The response of atmospheric nitrous oxide to climate variations during the last glacial period

Detailed insight into natural variations of the greenhouse gas nitrous oxide (N2O) in response to changes in the Earth's climate system is provided by new measurements along the ice core of the North Greenland Ice Core Project (NGRIP). The presented record reaches from the early Holocene back into the previous interglacial with a mean time resolution of about 75 years. Between 11 and 120 kyr BP, atmospheric N2O concentrations react substantially to the last glacial-interglacial transition (Termination 1) and millennial time scale climate variations of the last glacial period. For long-lasting Dansgaard/Oeschger (DO) events, the N2O increase precedes Greenland temperature change by several hundred years with an increase rate of about 0.8-1.3 ppbv/century, which accelerates to about 3.8-10.7 ppbv/century at the time of the rapid warming in Greenland. Within each bundle of DO events, the new record further reveals particularly low N2O concentrations at the approximate time of Heinrich events. This suggests that the response of marine and/or terrestrial N2O emissions on a global scale are different for stadials with and without Heinrich events.

A reconstruction of atmospheric carbon dioxide and its stable carbon isotopic composition from the penultimate glacial maximum to the last glacial inception

The reconstruction of the stable carbon isotope evolution in atmospheric CO2 (δ13Catm), as archived in Antarctic ice cores, bears the potential to disentangle the contributions of the different carbon cycle fluxes causing past CO2 variations. Here we present a new record of δ13Catm before, during and after the Marine Isotope Stage 5.5 (155 000 to 105 000 yr BP). The dataset is archived on the data repository PANGEA® (www.pangea.de) under 10.1594/PANGAEA.817041. The record was derived with a well established sublimation method using ice from the EPICA Dome C (EDC) and the Talos Dome ice cores in East Antarctica. We find a 0.4‰ shift to heavier values between the mean δ13Catm level in the Penultimate (~ 140 000 yr BP) and Last Glacial Maximum (~ 22 000 yr BP), which can be explained by either (i) changes in the isotopic composition or (ii) intensity of the carbon input fluxes to the combined ocean/atmosphere carbon reservoir or (iii) by long-term peat buildup. Our isotopic data suggest that the carbon cycle evolution along Termination II and the subsequent interglacial was controlled by essentially the same processes as during the last 24 000 yr, but with different phasing and magnitudes. Furthermore, a 5000 yr lag in the CO2 decline relative to EDC temperatures is confirmed during the glacial inception at the end of MIS5.5 (120 000 yr BP). Based on our isotopic data this lag can be explained by terrestrial carbon release and carbonate compensation.

A reconstruction of radiocarbon production and total solar irradiance from the Holocene ¹⁴C and CO₂ records: implications of data and model uncertainties

Radiocarbon production, solar activity, total solar irradiance (TSI) and solar-induced climate change are reconstructed for the Holocene (10 to 0 kyr BP), and TSI is predicted for the next centuries. The IntCal09/SHCal04 radiocarbon and ice core CO2 records, reconstructions of the geomagnetic dipole, and instrumental data of solar activity are applied in the Bern3D-LPJ, a fully featured Earth system model of intermediate complexity including a 3-D dynamic ocean, ocean sediments, and a dynamic vegetation model, and in formulations linking radiocarbon production, the solar modulation potential, and TSI. Uncertainties are assessed using Monte Carlo simulations and bounding scenarios. Transient climate simulations span the past 21 thousand years, thereby considering the time lags and uncertainties associated with the last glacial termination. Our carbon-cycle-based modern estimate of radiocarbon production of 1.7 atoms cm−2 s−1 is lower than previously reported for the cosmogenic nuclide production model by Masarik and Beer (2009) and is more in-line with Kovaltsov et al. (2012). In contrast to earlier studies, periods of high solar activity were quite common not only in recent millennia, but throughout the Holocene. Notable deviations compared to earlier reconstructions are also found on decadal to centennial timescales. We show that earlier Holocene reconstructions, not accounting for the interhemispheric gradients in radiocarbon, are biased low. Solar activity is during 28% of the time higher than the modern average (650 MeV), but the absolute values remain weakly constrained due to uncertainties in the normalisation of the solar modulation to instrumental data. A recently published solar activity–TSI relationship yields small changes in Holocene TSI of the order of 1 W m−2 with a Maunder Minimum irradiance reduction of 0.85 ± 0.16 W m−2. Related solar-induced variations in global mean surface air temperature are simulated to be within 0.1 K. Autoregressive modelling suggests a declining trend of solar activity in the 21st century towards average Holocene conditions.

