A beryllium-10 chronology of late-glacial moraines in the upper Rakaia valley, Southern Alps, New Zealand supports Southern- Hemisphere warming during the Younger Dryas

Interhemispheric differences in the timing of pauses or reversals in the temperature rise at the end of the last ice age can help to clarify the mechanisms that influence glacial terminations. Our beryllium-10 (10Be) surface-exposure chronology for the moraines of the upper Rakaia valley of New Zealand's Southern Alps, combined with glaciological modeling, show that late-glacial temperature change in the atmosphere over the Southern Alps exhibited an Antarctic-like pattern. During the Antarctic Cold Reversal, the upper Rakaia glacier built two well-defined, closely-spaced moraines on Reischek knob at 13,900 ± 120 [1σ; ± 310 yrs when including a 2.1% production-rate (PR) uncertainty] and 13,140 ± 250 (±370) yrs ago, in positions consistent with mean annual temperature approximately 2 °C cooler than modern values. The formation of distinct, widely-spaced moraines at 12,140 ± 200 (±320) and 11,620 ± 160 (±290) yrs ago on Meins Knob, 2 km up-valley from the Reischek knob moraines, indicates that the glacier thinned by ∼250 m during Heinrich Stadial 0 (HS 0, coeval with the Younger Dryas 12,900 to 11,600 yrs ago). The glacier-inferred temperature rise in the upper Rakaia valley during HS 0 was about 1 °C. Because a similar pattern is documented by well-dated glacial geomorphologic records from the Andes of South America, the implication is that this late-glacial atmospheric climate signal extended from 79°S north to at least 36°S, and thus was a major feature of Southern Hemisphere paleoclimate during the last glacial termination

An empirical study of normative dissociation in musical and non-musical everyday life experiences

Dissociative experiences involving music have received little research attention outside the field of ethnomusicology. This paper examines the psychological characteristics of normative dissociation (detachment) across musical and non-musical experiences in ‘real world’, everyday settings. It draws upon a subset of data arising from an empirical project designed to compare transformative shifts of consciousness, with and without music in daily life, and the ways in which use of music may facilitate the processes of dissociation and absorption. Twenty participants kept unstructured diaries for two weeks, recording free descriptions of involving experiences of any kind as soon as possible after their occurrence. All descriptions were subsequently subjected to Interpretative Phenomenological Analysis (IPA). Results suggest that dissociative experiences are a familiar occurrence in everyday life. Diary entries highlight an established practice of actively sought detachment from self, surroundings or activity, suggesting that, together with absorption, the processes of derealization (altered perception of surroundings) and depersonalization (detachment from self) constitute common means of selfregulation in daily life. Music emerges as a particularly versatile facilitator of dissociative experience because of its semantic ambiguity, portability, and the variety of ways in which it may mediate perception, so facilitating an altered relationship to self and environmen

Correspondence Among Mid-Latitude Glacier Equilibrium Line Altitudes, Atmospheric Temperatures, and Westerly Wind Fields

Mountain glaciers are highly sensitive to climate change. However, the extent to which glaciers capture regional to hemisphere-scale atmospheric processes remains uncertain, hindering paleoclimatic interpretations derived from moraine-based glacier reconstructions. Here, we evaluate how mid-latitude glacier systems monitor climate by comparing climate reanalysis products with glacier annual equilibrium line altitude (ELA) elevations from the antipodal Southern Alps of New Zealand and European Alps. We find significant regional and hemispheric correlations between glacier annual ELA and summer tropospheric temperatures. Annual ELA also exhibit positive correlations with the latitude of the westerly jets in both hemispheres. These results indicate that westerly wind-belt latitude modulates the proportion of cold versus warm air masses influencing these glacier systems. These results highlight the sensitivity of mid-latitude glaciers to atmospheric temperatures and circulation, with implications for interpreting moraine-based paleoclimate reconstructions. Combined impacts of ongoing tropospheric warming and poleward-shifting westerlies will likely accelerate recession of mid-latitude glaciers. © 2022. The Authors.Open access articleThis item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at [email protected]

Potencial alelopático de plantas de acapu (Vouacapoua americana): efeitos sobre plantas daninhas de pastagens Allelopathic potential of "acapu" (Vouacapoua americana) plants: effects on pasture weed

