Directed differentiation and functional maturation of cortical interneurons from human embryonic stem cells

Human pluripotent stem cells are a powerful tool for modeling brain development and disease. The human cortex is composed of two major neuronal populations: projection neurons and local interneurons. Cortical interneurons comprise a diverse class of cell types expressing the neurotransmitter GABA. Dysfunction of cortical interneurons has been implicated in neuropsychiatric diseases, including schizophrenia, autism, and epilepsy. Here, we demonstrate the highly efficient derivation of human cortical interneurons in an NKX2.1::GFP human embryonic stem cell reporter line. Manipulating the timing of SHH activation yields three distinct GFP+ populations with specific transcriptional profiles, neurotransmitter phenotypes, and migratory behaviors. Further differentiation in a murine cortical environment yields parvalbumin- and somatostatin-expressing neurons that exhibit synaptic inputs and electrophysiological properties of cortical interneurons. Our study defines the signals sufficient for modeling human ventral forebrain development in vitro and lays the foundation for studying cortical interneuron involvement in human disease pathology.

Asymmetric cyclopropanation of olefins catalysed by Cu(I) complexes of chiral pyridine-containing macrocyclic ligands (Pc-L*)

The synthesis and characterisation of copper(I) complexes of chiral pyridine-containing macrocyclic ligands (Pc-L*) and their use as catalysts in asymmetric cyclopropanation reactions are reported. All ligands and metal complexes were fully characterised, including crystal structures of some species determined by X-ray diffraction on single crystals. This allowed characterising the very different conformations of the macrocycles which could be induced by different substituents or by metal complexation. The strategy adopted for the ligand synthesis is very flexible allowing several structural modifications. A small library of macrocyclic ligands possessing the same donor properties but with either C-1 or C-2 symmetry was synthesized. Cyclopropane products with both aromatic and aliphatic olefins were obtained in good yields and enantiomeric excesses up to 99%.

Editorial: The Demands of Protection, Preservation,and Permanency: Where Has Family Preservation Gone?

This Journal issue provides three important articles that will aid us in explaining what we do in service to families. We are very pleased to have the opportunity to print a major address delivered by William Meezan on "Translating Rhetoric to Reality: The Future of Family and Children's Services." The challenges of serving families under an evolution of models in Kansas is presented in "Family Preservation Services Under Managed Care: Current Practices and Future Directions" by Melanie Pheatt, Becky Douglas, Lori Wilson, Jody Brook, and Marianne Berry. What people doing the work think is addressed by the piece titled, "Perceptions of Family Preservation Practitioners: A Preliminary Study" by Judith Hilbert, Alvin L. Sallee, and James K. Ott. Finally, this issue presents a number of very interesting reviews of new resources.

Family Preservation Services under Managed Care: Current Practices and Future Directions

Family preservation service agencies in the State of Kansas have undergone major changes since the implementation of a managed care model of service delivery in 1996. This qualitative study examines the successes and barriers experienced by agency directors in utilization of a managed care system. Outcome/ performance measures utilized by the State of Kansas are reviewed, and contributing factors to the successes and limitations of the program are discussed. Included in these reviews is an analysis and presentation of literature and research which has been used as support for the current program structure. Recommendations for further evolution of practice are proposed.

Family Preservation Journal, 2000, Volume 5, Issue 1. (Entire issue)

Entire issue (large pdf file) Articles include: Translating Rhetoric to Reality: The Future of Family and Children's Services. William Meezan Family Preservation Services under Managed Care: Current Practices and Future Directions. Melanie Pheatt, Becky Douglas, Lori Wilson, Jody Brook, and Marianne Berry Perceptions of Family Preservation Practitioners: A Preliminary Study Judith C. Hilbert, Alvin Sallee, and James K. Ott

Human placental lactogen enhancer: Tissue specificity and binding with specific proteins

Human placental lactogen (hPL) is a 22,000 dalton protein hormone produced in the placenta. The physiological actions of hPL are not well understood but its major activity is to regulate both maternal and fetal metabolism. hPL stimulates maternal lipolysis increasing free fatty acids in the maternal blood, allowing their use as an energy source by the mother, and sparing glucose for the fetus. It may also act as a growth promoting hormone for the fetus. hPL is produced in increasing amounts as pregnancy progresses. At term, hPL accounts for 10% of protein and 5% of total RNA in the placenta. This high level of hPL production is tissue-specific, as hPL is only produced in the placenta by syncytiotrophoblast cells.^ The objective of this work was to understand the mechanism by which such high levels of hPL are produced in a tissue-specific manner. A transcriptional enhancer found 2.2 kb 3$\sp\prime$ to one of the hPL genes (hPL$\sb3$) may explain the regulation of hPL expression. Transient transfection experiments using the hPL-producing human choriocarcinoma cell line JEG-3 localized the hPL enhancer to a 138 bp core element. This 138 bp sequence was found to be tissue specific in its actions as it did not promote transcription in heterologous cell lines. Gel mobility shift assays showed the hPL enhancer interacts specifically with nuclear proteins unique to hPL-producing cells. Within the 138 bp enhancer a 22 bp region was shown to be protected from DNase I digestion due to binding of proteins derived from placental nuclear extracts. Proteins binding this region of the enhancer may be instrumental in the tissue specific activity of the hPL enhancer. ^

