because near the equator the environment is less harsh compared to Canada. i live in Calgary and it is a harsh cold and dry climate. comparing Vancouver and Calgary, Vancouver is more humid and usually warmer so there can be more diversity. also there is more sunlight near the equator.
Although it is popularly thought that high biodiversity relates to the more “benign” and less demanding environment in hot climates, recent research by Michael Huston of the University of Texas in “Biological diversity, soils, and economics” and “Precipitation, soils, NPP, and biodiversity: resurrection of Albrecht's curve”, Australian ecologist Tim Flannery in The Future Eaters
plus Jason Weir and Dolph Schluter in “The latitudinal gradient in recent speciation and extinction rates of birds and mammals” show that these are misconceptions.
Flannery and Huston both demonstrate that owing to the roughly four orders of magnitude greater age of their soils (except in the volcanic regions of the Pacific Rim), the productivity of the Tropical and Unenriched Worlds is very much less than those of the Enriched World of the extratropical northern and western hemispheres. Weir and Schluter show that speciation rates are much lower in the Tropical World than in the depauperate fauna of the Enriched. One would presume that with their extreme geological stability the Unenriched World of Australia and Southern Africa would have still lower speciation rates than the humid tropics
. This is especially true when one considers that many birds and mammals in Australia and Southern Africa require so much labour for reproduction that most adults must serve as “helpers at the nest” rather than reproduce on their own, which acts as an extremely severe limiter on potential dispersal.
All these indicators point to the higher diversity of the Tropical and Unenriched Worlds as being due to reduced interspecific competition
compared to the young and highly productive Enriched World. Soils of an infertility universal in all of the Unenriched and most of the Tropical World are exceedingly rare in the Enriched World - occurring only in a few areas of exceptionally nutrient-poor parent materials
like ultrabasic rocks (serpentines, peridotites) - and then only outside of glaciation limits within which intrazonal parent materials are converted to highly fertile zonal soils. (In this context, it’s notable that the most northerly major biodiversity hotspot in the Klamath Basin is one of the major occurrences of serpentines in the world, as is the very rich tropical hotspot of New Caledonia).
In the Tropical and Unenriched World resources are so scarce in unfertilised environments that co-operation rather than competition tends to be the rule to allow plants to obtain the minimal nutrition possible on these soils. The absence of competition reduces extinction rates to a fraction of the level observed throughout the Enriched World: in essence, the creation of biodiversity occurs in the Enriched World, but it is rapidly pooled into reservoirs in the Tropical World, and the Unenriched retains older species (marsupials, mousebirds) dating from periods when its ecological conditions were globally general.
Although it is popularly thought that high biodiversity relates to the more "benign" and less demanding environment in hot climates, recent research by Michael Huston of the University of Texas in "Biological diversity, soils, and economics" and "Precipitation, soils, NPP, and biodiversity: resurrection of Albrecht's curve", Australian ecologist Tim Flannery in The Future Eaters plus Jason Weir and Dolph Schluter in "The latitudinal gradient in recent speciation and extinction rates of birds and mammals" show that these are misconceptions.
Flannery and Huston both demonstrate that owing to the roughly four orders of magnitude greater age of their soils (except in the volcanic regions of the Pacific Rim), the productivity of the Tropical and Unenriched Worlds is very much less than those of the Enriched World of the extratropical northern and western hemispheres. Weir and Schluter show that speciation rates are much lower in the Tropical World than in the depauperate fauna of the Enriched. One would presume that with their extreme geological stability the Unenriched World of Australia and Southern Africa would have still lower speciation rates than the humid tropics. This is especially true when one considers that many birds and mammals in Australia and Southern Africa require so much labour for reproduction that most adults must serve as "helpers at the nest" rather than reproduce on their own, which acts as an extremely severe limiter on potential dispersal.
All these indicators point to the higher diversity of the Tropical and Unenriched Worlds as being due to reduced interspecific competition compared to the young and highly productive Enriched World. Soils of an infertility universal in all of the Unenriched and most of the Tropical World are exceedingly rare in the Enriched World - occurring only in a few areas of exceptionally nutrient-poor parent materials like ultrabasic rocks (serpentines, peridotites) - and then only outside of glaciation limits within which intrazonal parent materials are converted to highly fertile zonal soils. (In this context, it's notable that the most northerly major biodiversity hotspot in the Klamath Basin is one of the major occurrences of serpentines in the world, as is the very rich tropical hotspot of New Caledonia).
In the Tropical and Unenriched World resources are so scarce in unfertilised environments that co-operation rather than competition tends to be the rule to allow plants to obtain the minimal nutrition possible on these soils. The absence of competition reduces extinction rates to a fraction of the level observed throughout the Enriched World: in essence, the creation of biodiversity occurs in the Enriched World, but it is rapidly pooled into reservoirs in the Tropical World, and the Unenriched retains older species (marsupials, mousebirds) dating from periods when its ecological conditions were globally general.
The weather there is more temperate and, therefore, more survivable.
The regions closer to the equator are hotter and more moist than those further from the equator. They receive more solar energy than the poles.
The least species diversity occurs in the areas that are the farthest from the equator
areas closer to the equator receive and
Because Mexico is closer to the equator.
-- your shirt more often -- your latitude
The regions closer to the equator are hotter and more moist than those further from the equator. They receive more solar energy than the poles.
The least species diversity occurs in the areas that are the farthest from the equator
Because FL. is closer to the equator and receives sun at a more direct angle. Because FL. is closer to the equator and receives sun at a more direct angle.
The light at the equator hits the earth perpendicular to the surface to the earth. The further you are from the equator, the light comes in at an angle closer and closer to parallel. The closer to parallel the light comes in at, the more of it is reflected, so it receives less energy than the perpendicular light at the equator.
The temperatures at the equator tend to be higher because the equator receives more direct sunlight.
Laos is closer to the Equator (:
WE are closer to they equator.
areas closer to the equator receive and
Mexico is closer to the equator
Laos
Because Mexico is closer to the equator.
-- your shirt more often -- your latitude