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The relevance of education and outreach (E&O) activities about the Antarctic Treaty has been recognized at the Antarctic Treaty Consultative Meetings (ATCM) and at the Committee for Environmental Protection (CEP). This study examines the key topics and the target audiences detailed in papers submitted to the ATCM on E&O. Since the Antarctic Treaty entered into force in 1961, a total of 216 ATCM papers on E&O have been produced. The number of papers has increased substantially since the mid-1990s. ‘Science’ (76.9%) and ‘Wildlife/Biodiversity/Environment’ (75.5%) were the most addressed topics in these papers, while the ‘Public’ (81.0%) and those attending ‘Schools’ (69.0%) are the main target audiences. ‘Science’ in ATCM papers increased ~120-fold from 1961–1997 to 2015–2023, while ATCM papers discussing engagement with the ‘Public’ increased ~40-fold during the same period. ‘Climate change’ was first mentioned in 2006, and the number of papers per year increased fourfold by 2015–2023. This study shows the increasing interest in E&O through time, addressing key topics to relevant audiences related to the Antarctic region. From an educational perspective, attention should be paid to emerging topics (e.g. equity, diversity and inclusion), and the engagement of early-career professionals and educators should be made a priority.
Ultra-processed foods (UPF), defined using the Nova classification system, are associated with increased chronic disease risk. More recently, evidence suggests the UPF subgroup of whole-grain breads and cereals is in fact linked with reduced chronic disease risk. This study aimed to explore associations of cardiometabolic risk measures with Nova UPF intake versus when foods with ≥25% or ≥50% whole grain are excluded from the definition. We considered dietary data from the Australian National Nutrition and Physical Activity Survey (NNPAS) 2011-12. Impacts on associations of UPF intake (quintiles) and cardiometabolic risk measures were analysed using regression models. The median proportion of UPF intake from high whole-grain foods was zero for all quintiles. Participants in the highest Nova UPF intake quintile had significantly higher weight (78.1kg [0.6]), BMI (27.2kg/m2 [0.2]), waist circumference (92.7cm [0.5]), and weight-to-height ratio (0.55 [0.003]) compared to the lowest quintile (p<0.05). Associations were the same when foods with ≥25% and ≥50% whole grain were excluded. Adjusted R-squared values remained similar across all approaches for all outcomes. In Australia, high whole-grain foods considered UPF may not significantly contribute to deleterious cardiometabolic risk associations. Until conclusive evidence on Nova UPF is available, prioritisation should be given to the nutrient density of high whole-grain foods and their potential contribution to improving whole-grain intakes and healthful dietary patterns in Australia.
Whole-grain intake is associated with reduced risk of non-communicable diseases. Greater understanding of major food sources of whole grains globally, and how intake has been quantified, is essential to informing accurate strategies aiming to increase consumption and reduce non-communicable disease risk. Therefore, the aim of this review was to identify the primary food sources of whole-grain intake globally and explore how they are quantified and reported within literature, and their recommendation within respective national dietary guidelines. A structured scoping review of published articles and grey literature used a predefined search strategy across electronic databases. Data were extracted and summarised based on identified outcomes (e.g. primary sources of whole-grain intake and quantification methods). Dietary intake values were noted where available. Thirteen records across twenty-four countries identified bread and bread rolls, and ready-to-eat cereals as primary sources of whole-grain intake in Australia, New Zealand, Europe, the UK and Northern America. Elsewhere, sources vary and for large parts of the world (e.g. Africa and Asia), intake data are limited or non-existent. Quantification of whole grain also varied across countries, with some applying different whole-grain food definitions, resulting in a whole-grain intake based on only consumption of select ‘whole-grain’ foods. National dietary guidelines were consistent in promoting whole-grain intake and providing examples of country-specific whole-grain foods. Consistency in whole-grain calculation methods is needed to support accurate and comparative research informing current intake evidence and promotional efforts. National dietary guidelines are consistent in promoting whole-grain intake; however, there is variability in recommendations.