An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120--800 ka

An accurate and coherent chronological framework is essential for the interpretation of climatic and environmental records obtained from deep polar ice cores. Until now, one common ice core age scale had been developed based on an inverse dating method (Datice), combining glaciological modelling with absolute and stratigraphic markers between 4 ice cores covering the last 50 ka (thousands of years before present) (Lemieux-Dudon et al., 2010). In this paper, together with the companion paper of Veres et al. (2013), we present an extension of this work back to 800 ka for the NGRIP, TALDICE, EDML, Vostok and EDC ice cores using an improved version of the Datice tool. The AICC2012 (Antarctic Ice Core Chronology 2012) chronology includes numerous new gas and ice stratigraphic links as well as improved evaluation of background and associated variance scenarios. This paper concentrates on the long timescales between 120–800 ka. In this framework, new measurements of δ18Oatm over Marine Isotope Stage (MIS) 11–12 on EDC and a complete δ18Oatm record of the TALDICE ice cores permit us to derive additional orbital gas age constraints. The coherency of the different orbitally deduced ages (from δ18Oatm, δO2/N2 and air content) has been verified before implementation in AICC2012. The new chronology is now independent of other archives and shows only small differences, most of the time within the original uncertainty range calculated by Datice, when compared with the previous ice core reference age scale EDC3, the Dome F chronology, or using a comparison between speleothems and methane. For instance, the largest deviation between AICC2012 and EDC3 (5.4 ka) is obtained around MIS 12. Despite significant modifications of the chronological constraints around MIS 5, now independent of speleothem records in AICC2012, the date of Termination II is very close to the EDC3 one.

Cell Cycle Regulatory Roles of Estrogen Receptor alpha (ERα) in Breast Cancer Cells

Previous studies have shown that Estrogen Receptor alpha (ERα) is an important indicator for diagnosis, prognosis and treatment of breast cancers. However, the question remains as to the role of ERα in the cell in the presence versus absence of 17-β estradiol In this dissertation the role of ERα in both its unliganded and liganded state, with respect to the cell cycle will be explored. The cell line models used in this project are ER-positive MCF-7 cells with and without siRNA to ERα and ER-positive MDA-MB-231 cells that have been engineered to express ERα. Cells were synchronized and the cell cycle progression was monitored by flow cytometric analysis. Using these methods, two specific questions were addressed: Does ERα modulate the cell cycle differently under liganded versus unliganded conditions? And, does the presence of ERα regulate cell cycle phase transitions? The results show for the first time that ERα is cell cycle regulated and modulates the progression of cells through S and G2/M phases of the cell cycle. Ligand bound ERα increases progression through S and G2/M phases, whereas unliganded ERα acts as an inhibitor of cell cycle progression. To further investigate the cell cycle regulated effects of liganded ERα, a luciferase assay was performed and showed that the transcription of target genes such as Progestrone Receptor (PgR) and Trefoil protein (pS2) increased duing S and G2/M phases when ERα is bound to ligand. Additionally, complex formation between cyclin B and ER α was shown by immunoprecipitation and led to the discovery that anaphase promoting complex (APC) is the E3 ligase for both cyclin B and ERα at the termination of M phase. Our findings suggest that unliganded ERα has an inhibitory effect on the progression of the cell cycle. Therefore, it is reasonable to speculate that the combination of drugs that lower estrogen level (such as aromatase inhibitors) and preserves ERα from degradation would provide better outcome for breast cancer treatment. We have shown that APC functions as the E3 ligase for ERα and thus might provide a target to design a specific inhibitor of ERα degradation.

