| Literature DB >> 32546223 |
Roberta Marques1, Rodrigo F Krüger1, A Townsend Peterson2, Larissa F de Melo1, Natália Vicenzi1, Daniel Jiménez-García3.
Abstract
Climate change ranks among the most important issues globally, affecting geographic distributions of vectors and pathogens, and inducing losses in livestock production among many other damaging effects. We characterized the potential geographic distribution of the ticks Rhipicephalus (Boophilus) microplus, an important vector of babesiosis and anaplasmosis globally. We evaluated potential geographic shifts in suitability patterns for this species in two periods (2050 and 2070) and under two emissions scenarios (RCPs 4.5 and 8.5). Our results anticipate increases in suitability worldwide, particularly in the highest production areas for cattle. The Indo-Malayan region resulted in the highest cattle exposure under both climate change projections (2050), with increases in suitability of > 30%. This study illustrates how ecological niche modeling can be used to explore probable effects of climate change on disease vectors, and the possible consequences on economic dimensions.Entities:
Year: 2020 PMID: 32546223 PMCID: PMC7298856 DOI: 10.1186/s13567-020-00802-z
Source DB: PubMed Journal: Vet Res ISSN: 0928-4249 Impact factor: 3.683
Figure 1Calibration area and the known distribution of()(points). Occurrence records used in model calibration (test and training) are shown; occurrences in Africa were used as independent data to evaluate the accuracy of model transfer worldwide.
Climate variables used in ecological niche modeling of current and future potential distributions of()
| Acronym | Description | % variable contribution |
|---|---|---|
| Bio1a | Annual mean temperature | 26.6 |
| Bio2 | Mean diurnal range | |
| Bio3 | Isothermality | |
| Bio4a | Temperature seasonality | 21.4 |
| Bio5 | Maximum temperature of warmest month | |
| Bio6 | Minimum temperature of coldest month | |
| Bio7 | Temperature annual range | |
| Bio8b | Mean temperature of wettest quarter | |
| Bio9b | Mean temperature of driest quarter | |
| Bio10 | Mean temperature of warmest quarter | |
| Bio11 | Mean temperature of coldest quarter | |
| Bio12a | Annual precipitation | 14.6 |
| Bio13 | Precipitation of wettest month | |
| Bio14a | Precipitation of driest month | 19.2 |
| Bio15 | Precipitation seasonality | |
| Bio16 | Precipitation of wettest quarter | |
| Bio17 | Precipitation of driest quarter | |
| Bio18b | Precipitation of warmest quarter | |
| Bio19b | Precipitation of coldest quarter | |
| RHa | Relative humidity | 18.1 |
Bioclimatic variables from the WorldClim data archive (version 1.4; Hijmans et al. [41]) and relative humidity [44] were used for modeling. Five variablesa were selected for modelling via our model selection processing [47].
bVariables excluded because they have unrealistic spatial artefacts [42].
Figure 2Present-day suitability for()according to the best ecological niche model, under current conditions and calibration area (detail).
Figure 3MOP analysis of extrapolation risk from the calibration area under current conditions to the whole world under future conditions. Blue values represent strict extrapolative areas. Red values represent levels of similarity between the calibration area and the different RCPs scenarios of projections.