Although food insecurity affects a significant proportion of young children in New Zealand (NZ)(1), evidence of its association with dietary intake and sociodemographic characteristics in this population is lacking. This study aims to assess the household food security status of young NZ children and its association with energy and nutrient intake and sociodemographic factors. This study included 289 caregiver and child (1-3 years old) dyads from the same household in either Auckland, Wellington, or Dunedin, NZ. Household food security status was determined using a validated and NZ-specific eight-item questionnaire(2). Usual dietary intake was determined from two 24-hour food recalls, using the multiple source method(3). The prevalence of inadequate nutrient intake was assessed using the Estimated Average Requirement (EAR) cut-point method and full probability approach. Sociodemographic factors (i.e., socioeconomic status, ethnicity, caregiver education, employment status, household size and structure) were collected from questionnaires. Linear regression models were used to estimate associations with statistical significance set at p <0.05. Over 30% of participants had experienced food insecurity in the past 12 months. Of all eight indicator statements, “the variety of foods we are able to eat is limited by a lack of money,” had the highest proportion of participants responding “often” or “sometimes” (35.8%). Moderately food insecure children exhibited higher fat and saturated fat intakes, consuming 3.0 (0.2, 5.8) g/day more fat, and 2.0 (0.6, 3.5) g/day more saturated fat compared to food secure children (p<0.05). Severely food insecure children had lower g/kg/day protein intake compared to food secure children (p<0.05). In comparison to food secure children, moderately and severely food insecure children had lower fibre intake, consuming 1.6 (2.8, 0.3) g/day and 2.6 (4.0, 1.2) g/day less fibre, respectively. Severely food insecure children had the highest prevalence of inadequate calcium (7.0%) and vitamin C (9.3%) intakes, compared with food secure children [prevalence of inadequate intakes: calcium (2.3%) and vitamin C (2.8%)]. Household food insecurity was more common in those of Māori or Pacific ethnicity; living in areas of high deprivation; having a caregiver who was younger, not in paid employment, or had low educational attainment; living with ≥2 other children in the household; and living in a sole-parent household. Food insecure young NZ children consume a diet that exhibits lower nutritional quality in certain measures compared to their food-secure counterparts. Food insecurity was associated with various sociodemographic factors that are closely linked with poverty or low income. As such, there is an urgent need for poverty mitigation initiatives to safeguard vulnerable young children from the adverse consequences of food insecurity.
The aim of the article is to reframe speculation from being seen as synonymous with unacademic conjecture, or as a means for questioning consensus and established narratives, to becoming a productive practical engagement with the archaeological and responding to its intrinsic uncertainties. In the first part of the article, we offer a review of speculation in the history of archaeological reasoning. In the second part, we proceed to discussing ways of embracing the speculative mandate, referring back to our engagements with the art/archaeology project Ineligible and reflections on how to work with the unknowns and uncertainties of archaeology. In the third and last part, we conclude by making the case for fertilizing the archaeological potential nested in the empirical encounter, creating more inceptions than conclusions, fostering ambiguities, contradictions and new spaces of experiential inquiry. This leads us to suggest that—when working with the archaeological—speculation should be seen not only as a privilege, but also as an obligation, due to the inherent and inescapable uncertainties of the discipline. In other words, archaeology has been given a mandate for speculation through its material engagements.
The high-energy/high-intensity laser facility PHELIX of the GSI Helmholtzzentrum für Schwerionenforschung in Darmstadt, Germany, has been in operation since 2008. Here, we review the current system performance, which is the result of continuous development and further improvement. Through its versatile frontend architecture, PHELIX can be operated in both long- and short-pulse modes, corresponding to ns-pulses with up to 1 kJ pulse energy and sub-ps, 200 J pulses, respectively. In the short-pulse mode, the excellent temporal contrast and the control over the wavefront make PHELIX an ideal driver for secondary sources of high-energy ions, neutrons, electrons and X-rays. The long-pulse mode is mainly used for plasma heating, which can then be probed by the heavy-ion beam of the linear accelerator of GSI. In addition, PHELIX can now be used to generate X-rays for studying exotic states of matter created by heavy-ion heating using the ion beam of the heavy-ion synchrotron of GSI.
This study assesses change in caregiver practices after integrating responsive care and early learning (RCEL) in nutrition and health services and community platforms in northern Ghana.
Design:
We trained health facility workers and community health volunteers to deliver RCEL counselling to caregivers of children under 2 years of age through existing health facilities and community groups. We assessed changes in caregivers’ RCEL practices before and after the intervention with a household questionnaire and caregiver–child observations.