Dose–effect relationship in routine outpatient psychotherapy: Does treatment duration matter?

Objective: There is an ongoing debate concerning how outcome variables change during the course of psychotherapy. We compared the dose–effect model, which posits diminishing effects of additional sessions in later treatment phases, against a model that assumes a linear and steady treatment progress through termination. Method: Session-by-session outcome data of 6,375 outpatients were analyzed, and participants were categorized according to treatment length. Linear and log-linear (i.e., negatively accelerating) latent growth curve models (LGCMs) were estimated and compared for different treatment length categories. Results: When comparing the fit of the various models, the log-linear LGCMs assuming negatively accelerating treatment progress consistently outperformed the linear models irre- spective of treatment duration. The rate of change was found to be inversely related to the length of treatment. Conclusion: As proposed by the dose–effect model, the expected course of improvement in psychotherapy appears to follow a negatively accelerated pattern of change, irrespective of the duration of the treatment. However, our results also suggest that the rate of change is not constant across various treatment lengths. As proposed by the “good enough level” model, longer treatments are associated with less rapid rates of change.

The role of Sse1 in the de novo formation and variant determination of the [PSI+] prion.

Yeast prions are a group of non-Mendelian genetic elements transmitted as altered and self-propagating conformations. Extensive studies in the last decade have provided valuable information on the mechanisms responsible for yeast prion propagation. How yeast prions are formed de novo and what cellular factors are required for determining prion "strains" or variants--a single polypeptide capable of existing in multiple conformations to result in distinct heritable phenotypes--continue to defy our understanding. We report here that Sse1, the yeast ortholog of the mammalian heat-shock protein 110 (Hsp110) and a nucleotide exchange factor for Hsp70 proteins, plays an important role in regulating [PSI+] de novo formation and variant determination. Overproduction of the Sse1 chaperone dramatically enhanced [PSI+] formation whereas deletion of SSE1 severely inhibited it. Only an unstable weak [PSI+] variant was formed in SSE1 disrupted cells whereas [PSI+] variants ranging from very strong to very weak were formed in isogenic wild-type cells under identical conditions. Thus, Sse1 is essential for the generation of multiple [PSI+] variants. Mutational analysis further demonstrated that the physical association of Sse1 with Hsp70 but not the ATP hydrolysis activity of Sse1 is required for the formation of multiple [PSI+] variants. Our findings establish a novel role for Sse1 in [PSI+] de novo formation and variant determination, implying that the mammalian Hsp110 may likewise be involved in the etiology of protein-folding diseases.

A biophysical model of synaptic plasticity and metaplasticity can account for the dynamics of the backward shift of hippocampal place fields.

Hippocampal place cells in the rat undergo experience-dependent changes when the rat runs stereotyped routes. One such change, the backward shift of the place field center of mass, has been linked by previous modeling efforts to spike-timing-dependent plasticity (STDP). However, these models did not account for the termination of the place field shift and they were based on an abstract implementation of STDP that ignores many of the features found in cortical plasticity. Here, instead of the abstract STDP model, we use a calcium-dependent plasticity (CaDP) learning rule that can account for many of the observed properties of cortical plasticity. We use the CaDP learning rule in combination with a model of metaplasticity to simulate place field dynamics. Without any major changes to the parameters of the original model, the present simulations account both for the initial rapid place field shift and for the subsequent slowing down of this shift. These results suggest that the CaDP model captures the essence of a general cortical mechanism of synaptic plasticity, which may underlie numerous forms of synaptic plasticity observed both in vivo and in vitro.

