Evolution of Castanea in North America: restriction‐site‐associated DNA sequencing and ecological modeling reveal a history of radiation, range shifts, and disease

2021 ◽  
Author(s):  
Elizabeth L. Spriggs ◽  
Matthew E. Fertakos
Keyword(s):  
North America ◽  
Dna Sequencing ◽  
Restriction Site ◽  
Ecological Modeling ◽  
Range Shifts ◽  
History Of

GEOGRAPHIC DISTRIBUTION AND BIOGEOGRAPHY OF REPRESENTATIVE SPECIES OF XERIC GRASSLAND-ADAPTED NEARCTIC LYGAEIDAE IN WESTERN NORTH AMERICA (INSECTA: HETEROPTERA)

1993 ◽  
Vol 125 (S165) ◽  
pp. 75-113 ◽  
Author(s):  
G.G.E. Scudder
Keyword(s):  
North America ◽  
Geographic Distribution ◽  
Restriction Site ◽  
Sequence Data ◽  
The North ◽  
Representative Species ◽  
History Of ◽  
Dna Restriction ◽  
Present Distribution ◽  
Late Wisconsinan

AbstractThis paper outlines the known distribution of eight xeric grassland-adapted species of Lygaeidae, and examines these distributions with respect to the glacial history of North America during the Pleistocene, and past and present distribution of grassland vegetation. Four of these species (Neosuris castanea, Sisamnes claviger, Ligyrocoris latimarginatus, and Melanopleurus perplexus) probably survived the Pleistocene in refugia south of the Late Wisconsinan ice sheet. Differences in climatic requirements may explain the variations in geographic distribution exhibited by these four insects and a methodology for testing this is discussed. The four other species (Crophius ramosus, Kolenetrus plenus, Slaterobius insignis, and Emblethis vicarius) may have occurred in the north prior to 1.2 mya and survived the Late Pleistocene in both the northern Beringian refugium and in southern refugia. Molecular systematics, especially use of DNA restriction site or sequence data, might provide the evidence needed to test historical biogeographic postulates based on the extant distribution of these species.

scholarly journals The population structure and recent colonization history of Oregon threespine stickleback determined using restriction-site associated DNA-sequencing

2013 ◽  
Vol 22 (11) ◽  
pp. 2864-2883 ◽  
Author(s):  
Julian Catchen ◽  
Susan Bassham ◽  
Taylor Wilson ◽  
Mark Currey ◽  
Conor O'Brien ◽  
...  
Keyword(s):  
Population Structure ◽  
Dna Sequencing ◽  
Restriction Site ◽  
Threespine Stickleback ◽  
Colonization History ◽  
History Of

A brief history of (DNA sequencing) time

2007 ◽  
Vol 8 (S1) ◽  
pp. S21-S21
Author(s):  
Elaine R. Mardis
Keyword(s):  
Dna Sequencing ◽  
History Of

Identity of the oribatid mite Oribata curva and transfer to Trichogalumna (Acari, Oribatida, Galumnidae), with discussion of nomenclatural and biogeographical issues in the ‘curva’ species-group

Zootaxa ◽  
2017 ◽  
Vol 4272 (4) ◽  
pp. 551
Author(s):  
ROY A. NORTON ◽  
SERGEY G. ERMILOV
Keyword(s):  
North America ◽  
Oribatid Mite ◽  
Species Group ◽  
Type Material ◽  
Similar Species ◽  
History Of ◽  
Molecular Assessment

Based on the study of type material, other historical specimens, and new collections, the adult of the thelytokous oribatid mite Oribata curva Ewing, 1907 (Galumnidae) is redescribed and the name is recombined to Trichogalumna curva (Ewing, 1907) comb. nov. A confusing history of synonymies and misidentifications is traced in detail, and their effect on published statements about biogeography is assessed. Reliable records of T. curva are only those from North America. The tropical mite Pergalumna ventralis (Willmann, 1932) is not a subspecies of T. curva. The widely-reported Trichogalumna nipponica (Aoki, 1966) and other similar species form a complex with T. curva that needs further morphological and molecular assessment. 

scholarly journals I.—History of the Names Cambrian and Silurian in Geology

1873 ◽  
Vol 10 (111) ◽  
pp. 385-395 ◽  
Author(s):  
T. Sterry Hunt
Keyword(s):  
Great Britain ◽  
North America ◽  
Upper Cambrian ◽  
History Of ◽  
Lower Palaeozoic ◽  
The Subject

It is proposed in the following pages to give a concise account of the progress of investigation of the lower Palæozoic rocks during the last forty years. The subject may naturally be divided into three parts: 1. The history of Silurian and Upper Cambrian in Great Britain from 1831 to 1854; 2. That of the still more ancient Palæozoic rocks in Scandinavia, Bohemia, and Great Britain up to the present time, including the recognition by Barrande of the so-called primordial Palæozoic; fauna; 3. The history of the lower Palæozoic rocks of North America.

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