Setting:
The study took place in Sagnarigu, Gushegu, Wa East and Mamprugu-Moagduri districts from April 2022 to March 2023. Study sites included seventy-nine child welfare clinics (CWC) at Ghana Health Service facilities and eighty village savings and loan association (VSLA) groups.
Participants:
We enrolled 211 adult caregivers in the study sites who had children 0–23 months at baseline and were enrolled in a CWC or a VSLA.
Results:
We observed improvements in RCEL and infant and young child feeding practices, opportunities for early learning (e.g. access to books and playthings) in the home environment and reductions in parental stress.
Conclusions:
This study demonstrates the effectiveness of integrating RCEL content into existing nutrition and health services. The findings can be used to develop, enhance and advocate for policies integrating RCEL into existing services and platforms in Ghana. Future research may explore the relationship between positive changes in caregiver behaviour and improvements in child development outcomes as well as strategies for enhancing paternal engagement in care practices, improving child supervision and ensuring an enabling environment.
The Laboratoire de Mesure du Carbone 14 (LMC14) has operated a radiocarbon dating laboratory for almost twenty years with ARTEMIS, the Accelerator Mass Spectrometer (AMS) based on a NEC 9SDH-2 Pelletron tandem accelerator. A first status report describing the chemical pretreatment methods was published in 2017 (Dumoulin et al. 2017). This article summarizes updates of the routine procedures and presents new protocols. The quality checks in place at the LMC14 and results obtained for the GIRI international inter-comparison are reported. New protocols developed by the laboratory over the last five years are described with the preparation of iron, lead white, cellulose, calcium oxalate, and mortar. This report also provides a summary of practical information for sample preparation and can help the laboratory users who provide samples and publish results to better understand all the work behind a 14C dating.
Medical-legal partnerships connect legal advocates to healthcare providers and settings. Maintaining effectiveness of medical-legal partnerships and consistently identifying opportunities for innovation and adaptation takes intentionality and effort. In this paper, we discuss ways in which our use of data and quality improvement methods have facilitated advocacy at both patient (client) and population levels as we collectively pursue better, more equitable outcomes.
Female fertility is a complex trait with age-specific changes in spontaneous dizygotic (DZ) twinning and fertility. To elucidate factors regulating female fertility and infertility, we conducted a genome-wide association study (GWAS) on mothers of spontaneous DZ twins (MoDZT) versus controls (3273 cases, 24,009 controls). This is a follow-up study to the Australia/New Zealand (ANZ) component of that previously reported (Mbarek et al., 2016), with a sample size almost twice that of the entire discovery sample meta-analysed in the previous article (and five times the ANZ contribution to that), resulting from newly available additional genotyping and representing a significant increase in power. We compare analyses with and without male controls and show unequivocally that it is better to include male controls who have been screened for recent family history, than to use only female controls. Results from the SNP based GWAS identified four genomewide significant signals, including one novel region, ZFPM1 (Zinc Finger Protein, FOG Family Member 1), on chromosome 16. Previous signals near FSHB (Follicle Stimulating Hormone beta subunit) and SMAD3 (SMAD Family Member 3) were also replicated (Mbarek et al., 2016). We also ran the GWAS with a dominance model that identified a further locus ADRB2 on chr 5. These results have been contributed to the International Twinning Genetics Consortium for inclusion in the next GWAS meta-analysis (Mbarek et al., in press).
In 2001, five French public organizations (CNRS, CEA, IRD, IRSN, and the Ministère de la Culture) signed an agreement to purchase a new accelerator mass spectrometer to provide radiocarbon dating services at the national level. The Laboratoire de Mesure du Carbone 14 (LMC14) was set up in Saclay (France) around ARTEMIS, an AMS system based on a 3MV Pelletron from NEC and installed in early 2003. In 2015, the LMC14 joined the Laboratoire des Sciences du Climat et de l’Environnement, making it possible to develop research projects in addition to the service activity and since 2021, the LMC14 has been a member of the IAEA Collaborating Centre “Atoms for Heritage” at the Université Paris-Saclay. Since 2003, 70,000 samples have been measured. Two-thirds of the samples have been prepared on site and one-third in two associated laboratories in Paris and Lyon. Over the past years, the LMC14 has participated in several international inter-comparisons and has continuously improved its capabilities by developing new protocols for preparation and measurement. In this paper, the radiocarbon dating services of the last 20 years for research institutions, museums and environmental monitoring are reviewed and recent results from environmental and archaeological research programs are highlighted.
