| Literature DB >> 30995811 |
Martin Koller1,2.
Abstract
Haloarchaea, the extremely halophilic branch of the Archaea domain, encompass a steadily increasing number of genera and associated species which accumulate polyhydroxyalkanoate biopolyesters in their cytoplasm. Such ancient organisms, which thrive in highly challenging, often hostile habitats characterized by salinities between 100 and 300 g/L NaCl, have the potential to outperform established polyhydroxyalkanoate production strains. As detailed in the review, this optimization presents due to multifarious reasons, including: cultivation setups at extreme salinities can be performed at minimized sterility precautions by excluding the growth of microbial contaminants; the high inner-osmotic pressure in haloarchaea cells facilitates the recovery of intracellular biopolyester granules by cell disintegration in hypo-osmotic media; many haloarchaea utilize carbon-rich waste streams as main substrates for growth and polyhydroxyalkanoate biosynthesis, which allows coupling polyhydroxyalkanoate production with bio-economic waste management; finally, in many cases, haloarchaea are reported to produce copolyesters from structurally unrelated inexpensive substrates, and polyhydroxyalkanoate biosynthesis often occurs in parallel to the production of additional marketable bio-products like pigments or polysaccharides. This review summarizes the current knowledge about polyhydroxyalkanoate production by diverse haloarchaea; this covers the detection of new haloarchaea producing polyhydroxyalkanoates, understanding the genetic and enzymatic particularities of such organisms, kinetic aspects, material characterization, upscaling and techno-economic and life cycle assessment.Entities:
Keywords: Archaea; Haloferax; bioeconomy; biopolyester; downstream processing; extremophiles; haloarchaea; halophiles; polyhydroxyalkanoates; salinity
Year: 2019 PMID: 30995811 PMCID: PMC6631277 DOI: 10.3390/bioengineering6020034
Source DB: PubMed Journal: Bioengineering (Basel) ISSN: 2306-5354
Figure 1Extract from the phylogenetic tree of haloarchaea, selecting those species reported to accumulate PHA biopolyesters. Colored (orange) background highlights the limited number of species to date cultivated on bioreactor scale to study PHA production. The asterisks indicate 3-hydroxyvalerate production by the strain from structurally unrelated substrates. (Bold: orders; red: families; italics and underlined: genera; italics: species).
Figure 2Simplified illustration of PHB and PHBHV biosynthesis by eubacteria (upper part, in grey; prototype organism: C. necator) and haloarchaea (lower part, in pink; prototype: Hfx. mediterranei). Enzymes and genes (in italics) involved in the PHA biosynthesis steps (starting from acetyl-CoA and propionyl-CoA) are in green text boxes. Special emphasis is dedicated to the propionyl-CoA supplying pathways in haloarchaea: Propionyl-CoA is generated (a) beginning with the coupling of pyruvate and acetyl-CoA, and the decarboxylation of 2-oxobutyrate (marked in brown), (b) starting from the conversion of the amino acids methionine or threonine to 2-oxobutyrate (marked in yellow), (c) starting from succinyl-CoA via methlymalonyl-CoA (marked in green), or (d) starting with carboxylation of acetyl-CoA to malonyl-CoA (marked in purple). Based on [26].
Figure 3(a) Pinkish, mucous Hfx. mediterranei colonies grown on solid medium. (b) Macroscopic appearance of samples taken from a Hfx. mediterranei bioreactor cultivation from the beginning (t = 0 h) until the end (t = 74 h) of the process. Own pictures of the author M. Koller.
PHA production by haloarchaea on shaking flask and stirred flask scale—collected data from literature.
