Rapid change in high-elevation precipitation patterns of western North America during the Middle Eocene Climatic Optimum (MECO)

2015 ◽  
Vol 315 (4) ◽  
pp. 317-336 ◽  
Author(s):  
A. Mulch ◽  
C. P. Chamberlain ◽  
M. A. Cosca ◽  
C. Teyssier ◽  
K. Methner ◽  
...  
2016 ◽  
Vol 450 ◽  
pp. 132-139 ◽  
Author(s):  
Katharina Methner ◽  
Andreas Mulch ◽  
Jens Fiebig ◽  
Ulrike Wacker ◽  
Axel Gerdes ◽  
...  

2011 ◽  
Vol 38 (11) ◽  
pp. n/a-n/a ◽  
Author(s):  
Brent B. Wolfe ◽  
Thomas W. D. Edwards ◽  
Roland I. Hall ◽  
John W. Johnston

1967 ◽  
Vol 6 (47) ◽  
pp. 737-748 ◽  
Author(s):  
V. R. McGregor

Young moraines and rock glaciers in the central part of the Ben Ohau Range, about 42 km. south of the highest peaks of the Southern Alps, are briefly described. A new formation, the Ben Ohau Formation, consisting of the Ferintosh, Jacks Stream and Dun Fiunary Members, is proposed for moraines and rock glaciers believed to have been built since the climatic optimum by three minor glacial advances. Moraines, and outwash and fan gravels, deposited during a more extensive pre-climatic optimum advance which was contemporaneous with the Cockburn Glacial Phase (Cochrane) in North America are assigned to the Birch Hill Formation. The sequence of glacial advances recorded in the Ben Ohau Range is compared with that found in western North America.


2019 ◽  
Vol 151 (04) ◽  
pp. 521-530 ◽  
Author(s):  
Vladimir N. Makarkin ◽  
S. Bruce Archibald ◽  
James E. Jepson

AbstractOne new genus of Inocelliidae (Raphidioptera) with one new species and one undetermined specimen is described from the Eocene of North America: Paraksenocellia borealis new genus, new species from the early Eocene (Ypresian) Okanagan Highlands shale at Driftwood Canyon, British Columbia, Canada (a forewing), and Paraksenocellia species from the middle Eocene (Lutetian) of the Coal Creek Member of the Kishenehn Formation, northwestern Montana, United States of America (a hind wing). These are the oldest records of the family. The new genus possesses many character states that are rare in Inocelliidae, e.g., a very long pterostigma extending to ScP in both the forewings and hind wings; the forewing subcostal space has three crossveins; the forewing and hind wing AA1 are deeply forked; the crossvein between CuA and CuP is located far distad the crossvein 1r-m. Paraksenocellia is confidently a member of the Inocelliidae, as it possesses a proximal shift of the basal crossvein 1r-m (connecting R and M) in the forewing and the loss of the basal crossvein 1r-m in the hind wing, both apomorphies of the family. It shares some character states with the Mesozoic Mesoraphidiidae, which we consider to be mostly stem-group plesiomorphies.


2020 ◽  
Vol 76 (2) ◽  
pp. 211-216
Author(s):  
Steven R. Manchester ◽  
Kory A. Disney ◽  
Kasey K. Pham

A new kind of fin-winged fruit is recognized from lacustrine shales of the early Eocene Tepee Trail Formation of northwestern Wyoming and from the middle Eocene Clarno Formation of central Oregon, USA. The fruits are obovate with five thick lateral wings, borne on a thick pedicel and bearing scars of hypogynous perianth and disk. The fruit surface is covered with small circular dots interpreted as glands. This combination of characters leads us to infer affinities with the Rutaceae, although no identical modern genus is known. We establish the new genus and species, Quinquala obovata.


2005 ◽  
Vol 83 (7) ◽  
pp. 1003-1011 ◽  
Author(s):  
M Kumala ◽  
D A McLennan ◽  
D R Brooks ◽  
A C Mason

The genus Cyphoderris, or hump-winged grigs, is represented by three species of cold-adapted, acoustic Ensifera with a geographic distribution that is generally restricted to the high-elevation coniferous forests of western North America. A phylogenetic analysis based on 29 morphological and 3 behavioural characters produced one tree, (C. buckelli (C. strepitans, C. monstrosa)) with a consistency index of 1.0. We discuss possible explanations for the observation that almost all of the autapomorphic change was concentrated in C. monstrosa.


1967 ◽  
Vol 6 (47) ◽  
pp. 737-748 ◽  
Author(s):  
V. R. McGregor

Young moraines and rock glaciers in the central part of the Ben Ohau Range, about 42 km. south of the highest peaks of the Southern Alps, are briefly described. A new formation, the Ben Ohau Formation, consisting of the Ferintosh, Jacks Stream and Dun Fiunary Members, is proposed for moraines and rock glaciers believed to have been built since the climatic optimum by three minor glacial advances. Moraines, and outwash and fan gravels, deposited during a more extensive pre-climatic optimum advance which was contemporaneous with the Cockburn Glacial Phase (Cochrane) in North America are assigned to the Birch Hill Formation. The sequence of glacial advances recorded in the Ben Ohau Range is compared with that found in western North America.


1998 ◽  
Vol 11 (12) ◽  
pp. 3095-3111 ◽  
Author(s):  
Michael D. Dettinger ◽  
Daniel R. Cayan ◽  
Henry F. Diaz ◽  
David M. Meko

Sign in / Sign up

Export Citation Format

Share Document