scholarly journals Postglacial recolonization of North America by spadefoot toads: integrating niche and corridor modeling to study species’ range dynamics over geologic time

Ecography ◽  
2020 ◽  
Vol 43 (10) ◽  
pp. 1499-1509
Author(s):  
Iulian Gherghel ◽  
Ryan Andrew Martin
1914 ◽  
Vol s4-38 (223) ◽  
pp. 1-27 ◽  
Author(s):  
C. Schuchert ◽  
J. Barrell

Author(s):  
Damien A. Fordham ◽  
Sean Haythorne ◽  
Stuart C. Brown ◽  
Jessie C. Buettel ◽  
Barry W. Brook

Paleobiology ◽  
1978 ◽  
Vol 4 (3) ◽  
pp. 367-372 ◽  
Author(s):  
Carl F. Koch

The published fossil record has significant bias in favor of common and biostratigraphically important taxa when compared with data obtained from a thorough examination of several hundred collections from the Western Interior of North America. Overall species diversity is underestimated by a factor of 3 to 4, and bivalve and gastropod diversity by a factor of 5. The proportion of bivalves increased from 40 to 56% of the fauna, and the proportion of ammonites decreased from 28 to 18%. Thirteen published reports listed 65 species from 203 reported occurrences. Data from all sources showed 170 species for 1050 occurrences. By using abundance data and assuming a log-normal distribution, as many as 200 fossilizable mollusc species may have inhabited the Western Interior during the uppermost biozone of the Cenomanian. The importance of this study is that it quantifies the bias in the published fossil record relative to the potential fossil record for an unusually well studied interval of geologic time. The bias would be greater for less well studied strata.


2019 ◽  
Vol 22 (11) ◽  
pp. 1940-1956 ◽  
Author(s):  
Natalie J. Briscoe ◽  
Jane Elith ◽  
Roberto Salguero‐Gómez ◽  
José J. Lahoz‐Monfort ◽  
James S. Camac ◽  
...  

1999 ◽  
Vol 77 (7) ◽  
pp. 1128-1135 ◽  
Author(s):  
Michael E Nelson ◽  
L David Mech

We examined the seasonal migration and home-range dynamics of a multigeneration white-tailed deer (Odocoileus virginianus) matriline comprising six females from four generations spanning a 20-year period in northeastern Minnesota. All, from the matriarch to her great-granddaughter, migrated to the same summer and winter ranges, the longest individual record being 14.5 years. Three maternal females concurrently occupied exclusive fawning sites within their ancestral matriarch's summer range, while two nonmaternal females explored new areas and ranged near their mothers. One great-granddaughter expanded her summer range 1 km beyond the matriarch's summer range while essentially vacating half of her ancestors' range and becoming nonmigratory the last 4 years of her life. These data indicate that individual movements of matriline members can potentially expand their ranges beyond the areas occupied by their ancestors through a slow process of small incremental changes. This suggests that the rapid extension of deer range in eastern North America resulted from natal dispersal by yearling deer rather than from the type of home-range expansion reported here.


2020 ◽  
Author(s):  
Yassine Messaoud ◽  
Anya Reid ◽  
Nadezhda M. Tchebakova ◽  
Annika Hofgaard ◽  
Faouzi Messsaoud

Abstract BackgroundThe climate variables effect on tree growth in boreal and temperate forests has received increased interest in the global context of climate change. However, most studies are geographically limited and involved few tree species. Here, sixteen tree species across western North America were used to investigate tree response to climate change at the species range scale. MethodsForest inventory data from 36,944 stands established between 1600 and 1968 throughout western Canada and USA were summarized. Height growth (total height at breast-height age of 50 years) of healthy dominant and co-dominant trees were related to annual and summer temperatures, annual and summer Palmer Drought Severity Index (PDSI, and tree establishment date (ED). Climate-induced height growth patterns were then tested to determine links to spatial environment (soil conditions and geographic locations), species range (coastal, interior, and both ranges) and species traits (shade tolerance and leaf form), using linear mixed model for the global height growth and general linear model to test the height growth patterns for each species. ResultsIncrease of temperatures and PDSI had a positive effect on height growth for most of the study species, whereas Alaska yellow-cedar (Chamaecyparis nootkatensis, (D. Don) Spach) height growth declined with ED. All explaining variables and the interactions explained 59% of the total height growth variance. Although tree height growth response was species-specific, increased height growth during the 20th century was more pronounced for coastal ranged species, high shade tolerant species, and broadleaf species. Furthermore, height growth increase occurred mostly on rich soil, at the northernmost species range, and, unexpectedly, at lower elevations. A decline in height growth for some species further north and especially higher in elevation possibly related to increased cloudiness and precipitation. However, drought conditions remain in interior areas despite moving northward and upward that decrease height growth. ConclusionThese results highlight the general trend (species characteristics and range) and the species-specific height patterns, indicating the spatio-temporal complexity of the growth response to recent global climate change.


1989 ◽  
Vol 8 (2) ◽  
pp. 150-158 ◽  
Author(s):  
Ellis Yochelson

In 1893, Walcott contributed to the debate on the length of geologic time. He approached the problem by calculating average thickness of the Paleozoic rock column in the west and dividing by rates of erosion and by rates of deposition to arrive at a time interval. Although he concentrated on the Cordilleran area, Walcott produced a general paleogeographic scheme for the Paleozoic of North America. He was quite clear in differentiating between chemical and mechanical deposits, and devoted most of his attention to the Paleozoic carbonates. Walcott chose western North America as the source for data, in part because of the long sections and in part because of the large amount of limestone relative to sandstone and shale. Throughout the discussion he included pertinent comments on such subjects as size of source areas and relative speed of deposition; he was familiar with many of the issues that occupy present-day sedimentologists. After considering various aspects of the issue, Walcott estimated 17,500,000 years for the duration of the Paleozoic. Walcott also derived a Paleozoic: Mesozoic: Cenozoic ratio of 12: 5: 2, the same ratio obtained today from radiometric dates. He estimated that the Algonkian was as long as Paleozoic and guessed 10,000,000 years for the duration of the Archean. The greatest flaws in his chain of logic were assumption of an erosion rate of 1 foot in 200 years and assumption that deposition of limestone was more or less continuous. Had he chosen 1 foot per 3,000 years, one of his other two calculations, he would have been close to present-day age figures. Perhaps it was the episodic, rather than the average, nature of sedimentation that was the pitfall. Nevertheless, Walcott's estimates of thicknesses of western Paleozoic rocks and his resulting calculations were the most detailed made on erosion/sedimentation rates to indicate the length of geologic time. His study was published in three journals, plus other outlets, and it may have been the most widely distributed paper of the decade. It was little cited, perhaps because within several years the debate on age shifted to use of ocean salinity as a potentially more precise calender. That approach in turn ultimately succumbed to the new concept of radiometric dating.


2013 ◽  
Vol 40 (8) ◽  
pp. 1463-1474 ◽  
Author(s):  
Marc Kéry ◽  
Gurutzeta Guillera-Arroita ◽  
José J. Lahoz-Monfort

Ecography ◽  
2016 ◽  
Vol 40 (9) ◽  
pp. 1050-1066 ◽  
Author(s):  
Diana Stralberg ◽  
Steven M. Matsuoka ◽  
Colleen M. Handel ◽  
Fiona K. A. Schmiegelow ◽  
Andreas Hamann ◽  
...  

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