Current Resources

Reviews of: Treating the Tough Adolescent: A Family-Based Step-by-St Guide. (1998) Scott P. Sells. New York: The Guilford Press. Reviewed by John P. Nasuti Essential Skills in Family Therapy: From the First Interview to Termination. (1998) JoEllen Patterson, Lee Williams, Claudia Grauf-Grounds, and Larry Chamow. New York: The Guilford Press. Reviewed by Rowena Fong Putting Families First America's Family Support Movement and the Challenge of Change. (1994) Sharon L. Kagan and Bernice Weissbound, Editors. San Francisco: Jossey-Bass Publishers. Reviewed by Anthony N. Maluccio The Work-Family Challenge Rethinking Employment. Edited by Susan Lewis and Jeremy Lewis. 1996. Thousand Oaks, California: SAGE Publications, Ltd. Reviewed by Harry J. Macy

Metabolism and action of 9-$\beta$-D-arabinofuranosyl-2-fluoroadenine

9-$\beta$-D-arabinofuranosyl-2-fluoroadenine (F-ara-A) is an analogue of adenosine and 2$\sp\prime$-deoxyadenosine with potent antitumor activity both in vitro and in vivo. The mechanism of action of F-ara-A was evaluated both in whole cells and in experimental systems with purified enzymes. F-ara-A was converted to its 5$\sp\prime$-triphosphate F-ara-ATP in cells and then incorporated into DNA in a self-limiting manner. About 98% of the incorporated F-ara-AMP residues were located at the 3$\sp\prime$-termini of DNA strands, suggesting a chain termination property of this compound. DNA synthesis in CEM cells was inhibited by F-ara-A treatment with an IC$\sb{50}$ value of 1 $\mu$M. Cells were not able to restore the normal level of DNA synthesis even after being cultured in drug-free medium for 40 h. A DNA primer extension assay with M13mp18(+) single-stranded DNA template using purified human DNA polymerases $\alpha$ and further revealed that F-ara-ATP competed with dATP for incorporation into the A sites of the elongating DNA strands. The incorporation of F-ara-AMP into DNA resulted in a termination of DNA synthesis at the incorporated A sites. Pol $\alpha$ and $\delta$ were not able to efficiently extend the DNA primer with F-ara-AMP at its 3$\sp\prime$-end. Furthermore, the presence of F-ara-AMP at the 3$\sp\prime$-end of an oligodeoxyribonucleotide impaired its ligation with an adjacent DNA fragment by human and T4 ligases. Human DNA polymerase $\alpha$ incorporated more F-ara-AMP into DNA than polymerase $\delta$ and was more sensitive to the inhibition by F-ara-ATP, suggesting that polymerase $\alpha$ may be a preferred target for this analogue. On the other hand, DNA-dependent nucleotide turnover experiments and sequencing gel analysis demonstrated that DNA polymerase $\delta$ was able to remove the incorporated F-ara-AMP residue from the 3$\sp\prime$-end of the DNA strand with its 3$\sp\prime$-5$\sp\prime$ exonuclease activity in vitro, subsequently permitting further elongation of the DNA strand.^ The incorporation of F-ara-AMP into DNA was linearly correlated both with the inhibition of DNA synthesis and with the loss of clonogenicity. Termination of DNA synthesis and deletion of genetic material resulted from F-ara-AMP incorporation may be the mechanism responsible for cytotoxicity of F-ara-A. (Abstract shortened with permission of author.) ^

Intracellular signalling by the insulin receptor

The insulin receptor transduces insulin's biological signal through the tyrosine kinase present in the receptor's B subunit. The activated insulin receptor kinase then phosphorylates a series of intracellular substrate including insulin receptor substrate 1 (IRS-1), which has been shown to be the pivotal substrate for insulin receptor signal transduction. The phosphorylated tyrosine residues in IRS-1 can bind and activate the downstream effectors, many of which are SH2 domain containing proteins such as phosphotidylinositol 3-kinase, growth factor binding protein 2, and SH2 phosphotyrosine phosphatase 2. Phosphorylated synthetic IRS-1 peptides with the corresponding sequences of the IRS-1 have been shown to associate and activate their respective SH2 domain containing proteins. Another important event happening during insulin binding with the insulin receptor is that the insulin receptor rapidly undergoes internalization. However, the insulin receptor signalling and the receptor endocytosis have been studied as two independent processes. The hypothesis of the present thesis is that the insulin receptor endocytosis is involved in insulin receptor signalling and signal termination. The results of the present investigation demonstrate that insulin receptors in the earliest stage of endocytosis contain significantly greater kinase activity towards IRS-1 peptides than the receptors localized at the plasma membrane, indicating that they are potentially more capable of transducing signals. On the other hand, insulin receptors in the middle and late stage of endocytosis lose their kinase activity, suggesting that insulin receptor kinase activity inactivation and signal termination might take place in the late phase of the insulin receptor internalization. In addition, this study also found that the increased insulin receptor kinase activity in the endosomes is related to the tyrosyl phosphorylation of the specific domains of the receptor's $\beta$ subunit. ^

