A unifying conceptual model is constructed for the major effects of alternating periods of global warming and cooling and sea-level changes on the geographical distributions and the ecological and genetic characteristics of species and ecological communities.
The main results found are:
The species in the interior of continuous global latitude and altitude temperature gradients are expected to follow the moving temperature zones without any major extinctions or any major changes in their physiological and ecological characteristics and adaptive roles during both global warming and global cooling periods, with competitive replacement of resident species by zonally dispersing pre-adapted species.
Many or all of the existing species at all the global cold boundary zones of both latitude and altitude temperature gradients are expected to become extinct during periods of global warming, which would be caused by competitive displacement by immigrating pre-adapted species from adjacent warmer zones.
Most existing species in the warm boundary zones of all the global temperature gradients are predicted to persist and adapt without competition to the increased temperature during periods of global warming, and to diversify by adaptations to newly created ecological opportunities.
Periods of global cooling are predicted to cause analogous opposite effects to the effects of global warming in the cold and warm boundaries of temperature gradients: that is, extinctions at the warm boundaries and persistence and adaptations at the cold boundaries:
Existing species in all islands and island-like isolated areas are predicted to persist in the absence of competitive displacement by immigrating pre-adapted species, and gradually adapt to the changing temperatures during periods of both global warming and global cooling.
During periods of global cooling, many more diverse opportunities for new adaptations and for invasions by pre-adapted species are expected and predicted in the large diversity of the newly open heterogeneous coldest and highest altitude zones of all the global altitude temperature gradients.
Long-term sequences of alternating periods of global warming and global cooling are expected to cancel and eliminate most of the ecological and adaptive changes which have occurred during the previous periods at all the latitude and altitude boundary zones. The species at the interior of continuous temperature gradients are expected to persist unchanged over long evolutionary time during repeated sequences of alternating periods of global warming and global cooling.
The effects of higher and lower global sea levels on the sea shore and intertidal species and communities during periods of global warming or cooling are expected to be analogous to the bio-geographical, ecological and genetic changes caused or predicted by global warming or cooling in the species and communities in terrestrial or marine temperature gradients.
Global sea-level changes which cause higher or lower shifting of the levels of the ecological zones in continuous sea shore gradients are expected therefore to cause continuous tracking and moving of the populations of the unchanged zonally adapted species. On the other hand, zonally adapted sea shore species are expected to be displaced or become extinct during periods of sea-level changes at the higher or lower boundary zones of the sea-level gradients in semi-isolated marine basins, and in locally discontinuous, fragmented or truncated sea shore ecological gradients.
Purchase
Buy instant access (PDF download and unlimited online access):
Institutional Login
Log in with Open Athens, Shibboleth, or your institutional credentials
Personal login
Log in with your brill.com account
Ackerly DD, , Loarie SR, , Cornwell WK. 2010. The geography of climate change: implications for conservation biogeography. Diversit Distrib. 16(3):476–487, May 2010.
Adam P. 2002. Salt marshes in a time of change. Environ Conserv. 29(1):39–61.
Aitken SN, , Yeaman S, , Holliday JA. 2008. Adaptation, migration or extirpation: climate change outcomes for tree populations. Evol Appl. 1(1):95–111, February 2008.
Alsos IG, Eidesen PB, Ehrich D. 2007. Frequent long-distance plant colonization in the changing Arctic. Science. 316(5831):1606–1609, June 15 2007.
Baldwin BG, , Wagner WL. 2010. Hawaiian Angiosperm radiations of North American origin. Annals of Botany. 103(6):849–879, June 2010.
Belmaker J, Brokovich E, China V. 2009. Estimating the rate of biological introductions: Lessepsian fishes in the Mediterranean. Ecology. 90:1134–1141.
Belmaker J, Parravicini V, Kulbicki M. 2013. Ecological traits and environmental affinity explain Red Sea fish introduction into the Mediterranean. Glob Change Biol. 19(5):1373–1382.
Chust G, Albaina A, Aranburu A 2013. Connectivity, neutral theories and the assessment of species vulnerability to global change in temperate estuaries. Estuar Coast Shelf S. 131:52–63, October 2013.
Colwell RK, , Lees DC. 2000. The mid-domain effect: geometric constraints on the geography of species richness. Trends Ecol Evol. 15:70–76.
Diaz-Varela RA, Colombo R, Meroni M. 2010. Spatio-temporal analysis of alpine ecotones: A spatial explicit model targeting altitudinal vegetation shifts. Ecol Model. 221(4):621–633, February 24 2010.
Drummond CS. 2008. Diversification of Lupinus (Leguminosae) in The Western New World: Derived evolution of perennial life history and colonization of montane habitats. Mol Phylogenet Evol. 48(2):408–421, August 2008.
