Contributions of the hippocampus and medial prefrontal cortex to energy and body weight regulation

The effects of selective ibotenate lesions of the complete hippocampus (CHip), the hippocampal ventral pole (VP), or the medial prefrontal cortex (mPFC) in male rats were assessed on several measures related to energy regulation (i.e., body weight gain, food intake, body adiposity, metabolic activity, general behavioral activity, conditioned appetitive responding). The testing conditions were designed to minimize the nonspecific debilitating effects of these surgeries on intake and body weight. Rats with CHip and VP lesions exhibited significantly greater weight gain and food intake compared with controls. Furthermore, CHip-lesioned rats, but not rats with VP lesions, showed elevated metabolic activity, general activity in the dark phase of the light-dark cycle, and greater conditioned appetitive behavior, compared with control rats without these brain lesions. In contrast, rats with mPFC lesions were not different from controls on any of these measures. These results indicate that hippocampal damage interferes with energy and body weight regulation, perhaps by disrupting higher-order learning and memory processes that contribute to the control of appetitive and consummatory behavior.     

Chimeric twins. T.S. and M.R. reexamined

A pair of chimeric twins, T.S. (male) and M.R. (female), were examined. The amounts of 'foreign' blood cells in each twin found on three occasions were compared. The percentages of M.R. cells found in the blood of T.S. in 1977 and in 1982 were similar and about 1/5 of that found in 1970. The amount of T.S.-blood cells found in M.R. was declining slowly from about 31% in 1970 to about 25% in 1982.     

Choroideremia: further evidence for assignment of the locus to Xq13–Xq21

Summary Choroideremia is an X-linked hereditary retinal dystrophy leading to blindness in early adulthood. RFLP analyses in three Danish families were consistent with close linkage between choroideremia and the locus DXYS1, located at Xq13–Xq21. Measurable linkage was found between choroideremia and DXS17, at Xq22. Furthermore, choroideremia was diagnosed in a boy with an interstitial deletion at Xq13–Xq21, strongly suggesting the assignment of the locus for choroideremia to this region of the X chromosome. The deletion also covered DXYS1, but did not include DXS17.     

Dicentric and monocentric Robertsonian translocations in man

Summary 5 balanced Robertsonian translocations in man were identified by fluorescence studies. Orcein staining showed two distinct centromeres in 4 of these cases (tdic(13;13), tdic(13;14), tdic(15;21), tdic(21;22)) indicating breaks in the short arms of the involved chromosomes. The dicentric translocation chromosomes were rather stable but monocentrics were noticed in each case. Fluorescence- and measurement studies seemed to indicate that an invisible centromere and part of the short arms were present in these monocentric chromosomes. One case, t(14q21q), was monocentric in all metaphase plates but measurement studies were very suggestive of a visible 21 centromere and incorporation of the invisible 14 centromere (and short arm material) in the long arm of the translocated 14 chromosome, indicating that this translocation originally might have been a real dicentric. Heterochromatin staining was carried out in all cases. The tdic(15;21) showed 6 heterochromatin blocks; 2 of these blocks were probably satellites from chromosome No. 21, visible too in fluorescence. The 4 other translocations showed 4 separated blocks. No differences were observed between monocentrics and dicentrics supporting the theory of a preserved, but invisible centromere in monocentrics.

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Zusammenfassung 5 balancierte humane Translokationen vom Robertson-Typ wurden durch Fluorescenzuntersuchungen identifiziert. Die Orceinfärbung zeigte in 4 dieser Fälle 2 distinkte Zentromere (tdic(13;13), tdic(13;14), tdic(15;21), tdic(21;22)). Dieser Fund ließ es als wahrscheinlich erscheinen, daß der Bruch am kurzen Arm der involvierten Chromosomen stattgefunden hatte. Die dizentrischen Translokationschromosomen waren verhältnismäßig stabil. Es wurden doch monozentrische Chromosomen in allen Fällen beobachtet. Eine Kombination von Fluorescenzuntersuchung und Messung der Chromosomen machte es wahrscheinlich, daß auch in diesen monozentrischen Chromosomen ein unsichtbares Zentromer und Teile der kurzen Arme vorhanden sind. Eine (14q21q)-Translokation hatte in allen Metaphasen nur ein Zentromer. Messungen jedoch deuteten an, daß das 21-Zentromer sichtbar war, daß aber das 14-Zentromer und Material der kurzen Arme am langen Arm des translozierten 14-Chromosoms inkorporiert waren. Das Translokationschromosom ist möglicherweise ursprünglich ein dizentrisches Chromosom gewesen. In allen Fällen wurde eine Heterochromatinfärbung ausgeführt. Die tdic(15;21) hatte 6 Heterochromatinblöcke. 2 davon waren wahrscheinlich die Satelliten des Chromosoms Nr. 21, die auch bei der Fluorescenzmikroskopie sichtbar waren. Die 4 anderen Translokationen hatten 4 separate Blöcke. Monozentrische und dizentrische Chromosomen zeigten hier keinen Unterschied, was die Theorie unterstützt, daß die Zentromere im monozentrischen Chromosomen erhalten, aber unsichtbar sind.

