scholarly journals Climate Regimes Override Micro-Site Effects on the Summer Temperature Signal of Scots Pine at Its Northern Distribution Limits

2018 ◽  
Vol 9 ◽  
Author(s):  
Jelena Lange ◽  
Allan Buras ◽  
Roberto Cruz-García ◽  
Marina Gurskaya ◽  
Risto Jalkanen ◽  
...  
2012 ◽  
Vol 77 (3) ◽  
pp. 344-354 ◽  
Author(s):  
Anna Coppola ◽  
Giovanni Leonelli ◽  
Maria Cristina Salvatore ◽  
Manuela Pelfini ◽  
Carlo Baroni

Tree rings from temperature-limited environments are highly sensitive climate proxies, widely used to reconstruct past climate parameters for periods prior to the availability of instrumental data and to analyse the effect of recent global warming on tree growth. An analysis of the climatic signal in five high-elevation tree-ring width chronologies of European larch (Larix decidua Mill.) from the tops of five different glacial valleys in the Italian Central Alps revealed that they contain a strong summer-temperature signal and that tree-ring growth is especially influenced by June temperatures. However, a moving correlation function analysis revealed a recent loss of the June temperature signal in the tree-ring chronologies. This signal reduction primarily involves the two lowest-altitude chronologies. It is probable that the observed increasing importance of late-summer temperature for tree-ring growth over the past 50 yr is an effect of the lengthening growing season and of the variations in the climate/tree-ring relationship over time. All the chronologies considered, especially those at the highest altitudes, show an increasing negative influence of June precipitation on tree-ring growth. The climatic signal recorded in tree-ring chronologies from the Italian Central Alps varies over time and is also differentially influenced by climatic parameters according to site elevation.


2009 ◽  
Vol 66 (8) ◽  
pp. 810-810 ◽  
Author(s):  
Hannu Salminen ◽  
Risto Jalkanen ◽  
Markus Lindholm

2019 ◽  
Vol 286 (1899) ◽  
pp. 20190442 ◽  
Author(s):  
Inger Maren Rivrud ◽  
Erling L. Meisingset ◽  
Leif Egil Loe ◽  
Atle Mysterud

With climate change, the effect of global warming on snow cover is expected to cause range expansion and enhance habitat suitability for species at their northern distribution limits. However, how this depends on landscape topography and sex in size-dimorphic species remains uncertain, and is further complicated for migratory animals following climate-driven seasonal resource fluctuations across vast landscapes. Using 11 years of data from a partially migratory ungulate at their northern distribution ranges, the red deer ( Cervus elaphus ), we predicted sex-specific summer and winter habitat suitability in diverse landscapes under medium and severe global warming. We found large increases in future winter habitat suitability, resulting in expansion of winter ranges as currently unsuitable habitat became suitable. Even moderate warming decreased snow cover substantially, with no suitability difference between warming scenarios. Winter ranges will hence not expand linearly with warming, even for species at their northern distribution limits. Although less pronounced than in winter, summer ranges also expanded and more so under severe warming. Summer habitat suitability was positively correlated with landscape topography and ranges expanded more for females than males. Our study highlights the complexity of predicting future habitat suitability for conservation and management of size-dimorphic, migratory species under global warming.


Author(s):  
Jeong-Wook Seo ◽  
Dieter Eckstein ◽  
Andrea Olbrich ◽  
Risto Jalkanen ◽  
Hannu Salminen ◽  
...  

1995 ◽  
Vol 73 (8) ◽  
pp. 1234-1241 ◽  
Author(s):  
Stephen D. Murphy ◽  
Liette Vasseur

Pollen and (or) pollinator limitation may be most likely to occur in spring wildflowers or populations of species near their distribution limits. From 1990 to 1992, we examined a 2-ha population of a perennial spring wildflower, Hepatica acutiloba (Ranunculaceae), at the northern distribution limit of the species. To distinguish between the often confounded effects of pollen and resource limitation, we applied partial and whole-plant treatments. Ramets were open-pollinated, cross-pollinated, open- and cross-pollinated (50% of flowers were open-pollinated, and 50% were hand-pollinated), or self-pollinated. Although there was year to year variation, plants with cross-pollinated flowers produced significantly more viable seeds and heavier seeds than plants with self- or open-pollinated flowers. Comparisons between seed numbers and masses from complete and partial treatments suggested that there was no reallocation of resources among flowers on a plant. From 1990 to 1992, a minimum of 95% of all visits to a subset of ramets of H. acutiloba were from Asclera ruficollis (Coleoptera: Oedemeridae), i.e., virtually the only insect active during flowering. Mark–recapture data for A. ruficollis indicated that even after 6–48 h, 22–40% of the individuals remained within 10 m of the same ramet of H. acutiloba. Observational data indicated that less than 50% of all flowering ramets of H. acutiloba may be visited by A. ruficollis. We conclude that pollen limitation, mediated by reliance on one sedentary pollinator, was the main cause of low seed production in open-pollinated flowers of H. acutiloba. Key words: Hepatica acutiloba, pollen limitation, pollinator limitation, distribution limit, Asclera ruficollis, Oedemeridae.


2015 ◽  
Vol 42 (1) ◽  
Author(s):  
Jan Esper ◽  
Oliver Konter ◽  
Paul J. Krusic ◽  
Matthias Saurer ◽  
Steffen Holzkämper ◽  
...  

Abstract Substantial effort has recently been put into the development of climate reconstructions from tree-ring stable carbon isotopes, though the interpretation of long-term trends retained in such timeseries remains challenging. Here we use detrended δ13C measurements in Pinus uncinata tree-rings, from the Spanish Pyrenees, to reconstruct decadal variations in summer temperature back to the 13th century. The June-August temperature signal of this reconstruction is attributed using decadally as well as annually resolved, 20th century δ13C data. Results indicate that late 20th century warming has not been unique within the context of the past 750 years. Our reconstruction contains greater am-plitude than previous reconstructions derived from traditional tree-ring density data, and describes particularly cool conditions during the late 19th century. Some of these differences, including early warm periods in the 14th and 17th centuries, have been retained via δ13C timeseries detrending - a novel approach in tree-ring stable isotope chronology development. The overall reduced variance in earlier studies points to an underestimation of pre-instrumental summer temperature variability de-rived from traditional tree-ring parameters.


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