created by a sudden application of extremely high pressure.

55. Tektites Small pieces of rock that were melted during the proposed impact and hurled into the atmosphere Many are found in Antarctica

56. Deposits of Huge Waves

57. Catastrophic Results Sunlight greatly diminished Earth's surface temperatures were drastically reduced. Sulfuric acid (H 2 SO 4 ) and nitric acid (HNO 3 ) resulted from vaporized rock and atmospheric gases –Both would have contributed to strongly acid rain that might have had devastating effects on vegetation and marine organisms

58. Climatic and Environmental Effects Over longer periods (decades to centuries) the abrupt injection of carbon biomass into the atmosphere by burning: –Increased CO 2 levels –Lead to global warming Large impacts are likely not long-term climate changers