Improving Human Diets and Welfare through Using Herbivore-Based Foods: 2. Environmental Consequences and Mitigations
Abstract
:Simple Summary
Abstract
1. Introduction
2. Land Use
- Traditional extensive grazing in southern Europe and mountainous ecosystems created a mosaic of habitats resulting in biodiversity;
- Short-term abandonment following overgrazing had positive effects in central Europe and lowlands but not in southern European mountains;
- The abandonment of long-term traditional grazing activities in mountainous ecosystems resulted in the extinction of populations of species tightly linked with open habitats; and
- In lowlands, the abandonment of some grazing patches augments habitat diversification and creates new habitats for more species, but overgrazing caused a significant decrease in biodiversity.
Production System | Comment | Reference | |||
---|---|---|---|---|---|
Meat from Feedlot-Fed Animals | Meat from Grazed-Pasture Animals | Plant-Based Meat | Lab-Grown Meat | ||
Beef +*22 | Western Canada—lifetime GHG emissions | [50] | |||
Dairy +3.8 to +6.2 | Mycoprotein based +2.4 to +2.6 | [51,52] | |||
+1.8 to +2.3 | [45] | ||||
Beef +9 to +42; Dairy +1 to +2 | Suckler herds +23 to +52 Extensive pastoral +12 to +129 | +1 to +2 | Review of numerous studies | [53] | |
+31 | +7.5 | Feedlot beef in upper midwest USA | [44] | ||
Dairy +4.3 to +4.9 Chicken meat +5.2 to +5.8 | Soymeal-based +2.6 to +2.8 Mycoprotein-based +5.5 to +6.1 | +23.9 to +24.6 | Cradle-to-plate life cycle | [43] | |
+150 | +35 | [54] | |||
+33—US feedlot | +3.5 per kg beef | Total cradle-to-distribution impacts Beyond Burger and U.S. beef in feedlot | [55] | ||
Feedlot from +6.09 to +6.12 due to soil erosion | Rotationally grazed systems moved from +9.62 to −6.65 due to soil erosion | Change due to inclusion of soil organic matter accumulation in analysis | [56] | ||
+48.4 | Full LCA for USA beef—includes feed production and feedlot | [57] | |||
+33—US feedlot beef | −3.5 for grazed pastures | Rotational grazed beef can in some circumstances have a negative carbon impact due to soil C sequestration | [58] | ||
+21.3 | Full LCA for USA beef for feedlot and processing, etc. | [59] | |||
Beef +48 to +210 Dairy +35 to +45 Sheep +80 to +190 | +5 to +35 | +15 to +40 | [60] | ||
+11 (feedlot finished beef) | −3.5 (grazed) | +3.5 (soy-based) +3 (pea-based) | Cradle-to-distribution LCA, but excludes GHGE potential of retail, restaurant, or at-home use, and end-of-life stages | [61] | |
+42 to +235 | +21 to +55 | Range depends on functional unit and allocation method | [62] | ||
+6.01 for sheep and +8.97 for beef cattle | “Cradle-to-grave” for average NZ sheep and beef (weighted for traditional and dairy beef)—grazed pasture | [63] | |||
+4.9 to +25.2 | [64] | ||||
Traditional beef +10.09 Dairy beef +6.88 Sheep +6.01 | NZ—Cradle-to-farm-gate GHG emissions per kg live-weight sold (kg CO2e kg−1 LW) for grazed pasture | [65] | |||
+11 (dairy +40 (beef) | +2.2 to +24.8 | Current benchmark; best and worst case for cultured meat | [66] |
3. Greenhouse Gas Emissions
- Feed type and quality: Improving the nutritive value of the grazed feed through replacing low-quality native pasture with improved higher-quality pasture increases the enteric methane emission (g/day) produced by ruminants but reduces the methane yield per unit of meat or wool produced [86,87]. The increase in dietary lipids that improves nutritive value through balancing the ratios of energy to protein in diets has been shown to reduce greenhouse gas emissions [88]. This has led to programs seeking to increase lipid levels in ryegrass [89,90]. It is also well known that the incorporation of species into pasture that express condensed tannins, which protect protein in the rumen will reduce greenhouse gas emissions [91,92]. Other forage species have been shown to reduce methane emissions when eaten such as biserrula (Biserrula pelecinus) [93,94], sulla (Hedysarum coronarium) [91,95], Lotus corniculatus [91,96], L. pedunculatus [97], and sainfoin (Onobrychis viciifolia) [98]. However, these species are agronomically inferior to the forages currently used and their management under grazing is a challenge. A program in white clover (Trifolium repens), the most used pasture legume in temperate areas, is set to achieve condensed tannin expression in leaf tissue through the use of a transcription factor taken from a closely related Trifolium species [99,100].
