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In the case of rodent infections with malaria parasites of which there are three known species, one of the features of P. berghei-, P. yoelii-, and P. chabaudi-infected erythrocytes is their ability to sequestrate in various organs of the body [ 30– 33]; however, the sequestration patterns differ from that of P. falciparum-infected erythrocytes [ 34, 35].
This will improve our understanding of the impact of physiological and environmental factors on CO2 efflux and sequestration patterns over the region.
As an alternative, model-based approaches can be specified to be dynamic by incorporating future forest conditions and global change scenarios to determine their implications on C stocks and sequestration patterns.
Although aridity was not found to influence the global distribution of coarse root biomass [8], what role might precipitation and/or its interaction with temperature and other climate variables play in determining future C sequestration patterns and stocks?
To test for differences in sequestration patterns between various mouse strains a transgenic P. berghei line (pbGFP-LUCsch) was used that expresses a GFP-luciferase fusion protein under the control of the schizont-specific promoter from the ama1 gene of P. berghei [27].
Finally, as a means of refining NGHGIs, climate-adjusted models depicting belowground C stocks should be adopted to incorporate the impacts of future global change and management scenarios on C sequestration patterns and stocks.
Similar(51)
The mechanism underlying the different sequestration pattern needs to be determined.
There are similarities in this sequestration pattern with other rodent malaria species.
The effects of RNIs on IRPs may therefore explain the iron-sequestration pattern that characterises macrophages under inflammatory conditions.
Although the comparison revealed some slight variability in CO2 efflux and uptake values for the variety of ecosystems presented (Table 3), the general observation revealed that soil moisture as well as other physiological properties of the ecosystems were very significant in the CO2 sequestration and efflux patterns over the regions.
Although the comparison revealed some slight variability in CO2 efflux and uptake values for the variety of ecosystems presented (Table 3), the general observation revealed that soil moisture as well as other physiological properties of the ecosystems were very significant in the CO2 sequestration and efflux patterns over the regions.
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