scholarly journals Occurrence, biology and harmfulness of Galerucella lineola (F.) (Coleoptera, Chrysomelidae) – Part 2. Larvae and this year’s beetles

2008 ◽  
Vol 53 (No. 9) ◽  
pp. 424-444
Author(s):  
J. Urban

The second part of the paper deals with the development and harmfulness of larvae and maturation feeding of this year’s beetles of <I>Galerucella lineola</I> (F.) before leaving for winter habitats. Embryogenesis takes on average 12 (in the laboratory 9) days. In the area of Žďár situated at a higher and colder location, larvae of the alder biological form occur on <I>Alnus glutinosa</I> and <I>A. incana</I> from June to August. In the warmer lowland area of Brno, larvae of the willow form occur on <i>Salix triandra, S. viminali</I>s and <I>S. caprea</I> from the 3<sup>rd</sup> decade of May to the beginning of August. In the laboratory, larvae of the alder form developed on average 16 days and larvae of the willow form 13 days. Larvae of the alder form damage on average 9.7 cm<sup>2</sup> leaves of <I>A. glutinosa</I> and larvae of the willow form 6.0 cm<sup>2</sup> leaves of <I>Salix caprea</I>. This year’s imagoes occur in the area of Žďár on alders from mid-July to the end of October and during 3 weeks, they damage on average 16 cm<sup>2</sup> leaves of <I>A. glutinosa</I>. This year’s imagoes occur on willows in the area of Brno from the end of June to the end of August. During 2 weeks, they damage on average 12 cm<sup>2</sup> leaves of <i>S. caprea</I>. The chrysomelid development is univoltine (in southern parts of Moravia partly bivoltine). The alder biological form of <I>G. lineol</I>a produced 2 (the willow form even 4) incomplete generations in the laboratory. This year’s imagoes damaged on average 36.6 cm<sup>2</sup> of <I>S. caprea</I> and laid 122 to 887 (on average 528) eggs. In the area of Brno, imagoes of the willow form were up to 65% parasitized by <I>Medina collaris</I> (Fall.) (Tachinidae).Tachinidae).

Biologia ◽  
2008 ◽  
Vol 63 (2) ◽  
Author(s):  
Jan Frouz

AbstractField microcosms consisting of mineral soil (spoil substrate) and two types of litter taken either from an unreclaimed site with spontaneously developed vegetation (mostly Salix caprea) or from an alder plantation (a mixture of Alnus glutinosa and A. incana) were exposed in spontaneously developed or reclaimed sites at a post-mining heap near Sokolov (Czech Republic) for one year. The litter types differed remarkably in C:N ratio which was 29 for spontaneous litter and 14 for alder litter. The two microcosm types were either accessible or not accessible to soil macrofauna. The effect of macrofauna exclusion on soil mixing was complex and depended on litter quality and the site that determined soil fauna composition. In reclaimed sites where macrofauna was dominated by saprophags, mainly earthworms, the macrofauna access increased soil mixing. In sites where predators dominated, the macrofauna exclusion probably suppressed fragmentation and mixing activity of the mesofauna.


Forests ◽  
2019 ◽  
Vol 10 (11) ◽  
pp. 939 ◽  
Author(s):  
Alexandra Špaldoňová ◽  
Jan Frouz

To explore the question how litter and macrofauna feces respond to temperature and how respiration differs for litter with a different CN ratio, we compared the decomposition rates of leaf litter (Alnus glutinosa, Salix caprea, and Acer campestre) and isopod (Armadillidium vulgare) feces produced from the same litter in response to three constant (8, 16, and 24 °C) and one fluctuating (first week 8 °C, the other week 24 °C) temperatures in a 50 week laboratory experiment and in a field trial. Microbial respiration of litter with lower CN ratio (alder and willow) was significantly higher than respiration of feces, no significant difference was found for maple litter with higher CN ratio. This was supported by field litter bag experiments where alder and willow litter decomposed faster than feces but the opposite was true for maple litter. Litter respiration was significantly affected by temperature but feces respiration was not. Fluctuating temperature caused either lower or equal respiration as compared to mean constant temperature. The content of phenolics was significantly higher in intact litter in comparison with decomposed litter and feces, either fresh or decomposed. The CN ratio decreased as litter turned to feces in maple and alder litter but increased in willow litter. In conclusion, microbial respiration of both litter and feces were substantially affected by litter quality; the litter was more sensitive to temperature than feces.