THE MECHANISM OF RETINOIC ACID REGULATION OF TISSUE TRANSGLUTAMINASE GENE EXPRESSION

Retinoic acid regulates cellular growth and differentiation by altering the expression of specific sets of genes, but the molecular mechanism by which this is achieved is unknown. We have used the rapid induction of a specific enzyme, tissue transglutaminase in mouse macrophages, human leukemia cells and a variety of other cell types to study the regulation of gene expression by retinoic acid. Soluble retinoic acid binding proteins, such as cellular Retinoic Acid Binding Protein (cRABP), have been proposed as specific mediators of retinoic acid regulation of gene expression. This thesis demonstrates the lack of cRABP in a number of cell lines which are sensitive to retinoic acid regulation of tissue transglutaminase expression. These cells are also devoid of other soluble retinoic acid binding activity. The level of retinoic acid binding activity that could have been detected (6 fmol) is far below that of most cells and tissues which are sensitive to the effects of retinoic acid on growth and differentiation. A mouse melanoma cell line, S91-C2, was found to contain an unusual retinoic acid binding protein which has a lower affinity for retinoic acid than mouse tissue cRABP and also behaves differently on gel filtration HPLC chromatography.^ The induction of tissue transglutaminase by retinoic acid in macrophages is specifically inhibited by pertussis toxin. Pertussis toxin ADP-riblosylates membrane GTP-binding proteins such as N(,i) and interferes with signalling from plasma membrane receptors to regulatory enzymes. Pertussis toxin inhibition of transglutaminase induction is due to inhibition of tissue transglutaminase mRNA accumulation and is paralleled by the ADP-ribosylation of a 41,000 dalton macrophage membrane protein. It is concluded that soluble retinoic acid binding proteins are not essential for retinoic acid induction of tissue transglutaminase and that a membrane GTP-binding protein is closely linked to the sensitive response of macrophages to retinoic acid. ^

THE BIOSYNTHESIS AND CHARACTERIZATION OF MURINE LEUKEMIA VIRAL PROTEINS

Two murine leukemia viruses (MuLVs), Rauscher (R-MuLV) and Moloney (Mo-MuLV) MuLVs, were studied to identify the biosynthetic pathways leading to the generation of mature virion proteins. Emphasis was placed on the examination of the clone 1 Mo-MuLV infected cell system.^ At least three genetic loci vital to virion replication exist on the MuLV genome. The 'gag' gene encodes information for the virion core proteins. The 'pol' gene specifies information for the RNA-dependent-DNA-polymerase (pol), or reverse transcriptase (RT). The 'env' gene contains information for the virion envelope proteins.^ MuLV specified proteins were synthesized by way of precursor polyproteins, which were processed to yield mature virion proteins. Pulse-chase kinetic studies, radioimmunoprecipitation, and peptide mapping were the techniques used to identify and characterize the MuLV viral precursor polyproteins and mature virion proteins.^ The 'gag' gene of Mo-MuLV coded for two primary gene products. One 'gag' gene product was found to be a polyprotein of 65,000 daltons M(,r) (Pr65('gag)). Pr65('gag) contained the antigenic and structural determinants of all four viral core proteins--p30, p15, pp12 and p10. Pr65('gag) was the major intracellular precursor polyprotein in the generation of mature viral core proteins. The second 'gag' gene product was a glycosylated gene product (gPr('gag)). An 85,000 dalton M(,r) polyprotein (gPr85('gag)) and an 80,000 dalton M(,r) (gPr80('gag)) polyprotein were the products of the 'gag' genes of Mo-MuLV and R-MuLV, respectively. gPr('gag) contained the antigenic and structural determinants of the four virion core proteins. In addition, gPr('gag) contained peptide information over and above that of Pr65('gag). Pulse-chase kinetic studies in the presence of tunicamycin revealed a separate processing pathway of gPr('gag) that did not seem to involve the generation of mature virion core proteins. Subglycosylated gPr('gag) was found to have a molecular weight of 75,000 daltons (Pr75('gag)) for both Mo-MuLV and R-MuLV.^ The Mo-MuLV 'pol' gene product was initially synthesized as a read-through 'gag-pol' intracellular polyprotein containing both antigenic and structural determinants of both the 'gag' and 'pol' genes. This read-through polyprotein was found to be a closely spaced doublet of two similarly sized proteins at 220-200,000 daltons M(,r) (Pr220/200('gag-pol)). Pulse-chase kinetic studies revealed processing of Pr220/200('gag-pol) to unstable intermediate intracellular proteins of 145,000 (Pr145('pol)), 135,000 (Pr135('pol)), and 125,000 (Pr125('pol)) daltons M(,r). Further chase incubations demonstrated the appearance of an 80,000 dalton M(,r) protein, which represented the mature polymerase (p80('pol)).^ The primary intracellular Mo-MuLV 'env' gene product was found to be a glycosylated polyprotein of 83,000 daltons M(,r) (gPr83('env)). gPr83('env) contained the antigenic and structural determinants of both mature virion envelope proteins, gp70 and p15E. In addition, gPr83('env) contained unique peptide sequences not present in either gp70 or p15E. The subglycosylated form of gPr83('env) had a molecular weight of 62,000 daltons (Pr62('env)).^ Virion core proteins of R-MuLV and Mo-MuLV were examined. Structural homology was observed betwen p30s and p10s. Significant structural non-homology was demonstrated between p15s and pp12s. ^