Dytham C. 2009. Evolved dispersal strategies at range margins. Proceedings of The Royal Society B-Biological Sciences. 276(1661):1407–1413.
Elith J, , Leathwick JR. 2009. Species distribution models: ecological explanation and prediction across space and time. Ann Rev Ecol Syst. 40:677–697.
Galbraith H, Jones R, Park R. 2002. Global climate change and sea level rise: Potential losses of intertidal habitat for shorebirds. Waterbirds. 25(2):173–183.
Galbreath KE, , Hafner DJ. 2009. When cold is Better: Climate-driven elevation shifts yield complex patterns of diversification and demography in an Alpine specialist (American Pika, Ochotona Princeps). Evolution. 63(11):2848–2863, November 2009.
Gilman SE, Urban MC, Tewksbury J. 2010. A framework for community interactions under climate change. Trends Ecol Evol. 23(6):323–331, June 2010.
Graham MH, Dayton PK, Erlandson JM. 2003. Ice ages and ecological transitions on temperate coasts. Trends Ecol Evol. 18(1):33–40.
Hamilton SK. 2010. Biogeochemical implications of climate change for tropical rivers and floodplains. Hydrobiologia. 657(1):19–35, December 2010.
Harsch MA, Hulme PE, McGlone MS. 2009. Are tree lines advancing? A global meta-analysis of tree line response to climate warming. Ecol Lett. 12(10):1040–1049, October 2009.
Jiguet F, Gregory RD, Devictor V. 2010. Population trends of European common birds are predicted by characteristics of their climatic niche. Glob Change Biol. 16(2):497–505, February 2010.
Jump AS, , Matyas C, , Penuelas J. 2009. The altitude-for-latitude disparity in the range retractions of woody species. Trends Ecol Evol. 24(12):694–701, December 2009.
Kawecki TJ, , Barton NH, , Fry JD.1997. Mutational collapse of fitness in marginal habitats and the evolution of ecological specialization. J Evol Biol. 10:407–429.
Kernan M, Ventura M, Bitusik P. 2009. Regionalization of remote European mountain lake ecosystems according to their biota: environmental versus geographical patterns. Freshwater Biol. 54(12):2470–2493, December 2009.
Kullman L, , Oberg L.2009. Post-Little Ice Age tree line rise and climate warming in the Swedish Scandes: a landscape ecological perspective. J Ecol. 97(3):415–429, May 2009.
La Sorte FA, , Jetz W. 2010. Avian distributions under climate change: Towards improved projections. J Exp Biol. 213:862–869 MAR 15 2010.
Lamback K, , Chappell J. 2001. Sea level change through the last glacial cycle. Science. 292(5517):679–686 27 April 2001.
Lande R. 2010. Adaptation to an extraordinary environment by evolution of phenotypic plasticity and genetic assimilation. J Evol Biol. 22(7):1433–1446, July 2009.
Lasram FBR, Guilhaumon F, Albouy C. 2010. The Mediterranean Sea as a ‘cul-de-sac’ for endemic fishes facing climate change. Glob Change Biol. 16(12):3233–3245, December 2010.
Lewis SE, , Sloss CR, Murray-Wallace CV. 2013. Post-glacial sea-level changes around the Australian margin: a review. Quaternary Sci Rev. 74(SI):115–138, August 15 2013.
Liebold MA, Holyoak M, Mouquet N. 2004. The meta community concept: a framework for multi-scale community ecology. Ecol Lett. 7:601–613.
McCain M, , Colwell RK. 2011. Assessing the threat to montaneous biodiversity from discordant shifts in temperature and precipitation in a changing climate. Ecol Lett. 14:1236–1245.
Murphy HT, , Van Der Wal J, , Lovett-Doust J. 2010. Signatures of range expansion and erosion in eastern North American trees. Ecol Lett. 13(10):1233–1244, October 2010.
Nicholls RJ, , Cazenave A. 2010. Sea-level rise and its impact on coastal zones. Science. 328(5985):1517–1520, June 18 2010.
Ohlemuller R, , Gritti ES, , Sykes MT, , Thomas CD. 2006. Quantifying components of risk for European woody species under climate change. Glob Change Biol. 12(9):1788–1799, September 2006.
Parmesan C. 2006. Ecological and evolutionary responses to recent climate change. Annu Rev Ecol Evol Syst. 37:637–669.
Reach TBH, , Thorsten BH, , Wood TE. 2007. Molecular ecology of global change. Mol Ecol. 16(19):3973–3992, October 2007.
Schoville SD, , Roderick GK. 2010. Evolutionary diversification of cryophilic Grylloblatta species (Grylloblattodea: Grylloblattidae) in alpine habitats of California. BMC Evol Biol. 10: Art. No. 163, June 2 2010.
