1,793 research outputs found

    Chinese Papermaking: A Multicultural and Environmental Education Strategy for Pre-K Teachers

    Full text link
    Many scholars see the urgency of implementing multicultural education (ME) and environmental education (EE) in the primary level (Abdullah, 2009; Bower, 1998; Cohen & Horm-Wingerd, 1993; Trubowitz, 1995). The scholars also share how hands-on and art approaches fit well in both Multicultural Education and Environmental Education fields (Adams & Chisholm, 1999; Bower, 1998; Damm, 2006; Seltzer-Kelly, Westwood, & Peña-Guzman, 2010). Chinese papermaking, an interactive and hands-on exercise in the creation of handmade paper, can be a means of integrating concepts of multiculturalism and sustainability into a young child‘s education. To address this issue, this study aimed at (a) introducing multicultural education, sustainability, and Chinese papermaking; (b) creating a new model MATCH to synthesize multicultural education and environmental education; (c) showing how papermaking is a culturally enriching activity; and, (d) demonstrating child-centered papermaking activities

    Thank you Earth's Future reviewers in 2019

    Get PDF
    AGU's open‐access transdisciplinary science journal Earth's Future continued to grow in size and stature in 2019, with ~40% acceptance rate for ~280 new submissions that were evaluated by a similar number of external reviewers; their names are listed here

    Homoclinic Solutions for a Class of Second Order Nonautonomous Singular Hamiltonian Systems

    Get PDF
    We are concerned with the existence of homoclinic solutions for the following second order nonautonomous singular Hamiltonian systems u¨+atWuu=0, (HS) where -∞<t<+∞, u=u1,u2, …,uN∈ℝNN≥3, a:ℝ→ℝ is a continuous bounded function, and the potential W:ℝN∖{ξ}→ℝ has a singularity at 0≠ξ∈ℝN, and Wuu is the gradient of W at u. The novelty of this paper is that, for the case that N≥3 and (HS) is nonautonomous (neither periodic nor almost periodic), we show that (HS) possesses at least one nontrivial homoclinic solution. Our main hypotheses are the strong force condition of Gordon and the uniqueness of a global maximum of W. Different from the cases that (HS) is autonomous at≡1 or (HS) is periodic or almost periodic, as far as we know, this is the first result concerning the case that (HS) is nonautonomous and N≥3. Besides the usual conditions on W, we need the assumption that a′t<0 for all t∈ℝ to guarantee the existence of homoclinic solution. Recent results in the literature are generalized and significantly improved

    Group 2i Isochrysidales produce characteristic alkenones reflecting sea ice distribution

    Get PDF
    Alkenones are biomarkers produced solely by algae in the order Isochrysidales that have been used to reconstruct sea surface temperature (SST) since the 1980s. However, alkenone based SST reconstructions in the northern high latitude oceans show significant bias towards warmer temperatures in core-tops, diverge from other SST proxies in down core records, and are often accompanied by anomalously high relative abundance of the C37 tetra-unsaturated methyl alkenone (%C37:4). Elevated %C37:4 is widely interpreted as an indicator of low sea surface salinity from polar water masses, but its biological source has thus far remained elusive. Here we identify a lineage of Isochrysidales that is responsible for elevated C37:4 methyl alkenone in the northern high latitude oceans through next-generation sequencing and lab-culture experiments. This Isochrysidales lineage co-occurs widely with sea ice in marine environments and is distinct from other known marine alkenone-producers, namely Emiliania huxleyi and Gephyrocapsa oceanica. More importantly, the %C37:4 in seawater filtered particulate organic matter and surface sediments is significantly correlated with annual mean sea ice concentrations. In sediment cores from the Svalbard region, the %C37:4 concentration aligns with the Greenland temperature record and other qualitative regional sea ice records spanning the past 14 kyrs, reflecting sea ice concentrations quantitatively. Our findings imply that %C37:4 is a powerful proxy for reconstructing sea ice conditions in the high latitude oceans on thousand- and, potentially, on million-year timescales.publishedVersio
    corecore