scholarly journals Punctuated invasion of water, ice, snow and terrestrial ecozones by segmented worms (Oligochaeta: Enchytraeidae: Mesenchytraeus )

2017 ◽  
Vol 284 (1864) ◽  
pp. 20171081 ◽  
Author(s):  
Shirley A. Lang ◽  
Naim Saglam ◽  
Joseph Kawash ◽  
Daniel H. Shain

Segmented worms (Annelida) are among the most successful animal inhabitants of extreme environments worldwide. An unusual group of enchytraeid oligochaetes of genus Mesenchytraeus are abundant in the Pacific northwestern region of North America and occupy geographically proximal ecozones ranging from low elevation rainforests and waterways to high altitude glaciers. Along this altitudinal transect, Mesenchytraeus representatives from disparate habitat types were collected and subjected to deep mitochondrial and nuclear phylogenetic analyses. Our data identify significant topological discordance among gene trees, and near equivalent interspecific divergence levels indicative of a rapid radiation event. Collectively, our results identify a Mesenchytraeus ‘explosion’ coincident with mountain building in the Pacific northwestern region that gave rise to closely related aquatic, ice, snow and terrestrial worms.

2019 ◽  
Vol 191 (1) ◽  
pp. 18-29 ◽  
Author(s):  
Linling Zhong ◽  
Huanhuan Liu ◽  
Dafu Ru ◽  
Huan Hu ◽  
Quanjun Hu

Abstract Radiation rather than bifurcating divergence has been inferred through a number of phylogenetic analyses using different DNA fragments. However, such inferences have rarely been tested by examining alternative hypotheses based on population genomic data. In this study, we sequenced the transcriptomes of 32 individuals from 13 populations of four Orychophragmus spp. (Brassicaceae) to investigate their divergence history. Cluster and population structure analyses recovered four distinct genetic clusters without any genetic mixture. Most orthologous genes produced unresolved bifurcating interspecific relationships with a star phylogeny. The resolved gene trees were highly inconsistent with each another in reconstructing interspecific relationships. Population genomic analyses suggested unexpectedly high genetic divergence and a lack of gene flow between the four species. We examined radiation vs. bifurcating divergence between these four species based on coalescent modelling tests of population genomic data. Our statistical tests supported a radiation of these species from a common ancestor at almost the same time, rejecting stepwise bifurcating interspecific divergence with time. This nearly simultaneous radiation was dated to the Quaternary, during which climate changes are suggested to have promoted species diversity in eastern Asia. Our results highlight the importance of population genomic data and statistical tests in deciphering interspecific relationships and tracing the divergence histories of closely related species.


2005 ◽  
Vol 83 (9) ◽  
pp. 1206-1213 ◽  
Author(s):  
Paula L Hartzell ◽  
Jefferson V Nghiem ◽  
Kristina J Richio ◽  
Daniel H Shain

Glacier ice worms, Mesenchytraeus solifugus (Emery, 1898) and Mesenchytraeus solifugus rainierensis Welch, 1916 (Enchytraeidae), are the only known oligochaetes adapted to life in ice. We have collected ice worm specimens from over 100 populations throughout the Pacific northwestern region of North America. Their current range extends ~2500 km along the Pacific coastline between south-central Alaska and central Oregon, with most populations occurring on relatively low-elevation, temperate glaciers. Phylogenetic analyses utilizing partial nuclear 28S rDNA and mitochondrial cytochrome c oxidase subunit I (COI) loci revealed the presence of two geographically distinct clades (northern and southern). The northern clade comprises all Alaskan populations, while the southern clade contains British Columbia, Washington State, and Oregon State populations. No evidence of gene flow was detected between these two lineages or between noncontiguous glaciers throughout their geographic range. Our results suggest that the mechanism of ice worm dispersal is primarily active, though at least one episode of passive dispersal is noted at the southern extent of their range.


2006 ◽  
Author(s):  
J.K. Madsen ◽  
D.J. Thorkelson ◽  
R.M. Friedman ◽  
D.D. Marshall

Geosphere, February 2006, v. 2, p. 11-34, doi: 10.1130/GES00020.1. Movie 1 - Tectonic model for the Pacific Basin and northwestern North America from 53 Ma to 39 Ma. The file size is 1.3 MB.


2021 ◽  
Vol 95 ◽  
Author(s):  
B. Neov ◽  
G.P. Vasileva ◽  
G. Radoslavov ◽  
P. Hristov ◽  
D.T.J. Littlewood ◽  
...  

