TY - CHAP
T1 - Bioenergetics theory and components
T2 - Periplasmic electron-transport systems in bacteria
AU - Richardson, D. J.
AU - Sawers, G.
AU - Van Spanning, R. J. M.
N1 - This is a reproduction of A.B. Hooper, A.A. DiSpirito, Chemolithotrophy, in Encyclopedia of Biological Chemistry (Second Edition), Edited by: William J. Lennarz, M. Daniel Lane, Elsevier Inc., 2013, https://doi.org/10.1016/B978-0-12-378630-2.00219-X.
PY - 2021/8/2
Y1 - 2021/8/2
N2 - The periplasmic compartment lies between the inner (cytoplasmic) and outer membranes of Gram-negative bacteria. It is frequently termed the ‘periplasmic space’, but this is a misnomer as the term ‘space’ suggests a void and the periplasmic compartment is far from that. In fact, it is a highly metabolically active compartment where many important respiratory electron-transfer proteins are located. In bacteria these periplasmic redox proteins result in a great respiratory diversity, as they can facilitate electron transfer between a range of electron donors (e.g., formate, hydrogen, reduced nitrogen species, and reduced sulfur species) and electron acceptors (e.g., nitrogen and sulfur oxyanions, dimethylsulfoxide, and trimethylamine N oxide). This underlies the success of bacteria in colonizing a wide range of the Earth׳s oxic and anoxic environments and the important contribution of bacteria to critical biogeochemical element cycles, such as the nitrogen, sulfur, and carbon cycles.
AB - The periplasmic compartment lies between the inner (cytoplasmic) and outer membranes of Gram-negative bacteria. It is frequently termed the ‘periplasmic space’, but this is a misnomer as the term ‘space’ suggests a void and the periplasmic compartment is far from that. In fact, it is a highly metabolically active compartment where many important respiratory electron-transfer proteins are located. In bacteria these periplasmic redox proteins result in a great respiratory diversity, as they can facilitate electron transfer between a range of electron donors (e.g., formate, hydrogen, reduced nitrogen species, and reduced sulfur species) and electron acceptors (e.g., nitrogen and sulfur oxyanions, dimethylsulfoxide, and trimethylamine N oxide). This underlies the success of bacteria in colonizing a wide range of the Earth׳s oxic and anoxic environments and the important contribution of bacteria to critical biogeochemical element cycles, such as the nitrogen, sulfur, and carbon cycles.
UR - http://www.scopus.com/inward/record.url?scp=85118518821&partnerID=8YFLogxK
U2 - 10.1016/B978-0-12-819460-7.00601-0
DO - 10.1016/B978-0-12-819460-7.00601-0
M3 - Entry for encyclopedia/dictionary
AN - SCOPUS:85118518821
SN - 9780128194607
VL - 2
SP - 31
EP - 37
BT - Encyclopedia of Biological Chemistry
PB - Elsevier
ER -