| Literature DB >> 27489146 |
Víctor de Lorenzo1, Philippe Marlière2, Ricard Solé3,4.
Abstract
Planet Earth's biosphere has evolved over billions of years as a balanced bio-geological system ultimately sustained by sunpower and the large-scale cycling of elements largely run by the global environmental microbiome. Humans have been part of this picture for much of their existence. But the industrial revolution started in the XIX century and the subsequent advances in medicine, chemistry, agriculture and communications have impacted such balances to an unprecedented degree - and the problem has nothing but exacerbated in the last 20 years. Human overpopulation, industrial growth along with unsustainable use of natural resources have driven many sites and perhaps the planetary ecosystem as a whole, beyond recovery by spontaneous natural means, even if the immediate causes could be stopped. The most conspicuous indications of such a state of affairs include the massive change in land use, the accelerated increase in the levels of greenhouse gases, the frequent natural disasters associated to climate change and the growing non-recyclable waste (e.g. plastics and recalcitrant chemicals) that we release to the Environment. While the whole planet is afflicted at a global scale by chemical pollution and anthropogenic emissions, the ongoing development of systems and synthetic biology, metagenomics, modern chemistry and some key concepts from ecological theory allow us to tackle this phenomenal challenge and propose large-scale interventions aimed at reversing and even improving the situation. This involves (i) identification of key reactions or processes that need to be re-established (or altogether created) for ecosystem reinstallation, (ii) implementation of such reactions in natural or designer hosts able to self-replicate and deliver the corresponding activities when/where needed in a fashion guided by sound ecological modelling, (iii) dispersal of niche-creating agents at a global scale and (iv) containment, monitoring and risk assessment of the whole process.Entities:
Mesh:
Substances:
Year: 2016 PMID: 27489146 PMCID: PMC4993180 DOI: 10.1111/1751-7915.12399
Source DB: PubMed Journal: Microb Biotechnol ISSN: 1751-7915 Impact factor: 5.813
Figure 1At least four scales need to be addressed for knocking‐in a new functionality within a pre‐existing ecological web: (A) the ecosystem level, characterized by interactions among species (S, H), external inputs/resources (R) in a biogeochemical context e.g. CO2, N2 and P availability. (B) the pair‐wise species interplay level, which may encompass transactions between actors of different kingdoms (microbial, plants, animals), specially mutualistic interactions, the components of which can be affected positively and negatively by external signals (M), water (W) being paramount in the whole setup. (C) the genetic, epigenetic and biochemical circuit level that rules the behaviour of single‐species following a logic network (the logicome) and (D) the specific DNA sequence necessary to make the biological or chemical activity of interest happen (Solé, 2015).
Major reactions undergone by life‐supporting chemical elements that affect the global balance of the Earth's cycles
| Chem species | Status | Issues | Remediation agenda |
|---|---|---|---|
| C | C acts at the surface of the Earth in two major roles. As the atomic component with most versatile connecting capability, it enables the construction and propagation of biomatter through genetically programmed formation of C‐C, C‐O, C‐H, C‐N and C‐S bonds. As a volatile element it cycles in the atmosphere, hydrosphere and Earth crust under redox forms ranging from fully reduced (CH4 and coal) to fully oxidized (CO2), entailing major planetary consequences because of their greenhouse and ocean acidification effects |
Energy vehicle |
Diversify carbon chemical reaction mechanisms by implanting in metabolism NTN Construct alternatives for CO2, CO, CH4 fixation so as to curb the release of greenhouse gas generation in the chemical industry and immobilize atmospheric carbon in biomaterial sinks |
| N | N is a universal component of biomatter (ca 15% cell dry mass) as constituent of nucleic acids and proteins. Humans require on average one mole of daily N nutritional intake. Nitrogen is used under its reduced form (ammonia) by living organisms but can be assimilated under oxidized form (nitrate, nitrite) or even N2 by nitrogen fixing bacteria. Vegetal growth in agriculture is mainly limited by nitrogen availability. The invention of |
Fixation |
Deploy alternative bioprocesses of nitrogen fixation from N2 tolerant to O2 in bacteria and eucaryotes (plants and fungi) through NTN biocatalysts so as to use air as feedstock Program efficient syntrophic microbe/plant associations |
| P | P is a universal component of biomatter (ca 1% cell dry mass) as part of nucleic acid backbone as well as animal skeleton. Humans require on average 10 mmoles of daily nutritional P intake. It exists under its oxidized form, phosphate, in the Earth crust. As such it is not volatile, does not recycle through the atmosphere and sinks in the hydrosphere to accumulate at ca 3 μM in the oceans. A phosphorus dearth is anticipated to occur in the not so distant future, once natural deposits of phosphate in Morocco, Russia and a few rare other locations will have been exhausted for fertilizing fields at the global level |
Non‐renewable |
Deploy alternatives to the use of phosphorus in industrial molecular products and production processes so as to spare natural resources and prevent eutrophication Deploy sustainable processes to extract P from seawater, marine sediments and wastewater using renewable energy so as to fulfil losses through seepage from continental lands |
| H2O | The elements hydrogen and oxygen mainly intervene at the surface of the Earth as water, which itself serves as reagent in a myriad of metabolic reactions for constructing biomatter. Freshwater is a rare and precious resource. |
Life support |
Exploring novel polymeric materials with highest resolution/specification of active structure and lowest cost of bioproduction, operation and environmental impact
Enhanced processing with novel ion exchange resins for desalting, adsorbing and sequestering elemental pollutants ( e.g. precious elements and heavy metals) |
NTN, new to nature.
Figure 2Biological metabolism versus industrial metabolism. The upper part of the figure sketches the basic metabolic cycle of the biosphere: a sustainable sequence of biochemical reactions for building (anabolism) and dismantling (catabolism) biomass and other bio‐compounds on the basis of available C, N and P species (and to a lesser extent others like Fe etc.) obtainable in the biosphere. The lower part outlines in a super‐simplified form the action of the so‐called Industrial metabolism (Ayres, 1994). This involves the integrated collection of human‐made physical and chemical processes that transform raw materials and (generally non‐renewable) energy into products, leaving wastes, e.g. CO2 and recalcitrant products and materials) along the way. The interplay between biological cycles and industrial processes at global scale was a popular topic in the late 1970s (de Rosnay, 1979). Alas, the current state of affairs makes such an industrial metabolism – and it is associated industrial ecology (Allenby, 2006) ultimately unsustainable. The notion of transmetabolism discussed in this article attempts to overcome the breach between the natural and the human‐made chemical domains by bridging the two with new reactions and rationally delivering them at a global scale by means of deeply engineered biological agents.