- Dietary additives such as oils, microalgae, macroalgae, nitrate, ionophores, protozoal control, phytochemicals from plant extracts, and 3-nitrooxypropanol have shown differing levels of efficacy in reducing methane production per kg dry matter consumed [101,102,103,104]. Macroalgae and 3-nitrooxypropanol have shown the greatest efficacy in reducing methane yield. The seaweeds Asparagopsis taxiformis and A. armata, when included at low concentrations in the feed of cattle and sheep, inhibit methanogenesis by up to 98% [105,106]. The active ingredient from these macroalgae are bromoforms (organic compounds that are classified as a probable human carcinogen by the US EPA, but can be found in chlorinated drinking water [107]). Bromoform inhibits an enzyme in the methanogenesis pathway [108]. Studies are mixed on whether there are negative impacts on animal health or food quality [109]. However, because bromoforms are rapidly metabolized by rumen microbes [110], to be effective they need to be included with feed at a rate of 0.4–1.0 mg/kg animal/day of bromoform [111]. For animals in pasture, the major difficulty is longevity of action. Further, to be cost effective the expense associated with wild harvest and indeed aquaculture production will need to be reduced [109]. Canola oil has been shown to reduce methane losses from cattle, but animal performance may be compromised due to lower feed intake and decreased fiber digestibility [112] Fumaric acid, which can utilize hydrogen (instead of it combining with carbon to form methane), has been disappointing as an additive [112,113,114], but when encapsulated in partially hydrogenated vegetable oil it suppressed methane formation by 19% [115]. The main ways that many of these additives reduce methane production is through reducing the number of rumen protozoa and inhibiting methanogen activity, increasing propionic acid production, which competes with methanogens for hydrogen, and inhibiting the activity of enzymes involved in methanogen activity [116].
- The breeding of animals with higher growth rates and increased fecundity [86,87,117]. Breeding ruminants with lower methane production has been shown to be a feasible option [118,119,120] with heritability of g methane/day of 0.29 ± 0.05, and for g methane/kg DMI of 0.13 ± 0.03 [121]. Breeding for animals with low methane production per unit of dry matter intake is unlikely to negatively affect fecal egg counts, adult ewe fertility, and litter survival traits, with no evidence for significant genetic correlations, but may reduce wool, live weight, and fat deposition traits [122].
- Rumen microbial manipulations through the use of vaccines [87,123,124,125]. A recent review has concluded that it is complicated to evaluate the real effectiveness of this strategy with few published studies that have directly assessed the complete approach from vaccination to enteric animal methane emission measurement [126]. Similarly, the antibiotic monensin as a rumen additive has shown some success in vitro but results from in vivo trials have been disappointing [113].
- Pasture management, which ensures grazing occurs when fiber content is low (e.g., prior to grasses maturing and flowering) has been proposed as a method of reducing methane emissions [91].
4. Water Use and Quality
- N fertilizer used in conjunction with urease inhibitors such as N-(n-butyl)-thiophosphoric triamide and N-(n-propyl)-thiophosphoric triamide with an ability to reduce N2O and ammonia emissions while preserving yield [168]. However, caution has been called for from a meta-analysis that concluded that urease inhibitors applied with 20–30 kg N/ha per application in the spring and autumn are unlikely to increase plant dry matter yields and lead to improved NUE [169].
- Supplementary feed formulations including essential oils [170].
- Plant breeding [174] to exploit genetic variation among and within species in traits that have the potential to improve NUE (such as condensed tannin content as discussed above [100]), internal and external critical N concentrations [175], protein degradability [176,177], and biological nitrification inhibition [178].