Sound general and sports nutrition knowledge in athletes is essential for making appropriate dietary choices. Assessment of nutrition knowledge enables evaluation and tailoring of nutrition education. However, few well-validated tools are available to assess nutrition knowledge in athletes. The objective of the present study was to establish the validity of the Platform to Evaluate Athlete Knowledge Sports – Nutrition Questionnaire (PEAKS-NQ) for use in the United Kingdom and Irish (UK-I) athletes. To confirm content validity, twenty-three sports nutritionists (SNs) from elite, UK-I sports institutes provided feedback on the PEAKS-NQ via a modified Delphi method. After minor changes, the UK-I version of the PEAKS-NQ was administered to UK-I SN from the British Dietetic Association Sport and Exercise Nutrition Register, and elite athletes (EA) training at elite sports institutes in the UK and Ireland. Independent samples t-test and independent samples median tests were used to compare PEAKS-NQ total and subsection scores between EA and SN (to assess construct validity). Cronbach's alpha (good ≥ 0⋅7) was used to establish internal consistency. The SN achieved greater overall [SN (n 23) 92⋅3 (9⋅3) v. EA (n 154): 71⋅4 (10⋅0)%; P < 0⋅001] and individual section scores (P < 0⋅001) except Section B, Identification of Food Groups (P = 0⋅07). Largest knowledge differences between SN and EA were in Section D, Applied Sports Nutrition [SN: 88⋅5 (8⋅9) v. EA: 56⋅7 (14⋅5)%; P < 0⋅00]. Overall ES was large (2⋅1), with subsections ranging from 0⋅6 to 2⋅3. Cronbach's alpha was good (0⋅83). The PEAKS-NQ had good content and construct validity, supporting its use to assess nutrition knowledge of UK-I athletes.
Estuaries and deltas are crucial zones to better understand the interactions between continents and oceans, and to characterize the mineralization and burial of different sources of organic matter (OM) and their effect on the carbon cycle. In the present study, we focus on the continental shelf of the northwest Mediterranean Sea near the Rhône river delta. Sediment cores were collected and pore waters were sampled at different depths at one station (Station E) located on this shelf. For each layer, measurements of dissolved inorganic carbon concentration (DIC) and its isotopic composition (δ13C and Δ14C) were conducted and a mixing model was applied to target the original signature of the mineralized OM. The calculated δ13C signature of the mineralized organic matter is in accordance with previous results with a δ13COM of marine origin that is not significantly impacted by the terrestrial particulate inputs from the river. The evolution with depth of Δ14C shows two different trends indicating two different Δ14C signatures for the mineralised OM. In the first 15 cm, the mineralized OM is modern with a Δ14COM = 100 ± 17‰ and corresponds to the OM produced during the nuclear period of the last 50 years. Deeper in the sediment, the result is very different with a depleted value Δ14COM = –172 ± 60‰ which corresponds to the pre-nuclear period. In these two cases, the marine substrate was under the influence of the local marine reservoir effect with more extreme Δ14C results. These differences can be largely explained by the influence of the river plume on the local marine DIC during these two periods.
Hydrodynamics and sediment processes at beach–inlet systems are dynamic and complicated. Beach–inlet systems are characteristic of mostly shallow and complicated bathymetry. As ocean waves propagate into shallow water with complex bathymetry, wave refraction, diffraction, shoaling, and breaking occur. The shallow water associated with the ebb tidal delta has significant influence on the pattern of wave propagation. Eventually in the vicinity of the shoreline and over the very shallow portions of the ebb tidal delta, waves break and generate intense turbulence that induce active sediment transport. Both wave and tide play significant roles in transporting sediments and causing morphology change at barrier–inlet systems. In general, wave-induced sediment transport dominates in areas far from the inlet where tidal currents tend to be weak. Within the deeper parts of inlet channels, tide-driven current constitutes the main mechanism for moving sediments. Over the ebb and flood tidal deltas, sediment movements are driven by both wave and current. This chapter reviews the above topics and commonly used equations on the hydrodynamics and sediment transport relevant to the beach–inlet system.
