scholarly journals Meiosis in Oenothera purpurata and Oe. blandina

This paper is a study of the essential stages of pollen meiosis in two Oenotheras which show seven pairs of chromosomes in diakinesis and the heterotypic metaphase. Its intention is to throw further light on the origin of the pairs and their relation to the method of synapsis. Although these forms agree in having seven pairs of chromosomes and no linkage ring, yet they show certain characteristic cytological differences, which will appear in the description. The problem of the origin of chromosome linkage or catenation (Gates, 1931), so characteristic of Oenothera, is also involved. Material and Methods . Oe. Purpurata was described by Klebahn (1925) from cultures derived from naturalised colonies of Oenothera on the Lunenburger Heide in North-western Germany. It is very much like Oe. Hookeri , but has small flowers. In crosses with Oe. Hookeri the smaller flowers of Oe. Purpurata are stated by Rudloff (1929, a ) to represent a monohybrid difference, the small flowers being dominant. By crossing it with various other forms, Rudloff found it to be homozygous, which he confirmed by showing that it had good pollen and seven free chromosome pairs in diakinesis.

PLoS ONE ◽  
2020 ◽  
Vol 15 (6) ◽  
pp. e0234044 ◽  
Author(s):  
J. Liebing ◽  
I. Völker ◽  
N. Curland ◽  
P. Wohlsein ◽  
W. Baumgärtner ◽  
...  

2012 ◽  
Vol 86 ◽  
pp. 138-149 ◽  
Author(s):  
C. Münsterer ◽  
J. Fohlmeister ◽  
M. Christl ◽  
A. Schröder-Ritzrau ◽  
V. Alfimov ◽  
...  

1997 ◽  
Vol 43 (145) ◽  
pp. 495-502 ◽  
Author(s):  
Jan A. Piotrowski ◽  
Anna M. Kraus

AbstractLaboratory tests on sediment over-ridden by the last ice sheet in north-western Germany reveal very low ice-induced pre-consolidation and high palaeo-pore-water pressures. Sediment consolidation at the base of the glacier was largely controlled by hydraulic properties of the substratum. Generally low permeabilities of the bed caused sustained high pore-water pressure in over-ridden sediments close to the flotation point. This implies a serious possibility of hydraulic lifting of the ice sheet. It is believed that the reduced basal coupling limited the transformation of glacier shear stress on to the bed sediments, which is indicated by a lack of sedimentological evidence for widespread pervasive bed deformation. Ice motion was probably focused at the glacier sole by some combination of sliding and ploughing. However, isolated spots with deformation occur, so that the subglacial system in the study area can be characterized as a stable/deforming mosaic.


1994 ◽  
Vol 12 (2) ◽  
pp. 137-179 ◽  
Author(s):  
S. Brakensiek

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