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Choudhury, P.K.;  Jena, R.;  Tomar, S.K.;  Puniya, A.K. Hydrogen is a Key Player in Rumen Fermentation. Encyclopedia. Available online: https://encyclopedia.pub/entry/38664 (accessed on 13 December 2024).
Choudhury PK,  Jena R,  Tomar SK,  Puniya AK. Hydrogen is a Key Player in Rumen Fermentation. Encyclopedia. Available at: https://encyclopedia.pub/entry/38664. Accessed December 13, 2024.
Choudhury, Prasanta Kumar, Rajashree Jena, Sudhir Kumar Tomar, Anil Kumar Puniya. "Hydrogen is a Key Player in Rumen Fermentation" Encyclopedia, https://encyclopedia.pub/entry/38664 (accessed December 13, 2024).
Choudhury, P.K.,  Jena, R.,  Tomar, S.K., & Puniya, A.K. (2022, December 13). Hydrogen is a Key Player in Rumen Fermentation. In Encyclopedia. https://encyclopedia.pub/entry/38664
Choudhury, Prasanta Kumar, et al. "Hydrogen is a Key Player in Rumen Fermentation." Encyclopedia. Web. 13 December, 2022.
Hydrogen is a Key Player in Rumen Fermentation
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This entry is adapted from the peer-reviewed paper 10.3390/methane1040024

Climate change and the urgent need to reduce greenhouse gas (GHG) emission from agriculture has resulted in significant pressure on the livestock industry for advanced practices that are environmentally more sustainable. Livestock is responsible for more than 15% of anthropogenic methane (CH4) emission via enteric fermentation and improved strategies for mitigating enteric CH4 production therefore represents a promising target to reduce the overall GHG contribution from agriculture. Ruminal CH4 is produced by methanogenic archaea, combining carbon dioxide (CO2) and hydrogen (H2). Removal of H2 is essential, as its accumulation inhibits many biological functions that are essential for maintaining a healthy rumen ecosystem. 

hydrogenotrophy methanogenesis propionogenesis reductive acetogenesis

1. Introduction

The rumen harbors a highly diverse and complex mixture of microorganisms, including archaea (108−109/mL), bacteria (1010−1011/mL), ciliate protozoa (106/mL), and fungi (106/mL), which facilitate the degradation of complex plant carbohydrates into small molecules [1] and ultimately provide metabolites that can be used by the ruminant animal [2][3][4][5]. Livestock are mainly fed with agricultural crops, which via microbial activity are converted to metabolic intermediates (i.e., volatile fatty acids (VFAs), such as acetate, butyrate and propionate, and hydrogen (H2) and gaseous end products such as carbon dioxide (CO2) and methane (CH4) [6]. Increased microbial H2 production and its subsequent accumulation, which can be promoted by a high-starch diet, have several detrimental effects on the rumen ecosystem and that can be attributed to a decrease in rumen pH triggered by starch fermentation. These effects include the deactivation of specific biomass-degrading enzymes from some of the most efficient fiber degraders of the rumen microbiome but also system-level responses, such as the reduction of feed conversion within the rumen [7][8]. Methanogens, a group of microbes belonging to the phylogenetic group of the archaea, combine molecular H2 with CO2 to produce CH4 during methanogenesis, enabling the removal of H2 from the system [9][10]. Although this removal of H2 is important for maintaining a healthy rumen ecosystem, from the viewpoint of nutrient expenditure methanogenesis is a costly process, accounting for a gross energy intake loss of 2–12% in ruminants [11][12][13][14]. Since the annual production of enteric CH4 accounts for ~15% of total anthropogenic CH4 emissions [11][15], with CH4 having a global warming potential 23-fold higher than that of CO2, there is also a real and severe environmental cost associated with the energy of the enteric CH4 that is released into the atmosphere.
Strategies and factors for CH4 abatement have been reviewed in the past [1][9][12][16][17][18][19][20][21][22][23][24][25] and many of the strategies used to mitigate CH4 from ruminants involve the use of antibiotics, ionophores [26], halogenated CH4 analogues [27][28][29], heavy metals [30], lipid-rich materials such as coconut oil [31][32][33], probiotics [27], bacteriocin [34], and numerous chemicals [35][36]. Immunization against methanogens [37][38], elimination of ciliate protozoa (defaunation) both in in vivo and in vitro [39] and addition of acetogenic bacteria to rumen fluid [40][41][42] in in vitro experiments have also been tested. Use of toxic chemicals and antibiotics as inhibitors, although considered an option in the past, are no longer accepted due to rising concerns regarding their impact on the environment, the animal, and potentially on the consumer of the animal products [43]. Interventions using phage therapy, altering methanogenic diversity and chemogenomic approaches [6] are some of the more recent technologies, but the extent to which these processes remove and eliminate the produced H2 still remains to be investigated. Therefore, a critical step for a successful CH4 reduction strategy may be one that uses natural processes within the rumen. One such approach relies on establishing a non-methanogenic sink for H2 produced during fermentation.

