sigam o carbono -1

39
Sigam o Carbono -1

Upload: jada-valencia

Post on 03-Jan-2016

21 views

Category:

Documents


1 download

DESCRIPTION

Sigam o Carbono -1. FOLLOW THE LIFE. Solvent Biogenic elements Source of Free Energy. . - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: Sigam o Carbono -1

Sigam o Carbono -1

Page 2: Sigam o Carbono -1

FOLLOW THE LIFE

• Solvent • Biogenic elements• Source of Free Energy

searches for life within our solar system commonly retreat from a search for life to a search for “life as we know it,” meaning life based on liquid water, a suite of so-called “biogenic” elements (most famously carbon), and a usable source of free energy.

(Chyba & Hand, 2005, p. 34)

Page 3: Sigam o Carbono -1

FOLLOW THE LIFE

• Follow the water• Follow the carbon• Follow the nitrogen• Follow the energy• Follow the entropy• Follow the information

Page 4: Sigam o Carbono -1

Universo Orgânico!

• 0.5 % da matéria bariônica “visível” está na forma molecular. (Fraser, McCoustra & Willians, 2002, A&G, 43, 2.11).

• ~170 Moléculas detectadas no espaço ~170 Moléculas detectadas no espaço (~50% orgânicas: CHON).(~50% orgânicas: CHON).

Page 5: Sigam o Carbono -1

Como as biomoléculas são encontradas?

Radiotelescopes Radiotelescopes (rotational (rotational lines)lines)

IR-Telescopes IR-Telescopes (vibrational lines)(vibrational lines)

Itapetinga, SPItapetinga, SP

VLAVLA

Page 6: Sigam o Carbono -1

Hale-BoppHale-Bopp MurchinsonMurchinson

Gaseous Pillars – Eagle NebulaGaseous Pillars – Eagle Nebula Key hole NebulaKey hole Nebula

TitanTitan

Onde são encontradas as biomoléculas?

Page 7: Sigam o Carbono -1

Interstellar and circumstellar molecules

H2

CO

C6H6

NH3

Page 9: Sigam o Carbono -1

Element Parts per million

Hydrogen 739,000

Helium 240,000

Oxygen 10,700

Carbon 4,600

Neon 1,340

Iron 1,090

Nitrogen 950

Silicon 650

Magnesium 580

Sulfur 440

All Others 650

Carbon in the Universe

Page 10: Sigam o Carbono -1
Page 11: Sigam o Carbono -1

Why Carbon?

• Carbon atom can form up to 4 chemical bonds with many other atoms – can form long and complex molecules

• Carbon can form compounds that readily dissolve in water.

Page 12: Sigam o Carbono -1

Typically only electrons from the outer shell (valence electrons) engage in chemical bonds

Hydrogen

Helium

Carbon

Outer shell/orbits

There is “optimal” number of electrons per shell. S-shell = 2 electronsP-shell = 8 electrons

P-shell S-shell

Page 13: Sigam o Carbono -1

Chemical bonds

• Covalent

• Ionic

• Hydrogen

Page 14: Sigam o Carbono -1

Carbon has 4 valence electrons – can form

up to 4 bonds

Methane Ethane

Page 15: Sigam o Carbono -1

ethanol

diamond

ethene

benzene

fullerene

Page 16: Sigam o Carbono -1

Polymerization

• A polymer is a substance composed of molecules with large molecular mass composed of repeating structural units, or monomers, connected by covalent chemical bonds. Well known examples of polymers include plastics and DNA.

Page 17: Sigam o Carbono -1

Silicon life?• Si is abundant and also can form four bonds at

once (like C). But!

• Si bonds are much weaker – complex molecules based on Si will be fragile

• Si does not form double bonds – less variety

Page 18: Sigam o Carbono -1

Organic and Inorganic Carbon

C can be in reduced or oxidized forms.

