Documentation, profile descriptions and analytical results of loes profiles from Bavaria, southern Germany

This study investigates the landscape evolution and soil development in the loess area near Regensburg between approximately 6000-2000 yr BP (radiocarbon years), Eastern Bavaria. The focus is on the question how man and climate influenced landscape evolution and what their relative significance was. The theoretical background concerning the factors that controlled prehistoric soil erosion in Middle Europe is summarized with respect to rainfall intensity and distribution, pedogenesis, Pleistocene relief, and prehistoric farming. Colluvial deposits , flood loams, and soils were studied at ten different and representative sites that served as archives of their respective palaeoenvironments. Geomorphological, sedimentological, and pedological methods were applied. According to the findings presented here, there was a high asynchronity of landscape evolution in the investigation area, which was due to prehistoric land-use patterns. Prehistoric land use and settlement caused highly difIerenciated phases of morphodynamic activity and stability in time and space. These are documented at the single catenas ofeach site. In general, Pleistocene relief was substantially lowered. At the same time smaller landforms such as dells and minor asymmetric valleys filled up and strongly transformed. However, there were short phases at many sites, forming short lived linear erosion features ('Runsen'), resulting from exceptional rainfalls. These forms are results of single events without showing regional trends. Generally, the onset of the sedimentation of colluvial deposits took place much earlier (usually 3500 yr BP (radiocarbon) and younger) than the formation of flood loams. Thus, the deposition of flood loams in the Kleine Laaber river valley started mainly as a consequence of iron age farming only at around 2500 yr BP (radiocarbon). A cascade system explains the different ages of colluvial deposits and flood loams: as a result of prehistoric land use, dells and other minor Pleistocene landforms were filled with colluvial sediments. After the filling of these primary sediment traps , eroded material was transported into flood plains, thus forming flood loams. But at the moment we cannot quantify the extent ofprehistoric soil erosion in the investigation area. The three factors that controlled the prehistoric Iandscapc evolution in the Ioess area near Regensburg are as follows: 1. The transformation from a natural to a prehistoric cultural landscape was the most important factor: A landscape with stable relief was changed into a highly morphodynamic one with soil erosion as the dominant process of this change. 2. The sediment traps of the pre-anthropogenic relief determined where the material originated from soil erosion was deposited: either sedimentation took place on the slopes or the filled sediment traps of the slopes rendered flood loam formation possible. Climatic influence of any importance can only be documented as the result of land use in connection with singular and/or statistic events of heavy rainfalls. Without human impact, no significant change in the Holocene landscape would have been possible.

Silva Fennica Vol. 1 (121). 1967.

Julkaistu Silva Fennica Vol. 2(1) -numeron liitteenä.

On the toxicity of some pesticides for fish [Translation from: Izv.gos.nauchno-issled.Inst.ozern.rybn.Khoz. 121, 95-96, 1977]

In the piscicide laboratory of GosNIORKh over a series of years was carried out the ichthyological evaluation of different agricultural pesticides, used both in our country and abroad. In all more than 300 different chemical substances were tested. Here, it was established that around 10% of them possessed high ichthyotoxic properties. Experiments were conducted under laboratory conditions on aquarium fish in groups, and also on representatives of different species of lake ichthyofauna. The basic criterion of evaluation of toxicity was the death of experimental fish during 120 hours. This short paper summarises the findings of this reasearch and offers a table presenting acute toxicity of pesticides for fish.

>~（121）C核高自旋态在束γ研究和BGC晶体球性能测定

本文描述了在束γ谱学实验方法，并用这种方法研究了~（121）Cs核的高自旋态能级结构，观测到了~（121）Cs核中基于9/2~+质子空穴态上的△J = 1 的带和基于11/2~-准质子带，并在这两个带上鉴定出了四条新能级及六条新的γ跃迁。对这一结果进行了分析讨论。本文还讨论了一个小型BGO晶体球性能的测试方法，并给出了测试结果

Le vieux caporal : drame en cinq actes. [suivi de] Diane de lys et de camélias, ou La femme du monde légère, liée à un homme bilieux qui n'entend pas la plaisanterie : grande parodie en 3 petits tableaux. Livr. 121 / par MM. Dumanoir et d'Ennery ; par MM. Delacour et Lambert Thiboust

Collection : Théâtre contemporain illustré ; 121e et 122e livraisons

Livre des Morts de Nésyménou. Egyptien 121

Fragment 3 :Col. 1 + vignette : chapitre 28 (formule pour empêcher qu'on ne retire son coeur au défunt). La vignette montre le coeur du défunt et une divinité assise sur une maison.Col. 2 + vignette : chapitre 30B (formule pour empêcher que s'oppose le coeur du défunt). La vignette représente un scarabée.Col. 3 + vignette : chapitre 31 (formule pour repousser un crocodile venu pour enlever la magie-hékaou du défunt).Fragment 1 : la vignette montre le défunt armé d'une pique, qui devait probablement transpercer un animal néfaste.Fragment 2 :Col. 1 + vignette : chapitre 32 (formule pour repousser un crocodile venu pour enlever la magie-hékaou d'un Bienheureux de son contrôle dans la nécropole). La vignette montre deux crocodiles qui devaient être transpercés par le défunt.Col. 2 + vignette : chapitre 33 (formule pour repousser un serpent). La vignette montre le défunt transperçant un insecte (on attendrait un serpent).Col. 3 + vignette : chapitre 37 (formule pour repousser les deux amies). La vignette montre le défunt transperçant un serpent enroulé.Col. 4 + vignette (très fragmentaires) : ?