THE TRANSLATION PRODUCTS OF MOLONEY MURINE SARCOMA VIRUS 124 GENOMIC RNA

Murine sarcoma viruses constitute a class of replication-defective retroviruses. Cellular transformation may be induced by these viruses in vitro; whereas, fibrosarcomas may result in animals infected with them in vivo (Tooze, 1973; Bishop, 1978). Hybridization studies suggest that murine sarcoma viruses arose by recombination between nondefective murine leukemia virus sequences and certain cellular sequences present in uninfected mouse cells (Hu et al., 1977). A specific gene product, however, has not been implicated in murine sarcoma virus transformation.^ One line of murine sarcoma virus-producing cells, Mo-MuSV-clone 124, (Ball et al., 1973), was studied biochemically because it mainly produces the sarcoma virus as a pseudotype packaged with helper murine leukemia virus proteins. The sarcoma viral RNA was translated in a sophisticated cell-free protein synthesizing system (Murphy and Arlinghaus, 1978). The translation products were analyzed by a number of techniques, including electrophoresis in denaturing gels of SDS polyacrylamide, immunoprecipitation, and peptide mapping. The major products of the total RNA purified from the virus preparation were shown to have molecular weights of about 63,000 (P63('gag)), 42,000 (P42), 40,000 (P40), 38,000 (P38), and 23,000 (P23). The size class of mRNA coding for each of the cell-free products was estimated using a poly(A) selection technique and sucrose gradient fractionation. These analyses were used to localize the coding information related to each of the in vitro synthesized cell-free products within the sarcoma virus genome.^ The major findings of these studies were: (1) the 5' half of the sarcoma viral RNA codes for the 63,000 dalton polypeptide and 42,000 - 38,000 dalton polypeptides derived from the "gag" gene; and (2) the 3' half of the sarcoma viral RNA codes for a 38,000 dalton polypeptide and possibly derived from the cellular acquired sequences. ^

Calculating Basal Thermal Zones Beneath the Antarctic Ice Sheet

A procedure is presented for using a simple flowline model to calculate the fraction of the bed that is thawed beneath present-day ice sheets, and therefore for mapping thawed, frozen, melting and freezing basal thermal zones. The procedure is based on the proposition, easily demonstrated, that variations in surface slope along ice flowlines are due primarily to variations in bed topography and ice-bed coupling, where ice-bed coupling for sheet flow is represented by the basal thawed fraction. This procedure is then applied to the central flowlines of flow bands on the Antarctic ice sheet where accumulation rates, surface elevations and bed topography are mapped with sufficient accuracy, and where sheet flow rather than stream flow prevails. In East Antarctica, the usual condition is a low thawed fraction in subglacial highlands, but a high thawed fraction in subglacial basins and where ice converges on ice streams. This is consistent with a greater depression of the basal melting temperature and a slower rate of conducting basal heat to the surface where ice is thick, and greater basal frictional heat production where ice flow is fast, as expected for steady-state flow. This correlation is reduced or even reversed where steady-state flow has been disrupted recently, notably where ice-stream surges produced the Dibble and Dalton Iceberg Tongues, both of which are now stagnating. In West Antarctica, for ice draining into the Pine Island Bay polynya of the Amundsen Sea, the basal thawed fraction is consistent with a prolonged and ongoing surge of Pine Island Glacier and with a recently initiated surge of Thwaites Glacier. For ice draining into the Ross Ice Shelf, long ice streams extend nearly to the West Antarctic ice divide. Over the rugged bed topography near the ice divide, no correlation consistent with steady-state sheet flow exists between ice thickness and the basal thawed fraction. The bed is wholly thawed beneath ice streams, even where stream flow is slow. This is consistent with ongoing gravitational collapse of ice entering the Ross Sea embayment and with unstable flow in the ice streams.