Extratos aquosos de folhas e cascas de plantas de acapu (Vouacapoua americana) foram preparados nas concentrações de 0, 1, 2, 3 e 5% (v/v), visando identificar e caracterizar a atividade potencialmente alelopática dessa espécie. Analisaram-se os efeitos dos extratos sobre a germinação de sementes e o alongamento da raiz primária das plantas daninhas malícia (Mimosa pudica) e malva (Urena lobata). Os bioensaios de germinação foram desenvolvidos em condições de 25 ºC e fotoperíodo de 12 horas. Para os bioensaios de alongamento da raiz primária, as condições estabelecidas foram de 25 ºC e fotoperíodo de 24 horas. Os resultados obtidos indicaram variações de respostas em função da fonte do extrato aquoso, do parâmetro analisado e da concentração do extrato. As reduções observadas tanto na germinação como no alongamento da raiz primária foram crescentes com o aumento da concentração do extrato, sendo os efeitos mais intensos observados na concentração de 5%. Independentemente da espécie receptora e do parâmetro analisado, o extrato preparado a partir das cascas do acapu evidenciou maior atividade alelopática inibitória. O alongamento da raiz primária foi o parâmetro mais sensível aos efeitos potencialmente alelopáticos do que a germinação das sementes. Comparativamente, cascas e folhas apresentaram diferenças em relação às classes de substâncias químicas. Nas cascas foram encontradas cumarinas que não estavam presentes nas folhas, as quais, por sua vez, apresentaram esteróides e triterpenóides, que não foram identificados nas cascas do acapu.<br>Aqueous extracts from leaves and bark of "Acapu" plants were prepared in concentration levels of 0, 1, 2, 3 and 5% to identify and characterize potential allelopathic activity of such plants. The extract effects on seed germination and primary root elongation of pasture weeds, such as Mimosa pudica and Urena lobata, were analyzed. The germination bioassays were developed under 25 ºC and a photoperiod of 12 hours. For the primary root elongation, the bioassay conditions were 25 ºC and photoperiod of 24 hours. The results indicated a variation in response, according to the source of aqueous extract, the analyzed parameter and the extract concentration. The reductions observed both in germination and primary root elongation increased with the increase of extract concentration. The most intense effects were observed at an extract concentration level of 5%. Regardless of the receiving species and the analyzed parameter, the extract prepared from the bark showed greater inhibiting allelopathic activity. The parameter primary root elongation was more sensitive to the potential allelopathic effects than seed germination. Comparatively, bark and leaves showed differences in relation to the chemical compound classes. Cumarins were identified in the bark but not in the leaves, while steroids and triterpenoids were observed in the leaves but not in the bark

Warming and glacier recession in the Rakaia valley, Southern Alps of New Zealand, during Heinrich Stadial 1

The termination of the last ice age featured a major reconfiguration of Earthʼs climate and cryosphere, yet the underlying causes of these massive changes continue to be debated. Documenting the spatial and temporal variations of atmospheric temperature during deglaciation can help discriminate among potential drivers. Here, we present a 10Be surface-exposure chronology and glaciological reconstruction of ice recession following the Last Glacial Maximum (LGM) in the Rakaia valley, Southern Alps of New Zealand. Innermost LGM moraines at Big Ben have an age of 17,840 ± 240 yrs, whereas ice-marginal moraines or ice-molded bedrock surfaces at distances up-valley from Big Ben of 12.5 km (Lake Coleridge), ∼25 km (Castle Hill), ∼28 km (Double Hill), ∼43 km (Prospect Hill), and ∼58 km (Reischek knob) have ages of 17,020 ± 70 yrs, 17,100 ± 110 yrs, 16,960 ± 370 yrs, 16,250 ± 340 yrs, and 15,660 ± 160 yrs, respectively. These results indicate extensive recession of the Rakaia glacier, which we attribute primarily to the effects of climatic warming. In conjunction with geomorphological maps and a glaciological reconstruction for the Rakaia valley, we use our chronology to infer timing and magnitude of past atmospheric temperature changes. Compared to an overall temperature rise of ∼4.65 °C between the end of the LGM and the start of the Holocene, the glacier recession between ∼17,840 and ∼15,660 yrs ago is attributable to a net temperature increase of ∼4.0 °C (from −6.25 to −2.25 °C), accounting for ∼86% of the overall warming. Approximately 3.75 °C (∼70%) of the warming occurred between ∼17,840 and ∼16,250 yrs ago, with a further 0.75 °C (∼16%) increase between ∼16,250 and ∼15,660 yrs ago. A sustained southward shift of the Subtropical Front (STF) south of Australia between ∼17,800 and ∼16,000 yrs ago coincides with the warming over the Rakaia valley, and suggests a close link between Southern Ocean frontal boundary positions and southern mid-latitude climate. Most of the deglacial warming in the Southern Alps occurred during the early part of Heinrich Stadial 1 (HS1) of the North Atlantic region. Because the STF is associated with the position of the westerly wind belt, our findings support the concept that a southward shift of Earthʼs wind belts accompanied the early part of HS1 cooling in the North Atlantic, leading to warming and deglaciation in southern middle latitudes