Expansion Of Deciduous Forests Research Articles

Late glacial and early Holocene hydroclimate variability in northwest Iran (Talesh Mountains) inferred from chironomid and pollen analysis

We reconstructed the paleohydrologic and climatic history of the Lake Neor region, NW Iran, from the end of the late glacial to the middle Holocene (15,500–7500 cal yr BP). Subfossil chironomid and pollen assemblages in a sediment core from a peatland located south of Lake Neor enabled identification of four main hydrologic phases. The period 15,500–12,700 cal yr BP was characterized by a relatively dry climate with an open landscape, suggested by the abundance of Irano-Turanian steppe plants (e.g. Amaranthaceae, Artemisia and Cousinia). Dominance of several shallow-water and semi-terrestrial chironomid taxa (e.g. Pseudosmittia, Smittia/Parasmittia and Paraphaenocladius/Parametriocnemus) during this period is indicative of lower water tables in the wetland. Between 12,700 and 11,300 cal yr BP, chironomid taxa indicate higher wetland water tables, as suggested by the presence of Zavrelia, Chironomus anthracinus/plumosus-type and Micropsectra, which are inhabitants of open-water, lacustrine areas. The open-steppe vegetation remained dominant in the watershed during this time. Increasing wetland moisture could be explained by: (1) cool summers that reduced the evaporation rate; and/or (2) a decrease in duration of the summer dry season. The period 11,300–8700 cal yr BP was characterized by lower wetland moisture, contemporaneous with a delay in the expansion of deciduous forest, suggesting persistent dry climate conditions throughout the beginning of the Holocene, which may have been related to the intensified seasonality of precipitation. Around 8700 cal yr BP, higher wetland water levels, inferred from chironomids, occurred simultaneously with the onset of regional deciduous forest expansion, probably caused by a shortening of the summer dry period. We concluded that chironomids are appropriate paleoecological proxies to investigate global and local hydrologic variability in the Middle East.

Impacts of Vegetation Change on the Regional Surface Climate: A Scenario-Based Analysis of Afforestation in Jiangxi Province, China

The afforestation is one of the most noticeable human activities that affect the climate through influencing not only the carbon sink but also the thermal properties of the land surface. This research accessed the potential effects of artificial vegetation change on the regional climate in Jiangxi Province, China. Based on simulation with the Weather Research and Forecasting (WRF) model, a comparative analysis was carried out on the future temperature and precipitation under four hypothetical vegetation cover scenarios. The simulation results indicated that the vegetation change would have significant effects on the regional climate. The simulated effects of annual average temperature showed a decreasing order: evergreen broadleaf > evergreen needleleaf > deciduous needleleaf > deciduous broadleaf, and the effects of annual average precipitation of the evergreen forests would be bigger than those of the deciduous forests. The deciduous forests play a positive role in decreasing the annual average temperature, while the evergreen forests promote the annual average temperature rise. Besides, the expansion of deciduous forests may result in severe drought in the summer in Jiangxi Province. These conclusions are of important policy implication to the future afforestation in Jiangxi Province, China, and other regions of the world.

Signatures of rapid climatic changes in organic matter records in the western Mediterranean Sea during the last glacial period

AbstractRecords of calcium carbonate, organic matter (organic carbon content, palynology) and planktonic foraminiferal oxygen isotopes from ODP Site 976, Alboran Sea, are used to reconstruct the evolution of continental climates and oceanic productivity in the westernmost Mediterranean over the past 50,000 years. The records mimic the Greenland ice core records in that they display the Heinrich events and the rapid Dansgaard/Oeschger-type stadial-interstadial oscillations. Warm interstadials correlate with an expansion of deciduous forests on the adjacent continents and enhanced river runoff and organic matter flux from terrestrial sources. In contrast, cold stadials are characterized by an expansion of semi-desert vegetation, reduced river runoff and limited terrestrial organic matter flux. The organic carbon record displays a longer-term cyclicity that correlates with the North Atlantic ’Bond’ cooling cycles. The records enable the documentation of rapid changes of continental climates in the western Mediterranean borderlands that caused changes in river runoff and in oceanic productivity that were driven by rapid fluctuations of the Atlantic inflow into the Mediterranean Sea. The combined terrestrial-marine patterns demonstrate the close linking of western Mediterranean climate with the climatic evolution in the North Atlantic region.

Abrupt vegetation changes in the Segura Mountains of southern Spain throughout the Holocene

Summary The fossil pollen record of Cañada de la Cruz in the Segura mountains of southern Spain yields insights into high‐elevation vegetational dynamics over the last c. 8320 years. Phases of xerophytic grassland alternate with high‐mountain open pine forests and expansion of deciduous forests and Mediterranean scrub at lower altitudes. Longer‐term stable vegetation patterns are interrupted by multidecadal to century‐scale shifts at about 7770, 3370, 2630, 1525 and 790 years BP. Some of the vegetation types have no modern analogues and represent high‐altitude remnants of widespread last‐glacial xerophytic communities. Other species patterns, characteristic of current scrub associations, appeared only within the last 800 years. The sequence fits within the regional context of a generally wet mid‐Holocene (c. 7700–3300 years BP) characterized by spread of mesophilous vegetation, between drier conditions characterized by greater abundance of xerophytes. The pollen record and current ecological studies on high‐elevation vegetation of Mediterranean Spain suggest that control of vegetation is primarily climatic although grazing pressure, which would have pushed vegetation over a threshold for change, cannot be discounted.

DIFFERING LEVELS OF AMONG-POPULATION DIVERGENCE IN THE MITOCHONDRIAL DNA OF PERIODICAL CICADAS RELATED TO HISTORICAL BIOGEOGRAPHY.

Mitochondrial DNA (mtDNA) haplotypes were determined for 118 individuals of 13-and 17-year periodical cicadas (genus Magicicada) collected from 16 localities throughout the Midwest and eastern United States. Two distinct mtDNA lineages, identified as A and B, differ by 2.5% based on analysis of fragment patterns and restriction maps. Observed levels of mtDNA diversity within each lineage are low compared to estimates for other taxa. The two lineages are regionally segregated, with the boundary line occurring at a latitude of approximately 33° North. The levels of mtDNA diversity and population genetic structure differ within the two lineages. There is a remarkably low level of mean mtDNA divergence and no genetic structure in lineage A, whereas lineage B exhibits an order of magnitude higher level of mtDNA diversity and significant genetic structure among sampled populations. The low level of mtDNA diversity in cicadas may be attributed to (1) a population bottleneck that most likely occurred during the Pleistocene, (2) recent colonization following the retreat of the glaciers and the expansion of deciduous forests, and/or (3) high among-family reproductive variance (as a consequence of large population size, high fecundity, aggregative behavior of adults, and clumping of eggs). The difference in mtDNA diversity and population genetic structure between the lineages suggests that they experienced different biogeographic histories; we relate this to Pleistocene changes.