Organic carbon Inorganic carbon (reduced) (oxidized)

‘CH2O’ CO2 carbon dioxideH2CO3 carbonic acid

Example: HCO3 bicarbonate ion

Glucose -- C6H12O6 CO32 carbonate ion

Page 19: Sigam o Carbono -1

Organic carbon(has C-H and C-C bonds)

Inorganic carbon(C-O bonds only)

Page 20: Sigam o Carbono -1

http://www.nationalfuelgas.com

                                              

http://www.upl.cs.wisc.edu/~stroker/jungle.jpg

JENNY HAGER/ THE IMAGE WORKS

Organiccarbon

Coal

Oil

Page 21: Sigam o Carbono -1

http://www.summerclouds.com/Vero/Sea%20Shells.jpg http://educate.si.edu/lessons/currkits/ocean/

http://www.cmas-md.org/Images/Sanjay/UnivTop4.jpg

Inorganiccarbon

Seashells

Coral

Page 22: Sigam o Carbono -1

Four types of organic macromolecules

in living systems. Most of the molecules in the living systems are

water (H2O) and large organic macromolecules:

• Carbohydrates

• Lipids

• Proteins

• Nucleic Acids

Page 23: Sigam o Carbono -1

Carbohydrates (sugars, starches)

• Representatives:Glucose, Fructose• Many hydroxyl groups (-OH)• Soluble in water• Form Polysaccharides• Good energy source• Structural support for organisms (cellulose- the main constituent of wood)

Page 24: Sigam o Carbono -1

Glucose

FructoseTable sugar

Page 25: Sigam o Carbono -1

Glucose polymerization

In starch molecule (potato) there can be 100s thousands of glucose units

H2O

Linked by dehydration reactionPolysaccharides

Page 26: Sigam o Carbono -1

Lipids (fats and oils)

• Representatives: fatty acids and cholesterol

• Poorly soluble in water

• Good (concentrated)

energy source

• Flexible

(cell membrane material)

Page 27: Sigam o Carbono -1
Page 28: Sigam o Carbono -1

Proteins

• “Proteios” – primary• Long “trains” of amino acids• Different proteins have different sequence of

amino acids • 20 amino acids used in any organism • Some provide structure (fingernails, hair) • Some serve as catalysts • Enzymes – proteins with catalitic properties

Page 29: Sigam o Carbono -1

L-Alanine Glycine

Linked by dehydration reaction

Page 30: Sigam o Carbono -1

Catalysts in Chemistry

• Suppose chemical reaction:

A + B AB is a slow reaction • The same reaction can be accelerated with catalyst

(D):

A + D AD fast step

B + AD AB + D fast step

The net result is still:

A + B AB but it is much faster

Page 31: Sigam o Carbono -1

Proteins (continued)

• Even though there are ~70 amino acids any known life uses only 20

• Amino acids derived abiotically are a mix of both “left-handed” and “right-handed” ones. Biological amino acids are only left-handed.

Chirality• Was there a common ancestor for all life?

Page 32: Sigam o Carbono -1

Biology uses only left-handed Alanine

Page 33: Sigam o Carbono -1

Large carbonaceous molecules in space

Ehrenfreund & Charnley 2000

PAHs ~ 15 %

Diamond << Graphite ?Fullerenes ~ 0.5 %

C-chains ~ 0.1%

Nanotubes

C-onions> 50% ??Soot

Page 34: Sigam o Carbono -1

Qual a Origem do Carbono?

Page 35: Sigam o Carbono -1

Credit: Y.Pendleton

Page 36: Sigam o Carbono -1
Page 37: Sigam o Carbono -1

Meteorites• A meteorite is a natural object originating in

outer space that survives an impact with the Earth's surface without being destroyed.

• Chondrites – 86%

(5% Carbonaceous Chondrites)

• Achondrites – 8%

• Iron meteorites – 5%

Page 38: Sigam o Carbono -1

Meteorites represent extraterrestrial material which can be studied on Earth !

Volatile fraction:

Insoluble C-fraction:60-80 % aromatic carbonhighly substituted smallaromatic moieties branchedby aliphatic chains

Murchison (1969, Australia)

Page 39: Sigam o Carbono -1

Abundances of soluble organic compounds in the Murchison meteorite (Botta & Bada 2002, Sephton 2002, 2004) Compound Class Concentration(ppm)

Amino Acids CM 17-60CI ~5

Aliphatic hydrocarbons >35Aromatic hydrocarbons 3.3Fullerenes > 1Carboxylic acids > 300Hydroxycarboxylic acids 15Dicarboxylic acids & Hydroxydicarboxylic acids 14Purines & Pyrimidines 1.3Basic N-heterocycles 7Amines 8Amides linear > 70

cyclic > 2Alcohols 11Aldehydes & Ketones 27Sulphonic acids 68Phosphonic acids 2