The coupled atmosphere–chemistry–ocean model SOCOL-MPIOM

The newly developed atmosphere–ocean-chemistry-climate model SOCOL-MPIOM is presented by demonstrating the influence of the interactive chemistry module on the climate state and the variability. Therefore, we compare pre-industrial control simulations with (CHEM) and without (NOCHEM) interactive chemistry. In general, the influence of the chemistry on the mean state and the variability is small and mainly restricted to the stratosphere and mesosphere. The largest differences are found for the atmospheric dynamics in the polar regions, with slightly stronger northern and southern winter polar vortices in CHEM. The strengthening of the vortex is related to larger stratospheric temperature gradients, which are attributed to a parametrization of the absorption of ozone and oxygen in the Lyman-alpha, Schumann–Runge, Hartley, and Higgins bands. This effect is parametrized in the version with interactive chemistry only. A second reason for the temperature differences between CHEM and NOCHEM is related to diurnal variations in the ozone concentrations in the higher atmosphere, which are missing in NOCHEM. Furthermore, stratospheric water vapour concentrations differ substantially between the two experiments, but their effect on the temperatures is small. In both setups, the simulated intensity and variability of the northern polar vortex is inside the range of present day observations. Sudden stratospheric warming events are well reproduced in terms of their frequency, but the distribution amongst the winter months is too uniform. Additionally, the performance of SOCOL-MPIOM under changing external forcings is assessed for the period 1600–2000 using an ensemble of simulations driven by a spectral solar forcing reconstruction. The amplitude of the reconstruction is large in comparison to other state-of-the-art reconstructions, providing an upper limit for the importance of the solar signal. In the pre-industrial period (1600–1850) the simulated surface temperature trends are in reasonable agreement with temperature reconstructions, although the multi-decadal variability is more pronounced. This enhanced variability can be attributed to the variability in the solar forcing. The simulated temperature reductions during the Maunder Minimum are in the lowest probability range of the proxy records. During the Dalton Minimum, when also volcanic forcing is an important driver of temperature variations, the agreement is better. In the industrial period from 1850 onward SOCOL-MPIOM overestimates the temperature increase in comparison to observational data sets. Sensitivity simulations show that this overestimation can be attributed to the increasing trend in the solar forcing reconstruction that is used in this study and an additional warming induced by the simulated ozone changes.

Alpine lacustrine varved record reveals summer temperature as main control of glacier fluctuations over the past 2250 years

Glacier fluctuations are a key indicator of changing climate. Their reconstruction beyond historical times unravels glacier variability and its forcing factors on long time scales, which can considerably improve our understanding of the climate–glacier relationship. Here, we present a 2250-year-long reconstruction of particle-mass accumulation rates recorded in the lacustrine sediments of Lake Trüebsee (Central Swiss Alps) that are directly related to glacier extent, thus reflecting a continuous record of fluctuations of the upstream-located Titlis Glacier. Mass accumulation rate values show strong centennial to multi-centennial fluctuations and reveal 12 well-pronounced periods of enhanced values corresponding to times of maximum extent of the neighboring Lower Grindelwald Glacier. This result supports previous studies of proglacial lake sediments that documented high mass accumulation rate values during glacier advances. The strong variability in the Lake Trüebsee mass accumulation rate record thus represents a highly sensitive paleoclimatic archive, which mirrors rapid and pronounced feedbacks of Titlis Glacier to climatic changes over the past 2250years. The comparison of our data with independent paleo-temperature reconstructions from tree rings suggests that variations in mean summer temperature were the primary driving factor of fluctuations of Titlis Glacier. Also, advances of Titlis Glacier occurred during the grand solar minima (Dalton, Maunder, Spörer, Wolf) of the last millennium. This relation of glacier extent with summer temperature reveals strong evidence that the mass balance of this Alpine glacier is primarily controlled by the intensity of glacier melting during summer.