     

A familial translocation t(6q+;8q-) identified by fluorescence microscopy

Summary A balanced translocation t(6q+;8q-) was identified by fluorescence studies in a family with multiple spontaneous abortions. It is suggested that a zygote, monosomic for the long arm of chromosome No. 8 is not viable.

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Zusammenfassung Eine balancierte Translokation t(6q+;8q-) wurde durch Fluorescenzuntersuchungen in einer Familie mit mehreren spontanen Aborten nachgewiesen. Es wird betont, daß eine Zygote mit Monosomie des langen Armes vom Chromosom 8 nicht lebensfähig ist.

     

DXS26 (HU16) is located in Xq21.1

Summary We have localized a single-copy DNA probe, HU16 (locus DXS26), to Xq21.1. The probe was isolated from a human-mouse hybrid X;13 library and mapped with human-mouse hybrids containing different portions of the human X chromosome and DNA from male patients with different X-chromosomal deletions. The following order of loci is proposed: Xcen-(DXS72, DXS169)-(DXS232,DXS26)-DXS121-DXS233-DXS165 TCD-DXS95-DXYSl-Xqter. HU16 will be useful in the study of the putative genes that reside in Xq21 and whose defects lead to deafness and mental retardation.     

Facies pattern and sea-level dynamics of the early Late Cretaceous transgression: a case study from the lower Danubian Cretaceous Group (Bavaria,southern Germany)

The facies development and onlap pattern of the lower Danubian Cretaceous Group (Bavaria, southern Germany) have been evaluated based on detailed logging, subdivision, and correlation of four key sections using an integrated stratigraphic approach as well as litho-, bio-, and microfacies analyses. Contrary to statements in the literature, the transgressive onlap of the Regensburg Formation started in the Regensburg–Kelheim area already in the early Early Cenomanian Mantelliceras mantelli ammonite Zone and not in the Late Cenomanian. In the Early Cenomanian, nearshore glauconitic-bioclastic sandstones prevailed (Saal Member), followed by Middle to lower Upper Cenomanian mid-shelf siliceous carbonates intercalated with fine-sandy to silty marls (Bad Abbach Member). Starting in the mid-Late Cenomanian (Metoicoceras geslinianum ammonite Zone), a considerable deepening pulse during the Cenomanian–Turonian Boundary Event (CTBE) initiated the deposition of the deeper shelf silty marls of the Eibrunn Formation, which range into the early Early Turonian. During the CTBE transgression, also the proximal Bodenwöhrer Senke (ca. 40 km NE of Regensburg) was flooded, indicated by the onlap of the Regensburg Formation onto Variscan granites of the Bohemian Massif, overlain by a thin tongue of lowermost Turonian Eibrunn Formation. A detailed record of the positive δ¹³C excursion of the global Oceanic Anoxic Event (OAE) 2 has been retrieved from this shallow-water setting. An integrated approach of bio-, event-, carbon stable isotope and sequence stratigraphy was applied to correlate the sections and to decipher the dynamics of this overall transgressive depositional system. The Cenomanian successions show five prominent unconformities, which correlate with those being known from basins in Europe and elsewhere, indicating their eustatic origin. The rate of sea-level rise during the CTBE suggests glacio-eustasy as a driving mechanism for Late Cenomanian sea-level changes. The Regensburg and Eibrunn formations of the lower Danubian Cretaceous Group are highly diachronous lithostratigraphic units. Their regional distribution and northeast-directed onlap pattern onto the southwestern margin of the Bohemian Massif can readily be explained by the lateral movements of roughly coast-parallel (i.e., NW/SE-trending) facies belts of a graded shelf system transgressing on a northeastward-rising substrate. It took the Cenomanian coastline ca. 6 Ma to transgress from southwest of Regensburg to the topographically elevated granite cliffs southeast of Roding in the Bodenwöhrer Senke (=60 km distance).