Microbial Mythology: Difference between revisions

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== Myth : Microbes Don't have a fossil record. ==
== Myth : Microbes Don't have a fossil record. ==
Well, it is a myth. Admittedly the fossil records of micro-organisms are sparse, and often taxonomically ambiguous. But they're there. In fact, considering that micro-organisms were the first organisms to develop on the planet, it should be no surprise that the oldest fossil organisms are actually microbes. The current record-holder (though challenged) is a collection of 3.56 billion year old coccoidal and bacciloidal (? rod-shaped) scraps of organic material from the Pilbara district of the Australian outback (J.W.Schopf, "Microfossils of the Early Archean Apex Chert: new evidence of the antiquity of life." Science 260, 640-646 (1993)). More recent fossils (which are only challenged by the more retarded of creationists) known as [http://en.wikipedia.org/wiki/Stromatolite stromatolites] are also the products of microbes affecting the deposition of sediment clasts and the precipitation of chemical sediments. Coming to the (almost) recent past are the ciliophora (alleged) fossils mentioned in the discussion at [[Ciliophora]].
Well, it is a myth. Admittedly the fossil records of micro-organisms are sparse, and often taxonomically ambiguous. But they're there. In fact, considering that micro-organisms were the first organisms to develop on the planet, it should be no surprise that the oldest fossil organisms are actually microbes. The current record-holder (though challenged) is a collection of 3.56 billion year old coccoidal and bacciloidal (? rod-shaped) scraps of organic material from the Pilbara district of the Australian outback (J.W.Schopf, "Microfossils of the Early Archean Apex Chert: new evidence of the antiquity of life." Science 260, 640-646 (1993)). More recent fossils known as [http://en.wikipedia.org/wiki/Stromatolite stromatolites] are also the products of microbes affecting the deposition of sediment clasts and the precipitation of chemical sediments. Coming to the (almost) recent past are the ciliophora (alleged) fossils mentioned in the discussion at [[Ciliophora]].

Revision as of 01:06, 24 January 2008

Textbooks and web sites propagate various misconceptions and simple errors about microbiology. Here we provide a place for microbiology educators to set the record straight.
Authors: Please provide primary references, in open-access sources whenever possible.

TCA cycle: ATP or GTP?

Succinyl-CoA synthetase, also known as succinate thiokinase, is the enzyme of the TCA cycle that interconverts succinyl-CoA with succinate, coupled to formation of a nucleotide triphosphate. Many textbooks and web sites state that succinyl-CoA synthetase phosphorylates only GDP to GTP. See example.

According to the primary literature, however, ADP phosphorylation predominates in E. coli (Margaret Birney et al, 1996) whereas in Pseudomonas sp., various nucleotide diphosphates are phosphorylated (Vinayak Kapatral et al, 2000). Human mitochondria have two forms of the enzyme, which phosphorylate ATP and GTP respectively (David Lambeth et al, 2004).


How do conjugation pili mediate DNA transfer?

During bacterial conjugation, the donor and recipient cells are brought together by protein filaments called pili. Since the pili are composed of hollow tubes of protein subunits, like a turret, it was thought for a while that DNA might travel down the hollow tube. The hollow tube theory is still taught; see example.

Actually, DNA is transferred across the bacterial envelope by a protein complex embedded in the membranes. For review of classic experiments, see Brigette Dreiseikelmann, 1994. For a more current review, see Inês Chen et al, 2005.

Myth : Microbes Don't have a fossil record.

Well, it is a myth. Admittedly the fossil records of micro-organisms are sparse, and often taxonomically ambiguous. But they're there. In fact, considering that micro-organisms were the first organisms to develop on the planet, it should be no surprise that the oldest fossil organisms are actually microbes. The current record-holder (though challenged) is a collection of 3.56 billion year old coccoidal and bacciloidal (? rod-shaped) scraps of organic material from the Pilbara district of the Australian outback (J.W.Schopf, "Microfossils of the Early Archean Apex Chert: new evidence of the antiquity of life." Science 260, 640-646 (1993)). More recent fossils known as stromatolites are also the products of microbes affecting the deposition of sediment clasts and the precipitation of chemical sediments. Coming to the (almost) recent past are the ciliophora (alleged) fossils mentioned in the discussion at Ciliophora.