- Combining traits in complementary forage species mixtures [179] rather than monoculture grass or simple two-species mixtures could substantially reduce N leakage to the environment. For example, in New Zealand, a combination of a N-fixing legume (e.g., white clover) with a N-demanding grass (e.g., perennial ryegrass, which has a relatively high critical internal N content) and a herb that inhibits nitrification in the soil and/or dilutes the N concentration of urine (e.g., plantain, [178,180,181]), has been shown to reduce N leaching by up to 80% in lysimeter studies [182] and 40% in field studies [183]. Proof of practice for this approach is currently underway in whole-farm systems experiments over multiple years [184].
5. Carbon Sequestration
- Fertilizer application: N inputs (10 to 20 kg N/ha/year) to low-fertility grasslands can increase soil carbon [197]. However, whether or not N inputs are associated with increased soil carbon depends on grazing intensity [198,199]. A process-based model of the dynamics of carbon and N cycling between plants, soils, and animals in grazed temperate pastures indicated that the optimal N input for balancing food production, carbon sequestration, N loss to the environment, and greenhouse gas emissions in New Zealand is approximately 150 kg/ha N fertilizer [154]. Alternatively, P fertilizer application appears to have little effect on soil carbon accumulation following conversion from native vegetation to grasslands for grazing [196,200].
- Irrigation can result in variable and contradictory impacts on soil carbon. In desert and semi-arid areas, irrigation can increase soil carbon substantially, while in humid environments, no consistent effects have been observed [201]. Whitehead et al. [192] concluded that “no change or decreases in soil carbon stocks in response to irrigation in humid climates but increases could be expected at more arid sites where plant productivity is very low prior to irrigation”. In New Zealand, irrigation has been shown to decrease soil C [196,202] due possibly to effects on soil N levels in different soil types and management systems [203], whereas in arid and semi-arid environments, irrigation might be expected to increase soil C stocks due to increased plant growth and inputs to soils [201]. However, under irrigation it is likely that N2O emissions will increase by up to 140% [201].
- Refraining from draining peaty soils, which contain high quantities of soil C (and which can lose soil organic matter through the oxidation of organic matter after drainage) [204].
- Use of supplementary feed, such as hay or silage, which may result in small increases in soil carbon on paddocks where it is used but may also result in a small decrease in soil carbon at locations where it is produced due to the “length of time between harvest and re-establishment of the new crop, maximizing returns of organic residues, and adopting minimum tillage and direct-drill methods to reduce disturbance” [192].
- Increased forage production also tends to increase soil carbon [207]. The Conant et al. review [207] indicated that the main drivers were use of more permanent pasture, improved grazing management, use of legumes, and increasing earthworm numbers. Grazing intensity can also impact soil carbon loss or accumulation. Overgrazing is generally considered to result in reduced soil carbon [197,198,208,209]. However, some studies have shown decreased soil carbon at both high and low grazing frequencies but most often the maximum accumulation occurred at a moderate grazing intensity [210,211]. This depends on balance—Parsons et al. [198]. A comparison of C4 and C3 gases in a meta-analysis has shown that higher grazing intensity results in increases in soil carbon in C4 grasslands but decreases in C3 grasslands [212]. This difference could be due to the high lignin levels in C4 grasses, which slow their decomposition and subsequent carbon release [213]. However, it is generally accepted that soil organic matter is greater in grazed pastures than non-grazed grasslands or land used for row crops or hay production [214].
- Species and diversity of species used: Whitehead et al. [192] concluded that forage species with deeper rooting and higher fine-root density at greater depths could increase soil carbon stocks. However, evidence that increased species diversity would increase soil carbon is inconclusive. The Jena Experiment setup in 2002 in Germany to investigate the effects of plant diversity on element cycling and trophic interactions do support increased soil carbon with increased pasture diversity, but the research involved mowing 2–4 times per year, i.e., there was no food production aspect [215].
- Use of biochar as a soil amendment may lead to an increase in soil carbon levels but its use as a widespread amendment to pasture soils is in many cases impractical [192].
