joint airapt-18 & hpcc-11 beijing, china -- 23-27 july 2001

28
Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001 High Pressure and the Origin of Life Robert Hazen, Nabil Boctor, Jay A. Brandes, George D. Cody, Russell J. Hemley, James Scott, Anurag Sharma, and Hatten S. Yoder, Jr. Carnegie Institution of Washington

Upload: tea

Post on 14-Jan-2016

43 views

Category:

Documents


2 download

DESCRIPTION

High Pressure and the Origin of Life. Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001. Robert Hazen, Nabil Boctor, Jay A. Brandes, George D. Cody, Russell J. Hemley, James Scott, Anurag Sharma, and Hatten S. Yoder, Jr. Carnegie Institution of Washington. - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

Joint AIRAPT-18 & HPCC-11Beijing, China -- 23-27 July 2001

High Pressure

and the Origin of Life

High Pressure

and the Origin of Life

Robert Hazen, Nabil Boctor, Jay A. Brandes, George D. Cody, Russell J. Hemley, James Scott,

Anurag Sharma, and Hatten S. Yoder, Jr. Carnegie Institution of Washington

Page 2: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

High-Pressure and the Origin of Life

High-Pressure and the Origin of Life

• What is the nature and distribution of life at high pressures?

• What are the extreme pressure limits to cellular life?• How might biomolecules adapt to high

pressure?•What roles might pressure have played

in prebiotic organic synthesis?

Page 3: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

High-Pressure LifeHigh-Pressure Life

HMS Challenger – 1870s

Page 4: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

High-Pressure LifeHigh-Pressure Life

1972

Page 5: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

High-Pressure LifeHigh-Pressure Life

Deep-Sea HydrothermalVents -- 1979

Page 6: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

High-Pressure LifeHigh-Pressure Life

Discoveries of Hydrothermal Vent Ecosystems

Page 7: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

High-Pressure LifeHigh-Pressure Life

Discoveries of Life in Crustal Rocks – 1990s

Page 8: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

High-Pressure LifeHigh-Pressure Life

Discoveries of life in extreme environments – 1990s

Page 9: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

High-Pressure LifeHigh-Pressure Life

Methane ice worms -- 1999

Page 10: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

Life at High Pressureson other Worlds?

Life at High Pressureson other Worlds?

Deep, wet environments may exist on Mars, Europa, etc.

Page 11: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

Pressure Limits of Life Pressure Limits of Life

Isolation and Culture of High-Pressure Microbes – 1980s

Page 12: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

Pressure Limits of Life Pressure Limits of Life

Isolation and Culture of High-Pressure Microbes – 1990s

Page 13: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

Pressure Limits of Life Pressure Limits of Life

Isolation and Culture of Microbes at 1 GPa – 2001

Page 14: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

Pressure Limits of LifePressure Limits of Life

Microbes continueto reduce formateat pressures above 10,000 atmospheres

Page 15: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

Effects of Pressure on BiomoleculesEffects of Pressure on Biomolecules

Pressure induces phase transitions in membrane-forming lipid molecules.

Page 16: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

Effects of Pressure on BiomoleculesEffects of Pressure on BiomoleculesHigh-pressure cell membranes employModified lipids with unsaturated bonds.

Page 17: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

Effects of Pressure on WaterEffects of Pressure on Water

Pressure dramatically alters the thermalstability and physical properties of water.

Page 18: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

Hydrothermal Organic SynthesisThree techniques

Hydrothermal Organic SynthesisThree techniques

Gold tube reactors

Page 19: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

Hydrothermal Organic SynthesisThree techniques

Hydrothermal Organic SynthesisThree techniques

• Hydrothermal Diamond

Anvil Cell

Page 20: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

Hydrothermal Organic SynthesisThree techniques

Hydrothermal Organic SynthesisThree techniques

Flow-through Reactor

Page 21: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

Hydrothermal F-T SynthesisHydrothermal F-T Synthesis

• Reactants:

CO2 + H2 + H2O

• Catalyst:

Iron metal• Conditions:

300oC

500 atm

24 hours

Page 22: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

Pyruvic AcidPyruvic Acid

• Reactants:Pyruvic acid + CO2 + H2O

• Conditions:200

oC

2,000 atm2 hours

• Products:A diverse suite of organic molecules

Page 23: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

Hydrothermal Organic SynthesisResearch Strategy

Hydrothermal Organic SynthesisResearch Strategy

Page 24: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

The Formation of C-C Bonds Under High-P Hydrothermal Conditions

The Formation of C-C Bonds Under High-P Hydrothermal Conditions

Page 25: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

The Formation of C-C Bonds Under High-P Hydrothermal Conditions

The Formation of C-C Bonds Under High-P Hydrothermal Conditions

Page 26: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

The Formation of C-C Bonds Under High-P Hydrothermal Conditions

The Formation of C-C Bonds Under High-P Hydrothermal Conditions

Page 27: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

Thomas Gold’s Hypothesis:Organic Synthesis in the Mantle

Thomas Gold’s Hypothesis:Organic Synthesis in the Mantle

Thomas Gold (1999) NY:Springer-Verlag.

Page 28: Joint AIRAPT-18 & HPCC-11 Beijing, China -- 23-27 July 2001

ConclusionsConclusions

• Deep life is abundant and richly varied.

• Cellular life can exist at pressures exceeding 1 GPa.

• We have much to learn about the pressure adaptations of biomolecules.

• High pressure facilitates and enhances many hydrothermal organic reactions, because pressure increases the temperature stability of the aqueous phase.