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This book considers how Samoans embraced and reshaped the English game of cricket, recasting it as a distinctively Samoan pastime, kirikiti. Starting with cricket's introduction to the islands in 1879, it uses both cricket and kirikiti to trace six decades of contest between and within the categories of 'colonisers' and 'colonised.' How and why did Samoans adapt and appropriate the imperial game? How did officials, missionaries, colonists, soldiers and those with mixed foreign and Samoan heritage understand and respond to the real and symbolic challenges kirikiti presented? And how did Samoans use both games to navigate foreign colonialism(s)? By investigating these questions, Benjamin Sacks suggests alternative frameworks for conceptualising sporting transfer and adoption, and advances understandings of how power, politics and identity were manifested through sport, in Samoa and across the globe.

Double strike: two linked earthquakes caused 2009 South Pacific tsunami The tsunami that struck the Samoan and northern Tongan islands in September 2009 was preceded by a magnitude-8 earthquake on the outer slope of the oceanic trench, where the Pacific plate bends as it enters the subduction zone. This was initially thought to be the sole source of the tsunami, but a more complex picture is emerging. Two groups report the occurrence of two earthquakes, a 'triggered doublet', at nearly the same time and place. What is not clear is which triggered the other. Beavan et al . use an analysis of Global Positioning System station displacements and tsunami models to show that the outer-rise earthquake was accompanied — possibly triggered by — a near-simultaneous mega-thrust earthquake in the adjacent Tonga subduction zone. Lay et al . analyse the available seismic data, and their model suggests that the outer-rise event triggered megathrust faulting. Either way, this dual strike suggests a mechanism for the occasional large tsunamis generated at the Tonga subduction zone. On 29 September 2009, a tsunami devastated the Samoan and northern Tongan islands. Here, an unusual earthquake sequence that preceded this tsunami is analysed. A magnitude-8.1 intraplate faulting event in the outer trench-slope at the northern end of the Tongan subduction zone was followed by extensive interplate faulting, with total moment equivalent to that of a magnitude-8.0 earthquake. Overlap of the seismic signals had obscured the fact that distinct faults had ruptured with different geometries. Great earthquakes (having seismic magnitudes of at least 8) usually involve abrupt sliding of rock masses at a boundary between tectonic plates. Such interplate ruptures produce dynamic and static stress changes that can activate nearby intraplate aftershocks, as is commonly observed in the trench-slope region seaward of a great subduction zone thrust event 1 , 2 , 3 , 4 . The earthquake sequence addressed here involves a rare instance in which a great trench-slope intraplate earthquake triggered extensive interplate faulting, reversing the typical pattern and broadly expanding the seismic and tsunami hazard. On 29 September 2009, within two minutes of the initiation of a normal faulting event with moment magnitude 8.1 in the outer trench-slope at the northern end of the Tonga subduction zone, two major interplate underthrusting subevents (both with moment magnitude 7.8), with total moment equal to a second great earthquake of moment magnitude 8.0, ruptured the nearby subduction zone megathrust. The collective faulting produced tsunami waves with localized regions of about 12 metres run-up that claimed 192 lives in Samoa, American Samoa and Tonga. Overlap of the seismic signals obscured the fact that distinct faults separated by more than 50 km had ruptured with different geometries, with the triggered thrust faulting only being revealed by detailed seismic wave analyses. Extensive interplate and intraplate aftershock activity was activated over a large region of the northern Tonga subduction zone.

By contrast, the World Bank lists the Independent State of Samoa as a low TB incidence jurisdiction with a reported TB incidence rate of 6.8 in 2021, comparable to that of New Zealand. Unlike the common rectangular domiciliary and institutional structures found in other Pacific Island groups and introduced to the Samoan Islands by the Europeans in the 19th century, often with airtight or insulated building shells, the traditional fale both lacking walls and being buffeted consistently by wind would provide housing space that was naturally ventilated and cooled. Recent World Health Organization estimates for the many Pacific Island jurisdictions show a wide range of TB incidence, no doubt the results of a multiplicity of factors; however, few Pacific Island jurisdictions report low TB incidence rates comparable to those of the Samoas (e.g., Tonga and the Cook Islands, both of which have near omnipresent wind similar to that in the Samoas and traditionally have had open and airy domestic architecture made of bamboo, wood, and palm fronds, with walls often omitted to enable easy passage of the trade winds in an extremely humid environment). The combination of trade winds and relatively wall-less domestic architecture has been by no means the sole contributor to the lower rates of TB in the Samoas compared with Pacific Island groups elsewhere in Polynesia and in Micronesia and Melanesia, which have differing environmental conditions, demographics, and traditional architecture that more customarily had a greater presence of walls.