Sexton, et al.. 2009. Evolution and ecology of species range limits. Annu Rev Ecol Evol Syst. 40:413–436.
Sterr H. 2008. Assessment of vulnerability and adaptation to sea-level rise for the coastal zone of Germany. J Coastal Res. 24(2):380–393, March 2008.
Svenning JC, , Skov F. 2004. Limited filling of the potential range in European tree species. Ecol Lett. 7:565–573, July 2004.
Svenning JC, , Skov F.2007. Could the tree diversity pattern in Europe be generated by postglacial dispersal limitation? Ecol Lett. 10(6):453–460, June 2007.
Thomas CD. 2010. Climate, climate change and range boundaries. Diversit Distrib. 16(3):488–495, May 2010.
Thuiller W, , Albert C, , Araujo MB, et al.. 2008. Predicting global change impacts on plant species' distributions: Future challenges. Perspectives In Plant Ecology Evolution And Systematics. 9(3–4):137–152.
Venditti C, , Pagel M. 2010. Speciation as an active force in promoting genetic evolution. Trends Ecol Evol. 23(1):14–20 Jan 2010.
Virkkala R, et al.. 2008. Projected large-scale range reductions of northern-boreal land bird species due to climate change. Biol Conserv. 141(5):1343–1353, May 2008.
Wake DB,, Hadly EA, , Ackerly DD. 2009. Biogeography, changing climates, and niche evolution. PNAS. 106:19631–19636 Suppl. 2, November 17 2009.
Wilson EO.1961. The Nature of the Taxon Cycle in the Melanesian ant fauna. The American Naturalist, 95(882):169–193 (May – June, 1961).
Yoder JB, et al.. 2010. Ecological opportunity and the origin of adaptive radiations. J Evol Biol. 23(8):1381–1396, August 2010.
| All Time | Past 365 days | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 328 | 61 | 13 |
| Full Text Views | 20 | 0 | 0 |
| PDF Views & Downloads | 12 | 0 | 0 |
A unifying conceptual model is constructed for the major effects of alternating periods of global warming and cooling and sea-level changes on the geographical distributions and the ecological and genetic characteristics of species and ecological communities.
The main results found are:
The species in the interior of continuous global latitude and altitude temperature gradients are expected to follow the moving temperature zones without any major extinctions or any major changes in their physiological and ecological characteristics and adaptive roles during both global warming and global cooling periods, with competitive replacement of resident species by zonally dispersing pre-adapted species.
Many or all of the existing species at all the global cold boundary zones of both latitude and altitude temperature gradients are expected to become extinct during periods of global warming, which would be caused by competitive displacement by immigrating pre-adapted species from adjacent warmer zones.
Most existing species in the warm boundary zones of all the global temperature gradients are predicted to persist and adapt without competition to the increased temperature during periods of global warming, and to diversify by adaptations to newly created ecological opportunities.
Periods of global cooling are predicted to cause analogous opposite effects to the effects of global warming in the cold and warm boundaries of temperature gradients: that is, extinctions at the warm boundaries and persistence and adaptations at the cold boundaries:
Existing species in all islands and island-like isolated areas are predicted to persist in the absence of competitive displacement by immigrating pre-adapted species, and gradually adapt to the changing temperatures during periods of both global warming and global cooling.
During periods of global cooling, many more diverse opportunities for new adaptations and for invasions by pre-adapted species are expected and predicted in the large diversity of the newly open heterogeneous coldest and highest altitude zones of all the global altitude temperature gradients.
Long-term sequences of alternating periods of global warming and global cooling are expected to cancel and eliminate most of the ecological and adaptive changes which have occurred during the previous periods at all the latitude and altitude boundary zones. The species at the interior of continuous temperature gradients are expected to persist unchanged over long evolutionary time during repeated sequences of alternating periods of global warming and global cooling.
The effects of higher and lower global sea levels on the sea shore and intertidal species and communities during periods of global warming or cooling are expected to be analogous to the bio-geographical, ecological and genetic changes caused or predicted by global warming or cooling in the species and communities in terrestrial or marine temperature gradients.
Global sea-level changes which cause higher or lower shifting of the levels of the ecological zones in continuous sea shore gradients are expected therefore to cause continuous tracking and moving of the populations of the unchanged zonally adapted species. On the other hand, zonally adapted sea shore species are expected to be displaced or become extinct during periods of sea-level changes at the higher or lower boundary zones of the sea-level gradients in semi-isolated marine basins, and in locally discontinuous, fragmented or truncated sea shore ecological gradients.
| All Time | Past 365 days | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 328 | 61 | 13 |
| Full Text Views | 20 | 0 | 0 |
| PDF Views & Downloads | 12 | 0 | 0 |