Fruit production in three masting tree species does not rely on stored carbon reserves

Fruiting is typically considered to massively burden the seasonal carbon budget of trees. The cost of reproduction has therefore been suggested as a proximate factor explaining observed mast-fruiting patterns. Here, we used a large-scale, continuous 13C labeling of mature, deciduous trees in a temperate Swiss forest to investigate to what extent fruit formation in three species with masting reproduction behavior (Carpinus betulus, Fagus sylvatica, Quercus petraea) relies on the import of stored carbon reserves. Using a free-air CO2 enrichment system, we exposed trees to 13C-depleted CO2 during 8 consecutive years. By the end of this experiment, carbon reserve pools had significantly lower δ13C values compared to control trees. δ13C analysis of new biomass during the first season after termination of the CO2 enrichment allowed us to distinguish the sources of built-in carbon (old carbon reserves vs. current assimilates). Flowers and expanding leaves carried a significant 13C label from old carbon stores. In contrast, fruits and vegetative infructescence tissues were exclusively produced from current, unlabeled photoassimilates in all three species, including F. sylvatica, which had a strong masting season. Analyses of δ13C in purified starch from xylem of fruit-bearing shoots revealed a complete turn-over of starch during the season, likely due to its usage for bud break. This study is the first to directly demonstrate that fruiting is independent from old carbon reserves in masting trees, with significant implications for mechanistic models that explain mast seeding.

A PHARMACOLOGICAL EVALUATION OF THE MECHANISM OF CYTOTOXICITY OF 9-BETA-D- XYLOFURANOSYLADENINE IN CHINESE HAMSTER OVARY CELLS

The biochemical determinants of cytotoxicity of the purine nucleoside analog, 9-(beta)-D-xylofuranosyladenine (xyl-A) were studied in wild-type Chinese hamster ovary cells and in nucleoside kinase deficient mutants. It was found that {('3)H}xyl-A was readily phosphorylated to the triphosphate level in both the wild-type and deoxycytidine kinase deficient mutant, but not by the adenosine kinase deficient cells. Values for the apparent Km and Vmax of this uptake process were 43.9 (mu)M and 118.7 nmol/min/10('9) cells, respectively. Cloning procedures indicated that the viability of CHO cells was decreased 90 per cent by a 5-hr incubation with 10 (mu)M xyl-A. However, the toxicity of xyl-A was increased 100-fold by the addition of a nontoxic concentration (10 (mu)M) of the adenosine deaminase inhibitor erythro-9-(2-hydroxy-3-nonyl)adenine (EHNA) to the medium. High-pressure liquid chromatographic analysis indicated that after 5 hr, the concentration of 9-(beta)-D-xylofuranosyladenine 5'-triphosphate (xyl-ATP) in cells incubated with xyl-A plus EHNA was 2.0 mM, four times greater than in those cells incubated with xyl-A alone. Incubation with xyl-A plus EHNA had no significant effect on the cellular concentrations of 5-phosphoribosyl-1-pyrophosphate after 1 hr whereas, treatment with 3'-dexoyadenosine (cordycepin) decreased the concentration of this metabolite. Determinations of the cellular nucleoside triphosphates indicated that under conditions that resulted in an intracellular accumulation of 500 (mu)M xyl-ATP, the endogenous concentrations of neither the ribonucleoside triphosphates nor deoxyribonucleoside triphosphates were significantly different from those of control cells. The ID(,50) for {('3)H}thymidine incorporation into DNA, 105 (mu)M xyl-ATP, was four-fold less than the ID(,50) for {('3)H}uridine incorporation into RNA suggesting that the process of DNA synthesis is more sensitive to the presence of xyl-ATP. When removed from exogenous xyl-A, CHO cells failed to recover their ability to synthesize RNA and DNA, although the intracellular xyl-ATP concentration decreased to less than 35 (mu)M. The selective inhibition of RNA synthesis by 6-azauridine did not prevent the expression of toxicity by xyl-ATP. However, the selective inhibition of DNA synthesis by ara-C significantly spared toxicity in cells that had accumulated an otherwise lethal concentration of xyl-ATP. It is shown that in cells which had accumulated 1.27 mM {('3)H}xyl-ATP, {('3)H}xyl-A was found to terminate cellular RNA chains at a frequency of 1.42 (mu)mol of {('3)H}xyl-A 3' termini per mol of mononucleotide. These results indicate that a general mechanism for the toxicity of xyl-A to CHO cells includes the cellular accumulation of xyl-ATP, which serves as a substrate for RNA synthesizing enzymes and subsequently is incorporated into nascent RNA transcripts as a chain terminator. A specific mechanism involving the premature termination of RNA primers required for the initiation of DNA synthesis is proposed to account for the inhibitory action of xyl-ATP on DNA synthesis. ^