Proportion of modification of. suitability to climate change scenarios according to zoogeographic regions and livestock abundance categories worldwide [54, 55] for 2050 scenarios
| Scenarios | Regions | Cattle abundance (individuals/10 km2) | |||||||
|---|---|---|---|---|---|---|---|---|---|
| 0–1 | 1–5 | 5–10 | 10–20 | 20–50 | 50–100 | > 100 | All categories (average) | ||
| RCP 4.5 | Afrotropic | 1.57 | 5.78 | 6.47 | 6.23 | 5.86 | 6.93 | 7.75 | 5.80 |
| Australasia | 6.26 | 6.10 | 0.91 | 1.41 | 9.94 | 7.81 | 3.99 | 5.20 | |
| Indo-Malayan | 3.02 | 2.82 | 3.55 | 3.27 | 5.64 | 8.76 | |||
| Nearctic | 3.62 | 2.87 | 4.52 | 4.40 | 2.46 | 8.49 | |||
| Neotropic | 9.42 | 5.71 | 4.87 | 5.61 | 5.70 | 4.44 | 8.95 | 6.39 | |
| Palearctic | 9.05 | 2.83 | 3.22 | 4.32 | 3.13 | 0.79 | 0.49 | 3.40 | |
| RCP 8.5 | Afrotropic | 0.60 | 1.96 | 1.33 | 2.19 | 1.98 | 1.23 | 1.72 | 1.57 |
| Australasia | 1.53 | 0.50 | 0.06 | 0.16 | 0.61 | 0.00 | 0.00 | 0.41 | |
| Indo-Malayan | 3.39 | 2.34 | 4.24 | 4.36 | 6.04 | 6.54 | 6.28 | 4.74 | |
| Nearctic | 2.50 | 1.90 | 1.62 | 5.65 | 30.36 | ||||
| Neotropic | 2.69 | 2.68 | 2.40 | 2.33 | 1.90 | 1.29 | 0.59 | 1.99 | |
| Palearctic | 6.61 | 4.80 | 1.78 | 12.28 | |||||
| Both | Afrotropic | 4.58 | 7.80 | 7.77 | 9.97 | 9.39 | |||
| Australasia | 5.97 | 8.18 | 7.26 | 9.26 | 7.92 | 2.91 | 7.88 | ||
| Indo-Malayan | 19.19 | ||||||||
| Nearctic | 4.25 | 2.50 | 1.68 | 2.35 | 8.62 | 3.01 | 10.39 | ||
| Neotropic | 9.71 | 7.82 | 5.44 | 8.87 | 12.50 | ||||
| Palearctic | 8.95 | 4.51 | 19.11 | ||||||
Values with increases greater than 10% are shown in italics.
Proportional modifications of()suitability to climate change scenarios divided by zoogeographic regions and livestock abundance categories worldwide [54, 55] for 2070 scenarios
| Scenarios | Regions | Cattle abundance (individuals/10 km2) | |||||||
|---|---|---|---|---|---|---|---|---|---|
| 0–1 | 1–5 | 5–10 | 10–20 | 20–50 | 50–100 | > 100 | All categories (average) | ||
| RCP 4.5 | Afrotropics | 3.23 | 8.86 | 9.04 | 5.10 | 1.96 | 7.09 | ||
| Australasia | 7.09 | 7.30 | 2.97 | 3.51 | 9.65 | 0.90 | 2.60 | 4.86 | |
| Indo-Malayan | 5.73 | 6.43 | 8.60 | 7.84 | 14.97 | ||||
| Nearctic | 2.19 | 1.81 | 2.03 | 1.22 | 0.82 | 0.00 | 2.82 | ||
| Neotropics | 9.47 | 8.88 | 6.95 | 11.29 | |||||
| Palearctic | 6.60 | 6.31 | 5.16 | 5.63 | 3.19 | 1.64 | 0.48 | 4.15 | |
| RCP 8.5 | Afrotropics | 0.09 | 0.81 | 0.50 | 0.75 | 1.16 | 4.03 | 5.97 | 1.90 |
| Australasia | 5.19 | 1.71 | 0.47 | 0.26 | 0.32 | 0.76 | 0.10 | 1.26 | |
| Indo-Malayan | 6.03 | 1.50 | 1.94 | 2.17 | 2.51 | 4.81 | 3.47 | 3.20 | |
| Nearctic | 2.25 | 1.11 | 0.78 | 1.73 | 4.97 | 4.03 | 14.43 | ||
| Neotropics | 0.95 | 2.02 | 1.33 | 1.45 | 1.76 | 1.06 | 0.09 | 1.24 | |
| Palearctic | 4.01 | 2.68 | 20.56 | ||||||
| Both | Afrotropics | 2.05 | 3.96 | 6.83 | 4.66 | 3.68 | 6.87 | 5.58 | |
| Australasia | 3.33 | 8.50 | 7.70 | 7.29 | 8.80 | ||||
| Indo-Malayan | 9.32 | 9.93 | 13.33 | ||||||
| Nearctic | 4.88 | 1.88 | 1.39 | 1.23 | 5.50 | 3.01 | 13.65 | ||
| Neotropics | 5.44 | 5.14 | 4.15 | 3.31 | 1.91 | 3.70 | 5.45 | ||
| Palearctic | 6.33 | 23.46 | |||||||
Values ≥ 10% are shown in italics.