- Full inversion tillage, which seeks to bury topsoil with high carbon levels to depths below 40 cm while bringing to the surface soil with a high carbon saturation deficit [192]. This would be achievable only on flat to moderately contoured sites and would be useful only where the soil carbon value for the topsoil is at least twofold greater than that of the subsoil [216].
6. Concluding Comments and Looking to the Future
- Increased use of white clover and plantain in pasture seed mixtures;
- Ensuring that pasture is composed of forage species that are highly digestible with high protein and high energy, and low fiber content;
- Using ruminant animals with higher growth rates and increased fecundity;
- Reduced tillage when resowing and use of a nitrification inhibitor when using N fertilizer on intensive pastures;
- Including forages with levels of condensed tannins and possibly other phytochemicals that reduce methane emissions and do not affect palatability;
- Matching the use of fertilizer N with the demand driven by the number of animals per hectare to ensure the efficient conversion of N and feed inputs to milk and meat;
- Direct injection of animal slurry into soil where this is feasible;
- Maximizing carbon sequestration in soil where and when this is possible through reducing soil disturbance and fallowing; and
- Avoiding overgrazing, which can negatively affect persistence and result in soil disturbance through resowing.
Author Contributions
Funding
Institutional Review Board Statement
Informed Consent Statement
Data Availability Statement
Conflicts of Interest
References
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Species | Feed System | Emissions (Million Tonnes CO2-eq) | Emission Intensity (Kg CO2-eq/kg Product) | ||
---|---|---|---|---|---|
Milk | Meat | Milk | Meat | ||
Dairy | Grazing 1 | 227 | 104 | 2.9 | 21.9 |
Mixed 2 | 1104 | 382 | 2.6 | 17.4 | |
Total | 1331 | 486 | 2.6 | 18.2 | |
Beef | Grazing 1 | - | 875 | - | 102 |
Mixed 2 | - | 1463 | - | 56 | |
Total | - | 2338 | - | 67 | |
Sheep | Grazing1 | 30 | 76 | 9.8 | 23.8 |
Mixed 2 | 37 | 115 | 7.5 | 23.2 | |
Total | 67 | 191 | 8.4 | 23.4 | |
Goat | Grazing 1 | 18 | 27 | 6.1 | 24.2 |
Mixed 2 | 44 | 84 | 4.9 | 23.1 | |
Total | 62 | 111 | 5.2 | 23.3 | |
Total from grazing systems 1 | 275 | 1082 | 6.3 | 43.0 | |
Total from mixed rations 2 | 1185 | 2044 | 5.0 | 30.0 | |
Grand total | 1460 | 3126 | 5.4 | 33.0 |
Variable | Land Use | ||
---|---|---|---|
Pastoral | Cropping and Horticulture | Native Forest | |
Total N | +0.85 | +0.45 | −0.39 |
Total P | +0.70 | +0.24 | −0.32 |
Visual clarity | −0.45 | −0.24 | +0.30 |
Escherichia coli presence | +0.80 | (0.17) | −0.34 |
NZ land area (km3) | 107,672 | 4174 | 65,675 |
Total NZ land area (%) | 39.6 | 1.5 | 24.1 |
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Caradus, J.R.; Chapman, D.F.; Rowarth, J.S. Improving Human Diets and Welfare through Using Herbivore-Based Foods: 2. Environmental Consequences and Mitigations. Animals 2024, 14, 1353. https://doi.org/10.3390/ani14091353
Caradus JR, Chapman DF, Rowarth JS. Improving Human Diets and Welfare through Using Herbivore-Based Foods: 2. Environmental Consequences and Mitigations. Animals. 2024; 14(9):1353. https://doi.org/10.3390/ani14091353
Chicago/Turabian StyleCaradus, John R., David F. Chapman, and Jacqueline S. Rowarth. 2024. "Improving Human Diets and Welfare through Using Herbivore-Based Foods: 2. Environmental Consequences and Mitigations" Animals 14, no. 9: 1353. https://doi.org/10.3390/ani14091353
APA StyleCaradus, J. R., Chapman, D. F., & Rowarth, J. S. (2024). Improving Human Diets and Welfare through Using Herbivore-Based Foods: 2. Environmental Consequences and Mitigations. Animals, 14(9), 1353. https://doi.org/10.3390/ani14091353