| Species | Strain Isolation | Salinity in Medium, Substrates, T | Product | Production Scale/Productivity | Ref. |
|---|---|---|---|---|---|
|
| Salt pond at the coast near Alicante, Spain | 150 g/L NaCl | PHBHV | 2.5 L aerated and stirred flasks 0.62 (g/L·h), qPmax. = 0.037 1/h (35 °C) | [ |
|
| ´´ | 200 g/L NaCl; T = 37 °C | PHBHV | Shaking flask scale; | [ |
|
| ´´ | 200 g/L NaCl; T = 37 °C | PHBHV | Shaking flask scale; 16.4 g/L PHA, 70 wt.% PHA in CDM, 0.17 g/(L·h) | [ |
|
| ´´ | 190 g/L total salts; 144 g/L NaCl; Alkaline hydrolyzed | PHBHV | Shaking flask scale; batch cultivation; | [ |
|
| ´´ | 220 g/L NaCl | PHBHV | Shaking flask scale, batch cultivation; | [ |
|
| ´´ | 156 g/L NaCl; | PHBHV | Shaking flask scale, batch cultivation; | [ |
|
| ´´ | 156 g/L NaCl; T = 37 °C | PHBHV | 500 mL shaking flasks, batch 0.95 g/L PHA, 15.6 % PHA in CDM; 0.007 g/(L·h) with optimum phosphate concentration 0.5 g/L KH2PO4 | [ |
|
| ´´ | 156 g/L NaCl; | PHBHV | Shaking flask scale; batch and fed-batch 0.4–1.5 g/L PHA, 10.3–27.1 wt.% PHA in CDM, 0.003–0.010 g/(L·h) (fed-batch, dependent on C-source) | [ |
|
| Dead Sea | 200 g/L NaCl; T = 37 °C | ? | Shaking flask scale; | [ |
|
| ´´ | 250 g/L NaCl; T = 37 °C | “PHB” | Shaking flask scale; | [ |
| Solar salterns of Ribandar in Goa, India | 200 g/L NaCl; T = 37 °C | ? | Shaking flask scale; | [ | |
|
| Salt pond at the coast near Alicante, Spain | “PHB” | Shaking flask scale; | [ | |
|
| Dead Sea | 200 g/L NaCl; | PHB | Shaking flak scale; | [ |
|
| Salt pond at the coast near Alicante, Spain | 250 g/L NaCl; T = 37 °C | “PHB” | Shaking flask scale; | [ |
|
| ´´ | 200 g/L NaCl; T = 37 °C | PHBHV | 0.09 wt.% PHA in CDM | [ |
|
| Hypersaline Urmia lake, Iran | 250 g/L NaCl | PHB | Shaking flask scale; | [ |
|
| ´´ | 250 g/L NaCl | PHB | Shaking flask scale; | [ |
| 250 g/L NaCl | PHB | Shaking flask scale; Max. 46.6 wt.% PHB in CDM (2% petrochemical wastewater, yeast extract, 47 °C | [ | ||
|
| ´´ | 250 g/L NaCl | PHB | Shaking flask scale; | [ |
| Solar salterns of Ribandar in Goa, India | 200 g/L NaCl; T = 37 °C | ? | Shaking flask scale; | [ | |
| Solar salterns of Marakkanam in Tamil Nadu, India | 200 g/L NaCl; T = 37 °C | PHB | Shaking flask scale; | [ | |
| Solar salterns of Marakkanam in Tamil Nadu, India | 200 g/L NaCl; T = 37 °C | PHBHV | Shaking flask scale; | [ | |
|
| ´´ | 200 g/L NaCl; T = 37 °C | PHBHV | Shaking flak scale; | [ |
|
| ´´ | 200 g/L NaCl; T = 37 °C | PHBHV | Shaking flask cultivations in batch mode; Starch: 4.6 g/L PHA, 0.02 g/(L·h), 74.2% PHA in CDM, Cassava bagasse: 1.52 g/L, 0.006 g/(L·h), 44.7% PHA in CDM | [ |
|
| Bore core of an Austrian Permian salt deposit | 200 g/L NaCl; T = 37 °C | PHBHV | Shaking flask scale; | [ |
|
| Dry rock salt from Austrian alpine salt mine | Complex saline medium; | PHBHV | Shaking flask scale; | [ |
|
| Stromatolites from the Hamelin pool in the Australian Shark Bay | Complex saline medium; | PHBHV | Shaking flask scale; | [ |
|
| Dead Sea | Complex saline medium; | PHBHV | Shaking flask scale; | [ |
|
| Crude sea-salt sample collected near Qingdao, PR China | Complex saline medium; | PHBHV | Shaking flask scale; | [ |
|
| Salt; Cadiz, Spain | Complex saline medium; | PHB | Shaking flask scale; | [ |
|
| Austrian alpine rock salt | Complex saline medium; | PHBHV | Shaking flask scale; | [ |
| Solar salterns of Ribandar in Goa, India | 200 g/L NaCl; T = 37 °C | n.d. | Shaking flask scale; | [ | |