2008 ◽  
Vol 53 (No. 8) ◽  
pp. 364-380
Author(s):  
J. Urban

In Moravia in 1995 to 2006, the abundant occurrence of <i>Galerucella lineola</i> (F.) was used to study its occurrence, biology and harmfulness. An “alder” biological form was studied in <i>Alnus glutinosa</i> and <i>A. incana</i> mainly in Polnička Forest District (Žďár region) and a “willow” form in <i>Salix viminalis</i>, <i>S. triandra</i> and <i>S. caprea</i> in riparian and accompanying stands of the Svitava river near Bílovice nad Svitavou (Brno region). Imagoes leave their sites usually in the 1st half of May. In the course of 2.5 to 3 months, they damage on average 22.6 cm<sup>2</sup> leaves of <i>A. glutinosa</i> and <i>S. caprea</i> (of this value, males 3.2 times less than females). Males eat on average 15 times during 24 hours for a period of 3.5 minutes, i.e. in total 52 minutes (3.6% day). Females eat on average 36 times for a period of 7 min, i.e. 252 min (17.5% day). Imagoes copulate on average 10.2 times per day for a period of 67 min. For the whole period of reproduction (about 42 days), they copulate on average 428 times, i.e. for 20 days. Eggs are laid into groups of 3 to 20 (on average 14) pieces. Females lay 457 to 791 (on average 612) eggs, i.e. about 15 eggs per day. <i>Medina collaris</i> (Fall.) (Tachinidae) and <i>Townesilitus fulviceps</i> (Ruthe) (Braconidae) belong, among others, to the enemies of imagoes.


2014 ◽  
Author(s):  
Luke Miller ◽  
Burcu A. Urgen ◽  
Maria Florendo ◽  
Jennifer Cook ◽  
Ayse P. Saygin

1999 ◽  
Vol 64 ◽  
Author(s):  
D. Van den Meersschaut ◽  
B. De Cuyper ◽  
K. Vandekerkhove ◽  
N. Lust

Natural  stand changes in the forest reserve of Liedekerke were analysed during the  period    1986-1996, using a permanent grid of circular plots. The monitoring  concentrated on natural    changes in species composition, using stem number and basal area as  indicators, and changes    in spatial distribution and colonization capacities of trees and shrubs,  with special interest in the    competition between exotic and indigenous species. After only a decade of  monitoring important    natural changes in the woody layer were detected. The pioneer forest is  gradually maturing    through self-thinning processes and shifts in species composition. The  overall stem number    decreased with 33.6%, while the basal area increased with 20.9%. Birch (Betula pendula/    pubescens) and indigenous oak (Quercus robur/petraea) remained  dominant. More tolerant    exotic species, like red oak (Quercus rubra) and sweet chestnut (Castanea  sativa), are slowly    increasing their share in the species composition and expanding their  range. Pioneer species on    the other hand, like aspen (Populus tremula), willow (Salix  capreaicinerealaurita), alder buckthorn    (Frangula alnus) and  common (Alnus glutinosa)  and grey alder (A. incana),  strongly declined.    Black cherry (Prunus serotina) seems to be slowly invading the forest due to its  massive    natural regeneration. Strong competition may be expected especially from  rowan ash (Sorbus    aucuparia), which showed similar regeneration  and colonization capacities. Elder (Sambucus    nigra) dramatically extented its range, though  its share remains marginal. Beech remained absent    most probably due to the lack of mature trees in the vacinity of the  forest. Finally this    change detection allowed that general predictions could be made on the  future natural development    and composition of this forest reserve, which could serve forest management  decisions.


1968 ◽  
Vol 5 (6) ◽  
pp. 1401-1407 ◽  
Author(s):  
Ronald Doig ◽  
Jackson M. Barton Jr.

Potassium-argon ages have been determined for alkaline rocks, including carbonatites, from some fifteen localities in Quebec. Nine centers of intrusion, including two previously documented localities, yield ages in the range 400 to 600 million years. All but two of these are located on or very near the northern boundary fault of the St. Lawrence graben system. Included in this group are four carbonatites with remarkably similar ages of intrusion (565 m.y.). The existence of this widespread coeval igneous activity along a 1200-mile segment of the lowland area and its westward extension supports the hypothesis that the St. Lawrence graben is a continuous structure, and indicates that the system has been active for at least 600 million years.


Author(s):  
A P Glinushkin ◽  
E M Motasova ◽  
T P Aysuvakova ◽  
A V Ovsiankina ◽  
N S Zhemchuzhina ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document