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Marine and Metabolic diversity

have two fundamental nutritional needs: • 1. Obtaining in a form that can be used to synthesize fatty , , DNA, and RNA

get their carbon from CO2

get carbon from organic sources vs

2 Metabolic diversity

• Organisms have two fundamental nutritional needs: • 2. Acquiring chemical in the form of ATP

: energy from light

(or ): energy from inorganic chemicals such as H2S, NH3, CH4

: energy from organic sources, such as sugars

3 Metabolic diversity

Category Energy source Carbon source or Examples source

Photolithoautotrophy Light CO2 Inorganic , bacteria Photoorganoautotrophy Light Organic compounds Organic compounds Purple non-sulfur

or H2 bacteria, aerobic, anoxygenic bacteria, archaea (?)

Chemolithoautotrphy Inorganic CO2 Inorganic Sulfur-oxidizing bacteria, , archaea Chemoorganoautotrophy Organic Organic compounds Organic compounds Wide range of compounds bacteria and archaea Mixotrophy (combination Organic Organic compounds Inorganic Sulfur-oxidizing of lithoautotrophy and compounds bacteria organoheterotrophy) of

Prebiotic Precellular Early LUCA Evolutionary chemistry life cellular life diversification 4.3-3.8 bya 3.8-3.7 bya

Biological RNA DNA Divergence of building blocks world synthesis bilayers Bacteria and Archaea Amino acids Catalytic RNA RNA – Replication Cellular Components of DNA Nucleosides Self-replicating RNA templated compartments replication, Sugars Early cells likely transcription, and had high rates translation all in of HGT place Submarine mounds and their possible link to the origin of life.

Model of the interior of a hydrothermal mound with hypothesized transitions from prebiotic chemistry to cellular life depicted

Differences between Archaea, Bacteria and

Characteristic Bacteria Archaea Eukaryotes type Prokaryotic Prokaryotic Eukaryotic No histones Have proteins Have histones similar to histones No introns Some introns Most contain introns size 70S 70S ribosomes 80S ribosomes Made of protein Not always present composition (lack peptidoglycan) : plasma membrane Fungi: linked Ester linked lipids Ester linked lipids composition with D- with L-Glycerol with proteinf (straight chain) (branch chain) (straight chain)

Themes: Growth & by

A. Bacterium before B. DNA replication starts. C. The new copy of DNA DNA replication. It proceeds in two is attached at a Bacterial is directions membrane site near the attached to the plasma parent DNA molecule. membrane.

E. Deposits of new F. The ongoing deposition D. New membrane grows membrane and new wall of membrane and wall between the two material extend down material divides the cell in attachment sites. into the . two. Themes: conjugation

nicked conjugation tube

A. A conjugation tube forms between a B. DNA replication starts on the nicked donor and a recipient cell. An has plasmid. The displaced DNA strand moves nicked the donor’s plasmid. through the tube and enters the recipient cell.

C. In the recipient cell, replication starts on D. The cells separate from each other; the the transferred DNA. circularize. Themes: Morphological diversity

• Many have flagella for swimming and pili for clinging to surfaces

Pili

• Typical Shapes:

Cocci Spirochetes Marine bacteria Planktonic Bacteria and Archaea

• Relatively few major Bold = ubiquitous in , others are specialized

Roseobacter • 25% marine bacteria • • Microbial mats • ice • Association with • Important in carbon and sulfur cycles Marine bacterial phenotypes

• Anoxygenic • Eg Purple phototrophs • Do not evolve during as • Many in shallow marine sediments

CO2 + H2S + H2O = (CH2O) + S + H2O

Rhodospirillum Marine bacterial phenotypes

• Oxygenic Photosynthesis • Cyanobacteria • – evolution of oxygen • and accessory photosynthetic pigments • “Blue green ” but many “red orange” • Very diverse , including extreme temperatures and hypersaline environments • Plankton, sea ice, shallow sediments, microbial mats • Many carry out • Only recently grouped together (16S )

Synechococcus Account for between 15-40% of carbon input to webs Marine bacterial phenotypes

• Nitrifying bacteria • Major role in nitrogen cycling, especially shallow coastal sediments, and beneath areas • and oxidize ammonia to • Chemolithoautotrophs • Nitrosobacter, , and Nitrococcus oxidize to nitrate • Usually chemolithoautotrophs also • Chemolithotrophs

Thiomargarita namibiensis Multicellular filamentous Aerobe in top few mm of Largest known bacteria, bacteria marine sediments filaments with common Uses reduced sulfur Upwelling sheath compounds Anoxic reduction of H2S and reduction nitrogen Upwelling Auto- or mixo-trphic Oxidizes sulfite using nitrate Marine Archaea Archaea

• Anaerobic process carried out only by (major ) • Large amount of methane is produced in marine sediments, but disappears before oxygen zone, where methane would be reduced • -reducing bacteria oxidize methane using sulfur

Desulfococcus Archaea • Extreme

Pyrococcus Anaerobic chemoorganotroph Optimal growth at 100oC Anaerobic chemoorganotroph, optimum growth at 800C Archaea

• Grow in concentrations greater than 9% NaCl

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