|
| Sea salt in Baja California, Mexico, Western Australia and Greece | 200 g/L NaCl; T = 37 °C | PHBHV | Shaking flask scale; | [ |
|
| Dead Sea | 200 g/L NaCl; T = 37 °C | PHBHV | Shaking flask scale; | [ |
| Samples collected from surface of hypersaline soil collected in Aswan, Egypt | 220 g/L NaCl; T = 42 °C (other T tested) | PHB | Shaking flask scale; | [ | |
|
| Indian salt production pans | 200 g/L NaCl (other salinities tested); T = 37 °C | PHBHV | Repeated batch cultivations in shaking flaks | [ |
| Kayacik saltern, Turkey | 250 g/L NaCl; | PHBHV | Shaking flak cultivations; | [ | |
|
| Soda slat lake liquors from the East African Magadi soda lake | 200 g/L NaCl; T = 37 °C alkaliphile; | PHB | Shaking flask scale; | [ |
|
| Magadi Lake, Kenia | 200 g/L NaCl; T = 37 °C alkaliphile; | PHBHV | Shaking flask scale; | [ |
|
| Sediments of the Great Salt Lake in Utah | 270 g/L NaCl (maximum described salinity optimum for living beings!); T = 50 °C | Not specified | Shaking flask scale; | [ |
|
| Hypersaline, anoxic deep-sea brine-sediment interface of the Red Sea | 270 g/L NaCl (maximum described salinity optimum for living beings!); T = 45 °C | Not specified | Shaking flask scale; | [ |
|
| Borehole at Polish salt mine | 200 g/L NaCl; T = 40 °C | Not specified | Shaking flask scale; | [ |
|
| Sinai peninsula and saltern crystallizers in Australia and Spain | 140–360 g/L NaCl for growth (optimum: >180 g/L); T = 25–45 °C | PHB | Shaking flaks scale; | [ |
PHA production by haloarchaea on bioreactor scale—collected data from literature.
| Species | Strain Isolation | Salinity in Medium, Substrates, T | Product | Production Scale/Productivity | Ref. |
|---|---|---|---|---|---|
|
| Salt pond at the coast near Alicante, Spain | 250 g/L marine salts | PHBHV (in publication: “PHB”) | Stable (monoseptic) continuous cultivation over 3 months in 1.5 L bioreactor; | [ |
|
| ´´ | 150 g/L NaCl; T = 37 °C | PHBHV | 10 L bioreactor; fed-batch feeding; | [ |
|
| ´´ | 200 g/L NaCl; T = 37 °C | PHBHV | 42 L bioreactor fed-batch process; 0.09 g/(L·h), 12.2 g/L PHBHV | [ |
|
| ´´ | 150 g/L NaCl; T = 37 °C | PHBHV | 200 L fed-batch | [ |
|
| ´´ | 200 g/L NaCl; T = 37 °C | PHBHV | 10 L bioreactor batch process | [ |
|
| ´´ | 156 g/L NaCl; T = 37 °C | PHBHV | 2 L bioreactor batch process | [ |
|
| ´´ | 150 g/L NaCl; T = 37 °C | PHBHV | 42 L/10 L bioreactor fed-batch process; | [ |
|
| ´´ | 200–230 g/L NaCl; T = 37 °C | PHBHV | 6 L bioreactor pH-stat fed-batch process; | [ |
|
| ´´ | 234 g/L NaCl; T = 37 °C | PHBHV | 5 L bioreactor; pH-stat feeding strategy; | [ |
| ´´ | 200 g/L NaCl; | PHBHV | Unsterile 50 L plug-flow PMMA bioreactor; | [ | |
|
| ´´ | 156 g/L NaCl; | PHBHV | Fed-batch bioreactor cultivation | [ |
| ´´ | 140 g/L total salts (110 g/L NaCl) | 7 L fed-batch bioreactor cultivation | [ | ||
|
| Tainan marine solar saltern near Lianyungang, PR China | 200 g/L NaCl; T = 37 °C | PHBHV | 7.5 L bioreactor; fed-batch feeding strategy; | [ |
| Samples collected from surface of hypersaline soil collected in Aswan, Egypt | 250 g/L NaCl; T = 40 °C | PHB | Corrosion-resistant 8 L composite bioreactor; batch feeding; | [ | |
|
| Saltern crystallizer pond at Fuente de Piedra saline lake, Malaga, Spain | 200 g/L NaCl; T = 37 °C | PHB | Bioreactor; batch setups and bioreactor equipped with ultrafiltration unit | [ |