Ecological restoration of forests, meadows, reefs, or other foundational ecosystems during climate change depends on the discovery and use of individuals able to withstand future conditions. For coral reefs, climate-tolerant corals might not remain tolerant in different environments because of widespread environmental adjustment of coral physiology and symbionts. Here, we test if parent corals retain their heat tolerance in nursery settings, if simple proxies predict successful colonies, and if heat-tolerant corals suffer lower growth or survival in normal settings. Before the 2015 natural bleaching event in American Samoa, we set out 800 coral fragments from 80 colonies of four species selected by prior tests to have a range of intraspecific natural heat tolerance. After the event, nursery stock from heat-tolerant parents showed two to three times less bleaching across species than nursery stock from less tolerant parents. They also retained higher individual genetic diversity through the bleaching event than did less heat-tolerant corals. The three best proxies for thermal tolerance were response to experimental heat stress, location on the reef, and thermal microclimate. Molecular biomarkers were also predictive but were highly species specific. Colony geno-type and symbiont genus played a similarly strong role in predicting bleaching. Combined, our results show that selecting for host and symbiont resilience produced a multispecies coral nursery that withstood multiple bleaching events, that proxies for thermal tolerance in restoration can work across species and be inexpensive, and that different coral clones within species reacted very differently to bleaching.

Here is your chance to get right off the tourism grid in the Polynesian Isles, with a full-colour planning section; guide to travel with children; chapters full of tips for families; inspirational image gallery, and more.

Multiplex bead immunoassays (MBA) can detect antibody responses to multiple antigens. Using MBA data from the Surveillance and Monitoring to Eliminate Lymphatic Filariasis (LF) and Scabies from Samoa (SaMELFS) 2018, we aim to estimate national seroprevalence of neglected tropical diseases (NTDs), vaccine-preventable diseases (VPDs), and arboviruses in Samoa. A community-based serosurvey of 3851 participants aged ≥ 5 years in 35 primary sampling units (PSUs). Using MBA, dried blood spots were assayed for antibodies (Ab) from 10 pathogens: LF, trachoma, yaws, tetanus, diphtheria, rubella, measles, dengue, Zika, and chikungunya. Seroprevalence was adjusted for study design, age, and gender. NTD seroprevalence for LF was 50.8% ( Bm33 Ab), 32.0% ( Wb123 Ab), 20.3% ( Bm14 Ab); 5.5% for trachoma; and 1.0% ( Tmpa Ab) and 0.2% ( Rp17 Ab) for yaws. VPD seroprevalence was 91.0% for tetanus, 83.5% for diphtheria, 79.0% for rubella, and 43.6% for measles. Arbovirus seroprevalence for dengue was 91.1% (dengue virus serotype-1 [DENV-1]), 97.2% (DENV-2), 96.9% (DENV-3), 94.7% (DENV-4); 85.7% for Zika; and 57.0% for chikungunya. Increasing age was associated with seropositivity to NTDs, arboviruses, tetanus, and measles. Clustering was highest at the household level; the strongest clustering was for DENV-3 (intraclass correlation coefficient [ICC]:0.32), Bm33 Ab (ICC:0.31), and Bm14 Ab (ICC:0.31). Integrated serosurveillance can provide a comprehensive picture of population-level immunity to multiple diseases. Our investigation into associations with seroprevalence can aid the development of evidence-based prevention, control, and elimination strategies.

Recent advances in DNA-sequencing technologies now allow for in-depth characterization of the genomic stress responses of many organisms beyond model taxa. They are especially appropriate for organisms such as reef-building corals, for which dramatic declines in abundance are expected to worsen as anthropogenic climate change intensifies. Different corals differ substantially in physiological resilience to environmental stress, but the molecular mechanisms behind enhanced coral resilience remain unclear. Here, we compare transcriptome-wide gene expression (via RNA-Seq using Illumina sequencing) among conspecific thermally sensitive and thermally resilient corals to identify the molecular pathways contributing to coral resilience. Under simulated bleaching stress, sensitive and resilient corals change expression of hundreds of genes, but the resilient corals had higher expression under control conditions across 60 of these genes. These “frontloaded” transcripts were less up-regulated in resilient corals during heat stress and included thermal tolerance genes such as heat shock proteins and antioxidant enzymes, as well as a broad array of genes involved in apoptosis regulation, tumor suppression, innate immune response, and cell adhesion. We propose that constitutive frontloading enables an individual to maintain physiological resilience during frequently encountered environmental stress, an idea that has strong parallels in model systems such as yeast. Our study provides broad insight into the fundamental cellular processes responsible for enhanced stress tolerances that may enable some organisms to better persist into the future in an era of global climate change.

New tungsten isotope data for modern ocean island basalts (OIB) from Hawaii, Samoa, and Iceland reveal variable 182W/184W, ranging from that of the ambient upper mantle to ratios as much as 18 parts per million lower. The tungsten isotopic data negatively correlate with ³He/⁴He. These data indicate that each OIB system accesses domains within Earth that formed within the first 60 million years of solar system history. Combined isotopic and chemical characteristics projected for these ancient domains indicate that they contain metal and are repositories of noble gases. We suggest that the most likely source candidates are mega–ultralow-velocity zones, which lie beneath Hawaii, Samoa, and Iceland but not beneath hot spots whose OIB yield normal 182W and homogeneously low ³He/⁴He.