2. Hydrogen: A Key Player in Rumen Fermentation

H2 concentration plays a major role in the regulation of microbial fermentation in the rumen [44][45][46][47]. The partial H2 pressure is a key regulator of H2 metabolism and the fate of ruminal H2 disposal with dissolved H2 gas and H2 ion determining the redox potential of the rumen liquor. The efficient elimination of H2 enhances fermentation by reducing its inhibitory effect on microbial growth and microbial degradation of plant material [48][49]. Destiny of H2 liberation is associated with favorable thermodynamic changes and an inverse correlation between Gibbs free energy (ΔG0) and the minimum partial H2-pressure that is required for a reaction to continue: a reaction is considered to be thermodynamically more competitive when its requirement of H2 partial pressure is low [50]. Due to this central regulatory role in rumen fermentation, H2 can be considered to be the currency of ruminal fermentation [51]. Removal of the major fraction of the rumen H2 occurs via the methanogenic archaea to CH4, during which four moles of H2 are consumed and converted into one mole of CH4, which is then released into the atmosphere though eructation. During hydrogenotrophic methanogenesis, methanogens use CO2 as carbon source and terminal electron acceptor and H2 as electron donor. Other non-methanogenic rumen microbes, using CO2 and other electron acceptors such as sulfate, nitrate, and fumarate, compete with methanogens for H2, but they play a less dominant role in the removal of H2 from the rumen ecosystem [52][53]. Non-methanogenic bacteria that use H2 as electron donor include acetogens that reduce CO2 to form acetate by the Wood-Ljungdahl pathway [54], sulfate-reducing bacteria (SRB) that reduce sulfate to hydrogen sulfide [55], nitrate-reducing bacteria (NRB) that reduce nitrate (NO3) to ammonia (NH4) and fumarate-reducing bacteria that use H2 to form succinate [56][57]. Succinate can subsequentially be decarboxylated to propionate, which is a valuable nutrient for the ruminant animal [58], either by the succinate producer itself or it can be transferred to succinate users as an intercellular electron carrier [45]. Figure 1 summarizes the microbial pathways for H2 removal from the rumen.
Methane 01 00024 g001 550
Figure 1. Major and minor H2 and CO2 sequestering pathways in rumen.
Ruminal methanogenesis, contributing CH4 to the atmosphere, is directly and inversely linked to the animal productivity. The ability to control CH4 emission especially reduce methanogenesis from agriculture has enormous environmental and socioeconomic implication, but it also requires a detailed understanding of the microorganisms and microbial processes that are involved. Although a complete understanding of these highly interwoven microbial and metabolic networks has still not been achieved and most likely will not be feasible in the immediate future, there are some aspects that are reasonably well understood. These aspects represent a promising starting point for targeted CH4 reduction from ruminants. One of the promising key intermediates that has been recognized as such and that has received significant attention for targeted CH4 mitigation is metabolic H2 and the metabolic pathways, microbes and enzymes involved its production and consumption.
Since H2 is an immediate precursor for the archaeal reduction of CO2 into CH4, biological approaches that redirect H2 away from archaeal methanogenesis and into alternate metabolic pathways seem to be the most promising approaches to convert feed carbon into metabolic energy for the ruminant instead of releasing it into the atmosphere. Redirecting H2 through reductive acetogenesis and propionogenesis has advantages over other pathways due to production of valuable metabolic end products that can be used by the host animal as nutrients and can be converted into animal proteins for human consumption. Although the understanding of how to redirect metabolic H2 into more favorable pathways facilitates the production of value-added metabolic intermediates and therefore redirects otherwise lost feed energy, several issues related to the fine tuning of this redirection, such as the co-factor requirements, toxicity of metabolic intermediates, as well as thermodynamics of competing metabolic processes, need to be investigated in greater detail. A further aspect that will have to be investigated in future and that will have direct implications for the translational value of findings on the area of rumen nutrition and function is the link and dependence of the rumen microbiome and its function in dietary conversion.

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Contributors MDPI registered users' name will be linked to their SciProfiles pages. To register with us, please refer to https://encyclopedia.pub/register :
Prasanta Kumar Choudhury
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Rajashree Jena
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Sudhir Kumar Tomar
,
Anil Kumar Puniya
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