Abstract The aim of the study is to test a hypothesis for the phylogenetic relationships among mammalian hymenolepidid tapeworms, based on partial (D1–D3) nuclear 28S ribosomal RNA (rRNA) genes, by estimating new molecular phylogenies for the group based on partial mitochondrial cytochrome c oxidase I (COI) and nuclear 18S rRNA genes, as well as a combined analysis using all three genes. New sequences of COI and 18S rRNA genes were obtained for Coronacanthus integrus, C. magnihamatus, C. omissus, C. vassilevi, Ditestolepis diaphana, Lineolepis scutigera, Spasskylepis ovaluteri, Staphylocystis tiara, S. furcata, S. uncinata, Vaucherilepis trichophorus and Neoskrjabinolepis sp. The phylogenetic analyses confirmed the major clades identified by Haukisalmi et al. (Zoologica Scripta 39: 631–641, 2010): Ditestolepis clade, Hymenolepis clade, Rodentolepis clade and Arostrilepis clade. While the Ditestolepis clade is associated with soricids, the structure of the other three clades suggests multiple evolutionary events of host switching between shrews and rodents. Two of the present analyses (18S rRNA and COI genes) show that the basal relationships of the four mammalian clades are branching at the same polytomy with several hymenolepidids from birds (both terrestrial and aquatic). This may indicate a rapid radiation of the group, with multiple events of colonizations of mammalian hosts by avian parasites.


2004 ◽  
Vol 5 (1) ◽  
pp. 16
Author(s):  
Dean A. Glawe

Chinese matrimony-vine (Lycium chinense Mill.) is a traditional medicinal plant grown in China and used as a perennial landscape plant in North America. This report documents the presence of powdery mildew on L. chinense in the Pacific Northwest and describes and illustrates morphological features of the causal agent. It appears to be the first report of a powdery mildew caused by Arthrocladiella in the Pacific Northwest. Accepted for publication 10 November 2004. Published 8 December 2004.


2009 ◽  
Vol 24 (6) ◽  
pp. 1732-1747 ◽  
Author(s):  
Alain Roberge ◽  
John R. Gyakum ◽  
Eyad H. Atallah

Abstract Significant cool season precipitation along the western coast of North America is often associated with intense water vapor transport (IWVT) from the Pacific Ocean during favorable synoptic-scale flow regimes. These relatively narrow and intense regions of water vapor transport can originate in either the tropical or subtropical oceans, and sometimes have been referred to as Pineapple Express events in previous literature when originating near Hawaii. However, the focus of this paper will be on diagnosing the synoptic-scale signatures of all significant water vapor transport events associated with poleward moisture transport impacting the western coast of Canada, regardless of the exact points of origin of the associated atmospheric river. A trajectory analysis is used to partition the events as a means of creating coherent and meaningful synoptic-scale composites. The results indicate that these IWVT events can be clustered by the general area of origin of the majority of the saturated parcels impacting British Columbia and the Yukon Territories. IWVT events associated with more zonal trajectories are characterized by a strong and mature Aleutian low, whereas IWVT events associated with more meridional trajectories are often characterized by an anticyclone situated along the California or Oregon coastline, and a relatively mature poleward-traveling cyclone, commonly originating in the central North Pacific.


1995 ◽  
Vol 11 (1) ◽  
pp. 1-18 ◽  
Author(s):  
Brian F. Atwater ◽  
Alan R. Nelson ◽  
John J. Clague ◽  
Gary A. Carver ◽  
David K. Yamaguchi ◽  
...  

Earthquakes in the past few thousand years have left signs of land-level change, tsunamis, and shaking along the Pacific coast at the Cascadia subduction zone. Sudden lowering of land accounts for many of the buried marsh and forest soils at estuaries between southern British Columbia and northern California. Sand layers on some of these soils imply that tsunamis were triggered by some of the events that lowered the land. Liquefaction features show that inland shaking accompanied sudden coastal subsidence at the Washington-Oregon border about 300 years ago. The combined evidence for subsidence, tsunamis, and shaking shows that earthquakes of magnitude 8 or larger have occurred on the boundary between the overriding North America plate and the downgoing Juan de Fuca and Gorda plates. Intervals between the earthquakes are poorly known because of uncertainties about the number and ages of the earthquakes. Current estimates for individual intervals at specific coastal sites range from a few centuries to about one thousand years.


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