High-resolution late-glacial chronology for the Gerzensee lake record (Switzerland): δ18O correlation between a Gerzensee-stack and NGRIP

Oxygen-isotope variations were analyzed on bulk samples of shallow-water lake marl from Gerzensee, Switzerland, in order to evaluate major and minor climatic oscillations during the late-glacial. To highlight the overall signature of the Gerzensee δ18O record, δ18O records of four parallel sediment cores were first correlated by synchronizing major isotope shifts and pollen abundances. Then the records were stacked with a weighting depending on the differing sampling resolution. To develop a precise chronology, the δ18O-stack was then correlated with the NGRIP δ18O record applying a Monte Carlo simulation, relying on the assumption that the shifts in δ18O were climate-driven and synchronous in both archives. The established chronology on the GICC05 time scale is the basis for (1) comparing the δ18O changes recorded in Gerzensee with observed climatic and environmental fluctuations over the whole North Atlantic region, and (2) comparing sedimentological and biological changes during the rapid warming with smaller climatic variations during the Bølling/Allerød period. The δ18O record of Gerzensee is characterized by two major isotope shifts at the onset and at the termination of the Bølling/Allerød warm period, as well as four intervening negative shifts labeled GI-1e2, d, c2, and b, which show a shift of one third to one fourth of the major δ18O shifts at the beginning and end of the Bølling/Allerød. Despite some inconsistency in terminology, these oscillations can be observed in various climatic proxies over wide regions in the North Atlantic region, especially in reconstructed colder temperatures, and they seem to be caused by hemispheric climatic variations.

A Record of Atmospheric Co2 During the Last 40,000 Years from the Siple Dome, Antarctica Ice Core

We have measured the CO2 concentration of air occluded during the last 40,000 years in the deep Siple Dome A ( hereafter Siple Dome) ice core, Antarctica. The general trend of CO2 concentration from Siple Dome ice follows the temperature inferred from the isotopic composition of the ice and is mostly in agreement with other Antarctic ice core CO2 records. CO2 rose initially at similar to 17.5 kyr B. P. ( thousand years before 1950), decreased slowly during the Antarctic Cold Reversal, rose during the Younger Dryas, fell to a local minimum at around 8 kyr B. P., and rose continuously since then. The CO2 concentration never reached steady state during the Holocene, as also found in the Taylor Dome and EPICA Dome C ( hereafter Dome C) records. During the last glacial termination, a lag of CO2 versus Siple Dome isotopic temperature is probable. The Siple Dome CO2 concentrations during the last glacial termination and in the Holocene are at certain times greater than in other Antarctic ice cores by up to 20 ppm (mumol CO2/mol air). While in situ production of CO2 is one possible cause of the sporadic elevated levels, the mechanism leading to the enrichment is not yet clear.