Although barrier islands occur under a variety of coastal settings, coasts with an ample supply of sand-sized sediment, a wide and gentle continental shelf, and a broad coastal plain are more conducive to the formation of barrier islands. When the above three conditions, combined with a slow sea-level rise rate of 1–3 mm/year, occur, barrier islands can be the dominant coastal features, such as along the US Gulf of Mexico and Atlantic Ocean coasts. Although not as common, barrier islands also occur along rocky coasts and river-delta coasts. This chapter discusses different morphologic and sedimentologic characteristics under different geologic and oceanographic settings. The various sub-environments, also referred to as morphologic features, that compose a barrier–inlet system are described, along with a morphodynamic classification of barrier island under different coastal settings. These morphologic features and the morphodynamic classification are used in the following chapters discussing sediment transport processes, sediment exchange among the different features and the associated pathways, and management of the sediment resources among the various morphologic features.
A beach–inlet system is composed of several sub-environments, including beach and nearshore, tidal inlet and ebb and flood tidal deltas, and coastal dunes. Building upon Chapter 2, this chapter discusses in detail the sedimentologic characteristics and morphodynamics of the various sub-environments composing a beach–inlet system. Commonly used concepts in quantifying beach morphology and its changes, including equilibrium beach profile, depth of closure, and the Bruun Rule, are reviewed. Coastal dunes and their morphodynamics are discussed in the context of beach–dune interaction. Morphologic and sedimentologic characteristics of tidal inlets and their associated ebb tidal delta and flood tidal delta are described in detail in terms of various morphology features. General patterns of sediment exchange for wave-dominated and mixed-energy beach–inlet systems are introduced.
Building upon regional scale discussions in Chapter 2, this chapter discusses the interactions between barrier beaches and tidal inlets at a local scale from the perspective of inlet stability, and mechanisms and pathways of sediment bypassing across tidal inlets. Inlet stability can be significantly influenced by local geologic conditions such as outcropping of erosion resistant bedrocks or stiff mud, in addition to hydraulic conditions as controlled by tidal prism. Local geology such as shoreline exposure of bedrocks and stiff mud can also influence beach morphodynamics by controlling its planform. However, tidal inlets and their ebb tidal deltas impose the major interruption to the continuity of longshore sand transport. How sand moving along the beach can reach from one barrier island to another constitutes the main issue for beach–inlet interaction, and subsequently the erosion or accretion of barrier beaches. Several conceptual models have been developed and are discussed in this chapter. The rapidly improving numerical modeling provides a promising tool to quantify sediment bypassing and is introduced here.
The concept and application of resilience have been significantly expanded in the last three decades and the term is being used more and more broadly to represent a large-scale multi-disciplinary and comprehensive approach to both natural and human-related coastal issues associated with rising sea level, increased storm frequency and intensity, and human stressors. This chapter reviews the relevant findings from the recent global climate-change reports and introduces the resilience of barrier–inlet systems. In terms of the natural system, the survival of the very landform under the condition of accelerating sea-level rise is discussed via a conceptual model or a couple of numerical models. The resiliency of the human–natural barrier–inlet environment is far more complicated than just the natural system. The concepts and complicated framework outlined in the recent NRC (National Research Council) and USGCRP (US Global Climate Research Program) reports are reviewed, and illustrated with two case studies.
Prior to the 1950s, general shore-protection practice was to use hard structures to protect against beach erosion or storm damage. Generally, the hard structures can be divided into two categories. The first category functions through anchoring the position of either a shoreline or a dune-line, such as seawalls and revetments. The second category is mainly sand-trapping structures such as groins and detached breakwaters. Realizing that the accumulation of sand produced by a structure is at the expense of an adjacent section of the shore, since the 1970s, 90% of the US Federal appropriation for shore protection has been for beach nourishment. Although beach and dune nourishment has become by far the most dominant approach to shore protection, principles of hard engineering structures are still reviewed in this chapter. More recently, since the 2010s, Engineering with Nature (EWN), defined as the intentional alignment of natural and engineering processes to efficiently and sustainably deliver economic, environmental, and social benefits through collaborative processes, are being promoted and applied more and more. The concept and practice of EWN are introduced in this chapter.