Evidence of an active volcanic heat source beneath the Pine Island Glacier

Tectonic landforms reveal that the West Antarctic Ice Sheet (WAIS) lies atop a major volcanic rift system. However, identifying subglacial volcanism is challenging. Here we show geochemical evidence of a volcanic heat source upstream of the fast-melting Pine Island Ice Shelf, documented by seawater helium isotope ratios at the front of the Ice Shelf cavity. The localization of mantle helium to glacial meltwater reveals that volcanic heat induces melt beneath the grounded glacier and feeds the subglacial hydrological network crossing the grounding line. The observed transport of mantle helium out of the Ice Shelf cavity indicates that volcanic heat is supplied to the grounded glacier at a rate of ~ 2500 ± 1700 MW, which is ca. half as large as the active Grimsvötn volcano on Iceland. Our finding of a substantial volcanic heat source beneath a major WAIS glacier highlights the need to understand subglacial volcanism, its hydrologic interaction with the marine margins, and its potential role in the future stability of the WAIS

CLE14/CLE20 peptides may interact with CLAVATA2/CORYNE receptor-like kinases to irreversibly inhibit cell division in the root meristem of Arabidopsis

Towards an understanding of the interacting nature of the CLAVATA (CLV) complex, we predicted the 3D structures of CLV3/ESR-related (CLE) peptides and the ectodomain of their potential receptor proteins/kinases, and docking models of these molecules. The results show that the ectodomain of CLV1 can form homodimers and that the 12-/13-amino-acid CLV3 peptide fits into the binding clefts of the CLV1 dimers. Our results also demonstrate that the receptor domain of CORYNE (CRN), a recently identified receptor-like kinase, binds tightly to the ectodomain of CLV2, and this likely leads to an increased possibility for docking with CLV1. Furthermore, our docking models reveal that two CRN-CLV2 ectodomain heterodimers are able to form a tetramer receptor complex. Peptides of CLV3, CLE14, CLE19, and CLE20 are also able to bind a potential CLV2-CRN heterodimer or heterotetramer complex. Using a cell-division reporter line, we found that synthetic 12-amino-acid CLE14 and CLE20 peptides inhibit, irreversibly, root growth by reducing cell division rates in the root apical meristem, resulting in a short-root phenotype. Intriguingly, we observed that exogenous application of cytokinin can partially rescue the short-root phenotype induced by over-expression of either CLE14 or CLE20 in planta. However, cytokinin treatment does not rescue the short-root phenotype caused by exogenous application of the synthetic CLE14/CLE20 peptides, suggesting a requirement for a condition provided only in living plants. These results therefore imply that the CLE14/CLE20 peptides may act through the CLV2-CRN receptor kinase, and that their availabilities and/or abundances may be affected by cytokinin activity in planta

Evolution of the B3 DNA Binding Superfamily: New Insights into REM Family Gene Diversification

Background: The B3 DNA binding domain includes five families: auxin response factor (ARF), abscisic acid-insensitive3 (ABI3), high level expression of sugar inducible (HSI), related to ABI3/VP1 (RAV) and reproductive meristem (REM). The release of the complete genomes of the angiosperm eudicots Arabidopsis thaliana and Populus trichocarpa, the monocot Orysa sativa, the bryophyte Physcomitrella patens,the green algae Chlamydomonas reinhardtii and Volvox carteri and the red algae Cyanidioschyzon melorae provided an exceptional opportunity to study the evolution of this superfamily. Methodology: In order to better understand the origin and the diversification of B3 domains in plants, we combined comparative phylogenetic analysis with exon/intron structure and duplication events. In addition, we investigated the conservation and divergence of the B3 domain during the origin and evolution of each family. Conclusions: Our data indicate that showed that the B3 containing genes have undergone extensive duplication events, and that the REM family B3 domain has a highly diverged DNA binding. Our results also indicate that the founding member of the B3 gene family is likely to be similar to the ABI3/HSI genes found in C. reinhardtii and V. carteri. Among the B3 families, ABI3, HSI, RAV and ARF are most structurally conserved, whereas the REM family has experienced a rapid divergence. Thes

Društveno-ekonomski aspekti učiteljstva

U radu se prvo definira učiteljstvo kao profesija, zajednički stručni naziv – učitelj (i za učitelja, nastavnika, profesora i stručnog suradnika u školi). Zatim se govori o vrijednosti učiteljske profesije. Slijedi analiza materijalne osnove i financiranja učiteljstva, plaće učitelja i ostala materijalna prava. Potom slijedi prikaz učiteljskih udruga i učiteljske nagrade „Ivan Filipović“. Posebno se obrađuje pitanje – kakvi su učitelji potrebni novoj hrvatskoj školi. Hrvatskoj školi potrebni su sposobni, obrazovni, stručno pedagoško osposobljeni, motivirani, materijalno situirani, zadovoljni, samostalni, slobodni i demokratski učitelji. Svjetski dan učitelja prigoda je da se sjetimo svoje učiteljice-učitelja, njihovih riječi i djela koja su obilježila naše odrastanje i ostavili duboki trag u našim srcima

Assessment of variation in immunosuppressive pathway genes reveals TGFBR2 to be associated with risk of clear cell ovarian cancer

BACKGROUND: Regulatory T (Treg) cells, a subset of CD4+ T lymphocytes, are mediators of immunosuppression in cancer, and, thus, variants in genes encoding Treg cell immune molecules could be associated with ovarian cancer. METHODS: In a population of 15,596 epithelial ovarian cancer (EOC) cases and 23,236 controls, we measured genetic associations of 1,351 SNPs in Treg cell pathway genes with odds of ovarian cancer and tested pathway and gene-level associations, overall and by histotype, for the 25 genes, using the admixture likelihood (AML) method. The most significant single SNP associations were tested for correlation with expression levels in 44 ovarian cancer patients. RESULTS: The most significant global associations for all genes in the pathway were seen in endometrioid (p = 0.082) and clear cell (p = 0.083), with the most significant gene level association seen with TGFBR2 (p = 0.001) and clear cell EOC. Gene associations with histotypes at p < 0.05 included: IL12 (p = 0.005 and p = 0.008, serous and high-grade serous, respectively), IL8RA (p = 0.035, endometrioid and mucinous), LGALS1 (p = 0.03, mucinous), STAT5B (p = 0.022, clear cell), TGFBR1 (p = 0.021 endometrioid) and TGFBR2 (p = 0.017 and p = 0.025, endometrioid and mucinous, respectively). CONCLUSIONS: Common inherited gene variation in Treg cell pathways shows some evidence of germline genetic contribution to odds of EOC that varies by histologic subtype and may be associated with mRNA expression of immune-complex receptor in EOC patients

The Greenland and Antarctic ice sheets under 1.5◦C global warming

Even if anthropogenic warming were constrained to less than 2°C above pre-industrial, the Greenland and Antarctic ice sheets will continue to lose mass this century, with rates similar to those observed over the last decade. However, nonlinear responses cannot be excluded, which may lead to larger rates of mass loss. Furthermore, large uncertainties in future projections still remain, pertaining to knowledge gaps in atmospheric (Greenland) and oceanic (Antarctica) forcing. On millennial timescales, both ice sheets have tipping points at or slightly above the 1.5-2.0°C threshold; for Greenland, this may lead to irreversible mass loss due to the surface mass balance elevation feedback, while for Antarctica, this could result in a collapse of major drainage basins due to ice-shelf weakening