On climate change and cultural geography: farming on the Lizard Peninsula, Cornwall, UK

Climate change as a global problem has moved relatively swiftly into high profile political debates over the last 20 years or so, with a concomitant diffusion from the natural sciences into the social sciences. The study of the human dimensions of climate change has been growing in momentum through research which attempts to describe, evaluate, quantify and model perceptions of climate change, understand more about risk and assess the construction of policy. Cultural geographers’ concerns with the construction of knowledge, the workings of social relations in space and the politics and poetics of place-based identities provide a lens through which personal, collective and institutional responses to climate change can be evaluated using critical and interpretative methodologies. Adopting a cultural geography approach, this paper examines how climate change as a particular environmental discourse is constructed through memory, observation and conversation, as well as materialised in farming practices on the Lizard Peninsula, Cornwall, UK

Anticipatory objects and uncertain imminence: cattle grids, landscape and the presencing of climate change on the Lizard Peninsula, UK

In this paper we show how a seemingly unremarkable object – a cattle grid – has come to presence climate change in partial and contingent ways on the Lizard Peninsula, Cornwall, UK. We identify the cattle grid as an ‘anticipatory object’ through which conservation organisations seek to manage the future and adapt to climate change, but which at the same time presences that unthought-of future for others in the landscape. We explore the ways in which the cattle grid acts to presence something that is not only absent – climate change – but has uncertain imminence. We investigate the ways in which the cattle grid make climate relevant as an embodied and experiential process, a physical and intellectual artefact, and the means to imagine climate and the ways it might change. Drawing upon interpretative approaches informed by theorisations of materiality, presence and absence to understand climate change as a social phenomenon, we go beyond a consideration of this ordinary object defined by its function to consider how the object is experienced, the processes and practices through which people relate to it, and the ways in which social meaning accumulates around it. The empirical basis for this argument is provided by in-depth interviews with local representatives of Natural England, residents and farmers.

Ice-stream initiation, duration and thinning on James Ross Island, northern Antarctic Peninsula

Predicting the future response of the Antarctic Ice Sheet to climate change requires an understanding of the ice streams that dominate its dynamics. Here we use cosmogenic isotope exposure-age dating (26Al, 10Be and 36Cl) of erratic boulders on ice-free land on James Ross Island, north-eastern Antarctic Peninsula, to define the evolution of Last Glacial Maximum (LGM) ice in the adjacent Prince Gustav Channel. These data include ice-sheet extent, thickness and dynamical behaviour. Prior to ∼18 ka, the LGM Antarctic Peninsula Ice Sheet extended to the continental shelf-edge and transported erratic boulders onto high-elevation mesas on James Ross Island. After ∼18 ka there was a period of rapid ice-sheet surface-lowering, coincident with the initiation of the Prince Gustav Ice Stream. This timing coincided with rapid increases in atmospheric temperature and eustatic sea-level rise around the Antarctic Peninsula. Collectively, these data provide evidence for a transition from a thick, cold-based LGM Antarctic Peninsula Ice Sheet to a thinner, partially warm-based ice sheet during deglaciation.

Landscape evolution and ice-sheet behaviour in a semi-arid polar environment: James Ross Island, NE Antarctic Peninsula

This study of landscape evolution presents both new modern and palaeo process-landform data, and analyses the behaviour of the Antarctic Peninsula Ice Sheet through the Last Glacial Maximum (LGM), the Holocene and to the present day. Six sediment-landform assemblages are described and interpreted for Ulu Peninsula, James Ross Island, NE Antarctic Peninsula: (1) the Glacier Ice and Snow Assemblage; (2) the Glacigenic Assemblage, which relates to LGM sediments and comprises both erratic-poor and erratic-rich drift, deposited by cold-based and wet-based ice and ice streams respectively; (3) the Boulder Train Assemblage, deposited during a Mid-Holocene glacier readvance; (4) the Ice-cored Moraine Assemblage, found in front of small cirque glaciers; (5) the Paraglacial Assemblage including scree, pebble-boulder lags, and littoral and fluvial processes; and (6) the Periglacial Assemblage including rock glaciers, protalus ramparts, blockfields, solifluction lobes and extensive patterned ground. The interplay between glacial, paraglacial and periglacial processes in this semi-arid polar environment is important in understanding polygenetic landforms. Crucially, cold-based ice was capable of sediment and landform genesis and modification. This landsystem model can aid the interpretation of past environments, but also provides new data to aid the reconstruction of the last ice sheet to overrun James Ross Island.

Antarctic Peninsula ice sheet evolution during the Cenozoic Era

The Antarctic Peninsula region is currently undergoing rapid environmental change, resulting in the thinning, acceleration and recession of glaciers and the sequential collapse of ice shelves. It is important to view these changes in the context of long-term palaeoenvironmental complexity and to understand the key processes controlling ice sheet growth and recession. In addition, numerical ice sheet models require detailed geological data for tuning and testing. Therefore, this paper systematically and holistically reviews published geological evidence for Antarctic Peninsula Ice Sheet variability for each key locality throughout the Cenozoic, and brings together the prevailing consensus of the extent, character and behaviour of the glaciations of the Antarctic Peninsula region. Major contributions include a downloadable database of 186 terrestrial and marine calibrated dates; an original reconstruction of the LGM ice sheet; and a new series of isochrones detailing ice sheet retreat following the LGM. Glaciation of Antarctica was initiated around the Eocene/Oligocene transition in East Antarctica. Palaeogene records of Antarctic Peninsula glaciation are primarily restricted to King George Island, where glacigenic sediments provide a record of early East Antarctic glaciations, but with modification of far-travelled erratics by local South Shetland Island ice caps. Evidence for Neogene glaciation is derived primarily from King George Island and James Ross Island, where glaciovolcanic strata indicate that ice thicknesses reached 500–850 m during glacials. This suggests that the Antarctic Peninsula Ice Sheet draped, rather than drowned, the topography. Marine geophysical investigations indicate multiple ice sheet advances during this time. Seismic profiling of continental shelf-slope deposits indicates up to ten large advances of the Antarctic Peninsula Ice Sheet during the Early Pleistocene, when the ice sheet was dominated by 40 kyr cycles. Glacials became more pronounced, reaching the continental shelf edge, and of longer duration during the Middle Pleistocene. During the Late Pleistocene, repeated glacials reached the shelf edge, but ice shelves inhibited iceberg rafting. The Last Glacial Maximum (LGM) occurred at 18 ka BP, after which transitional glaciomarine sediments on the continental shelf indicate ice-sheet retreat. The continental shelf contains large bathymetric troughs, which were repeatedly occupied by large ice streams during Pleistocene glaciations. Retreat after the LGM was episodic in the Weddell Sea, with multiple readvances and changes in ice-flow direction, but rapid in the Bellingshausen Sea. The late Holocene Epoch was characterised by repeated fluctuations in palaeoenvironmental conditions, with associated glacial readvances. However, this has been subsumed by rapid warming and ice-shelf collapse during the twentieth century.

Mid-Holocene land-surface conditions in northern Africa and the Arabian peninsula: a data set for the analysis of biogeophysical feedbacks in the climate system

Large changes in the extent of northern subtropical arid regions during the Holocene are attributed to orbitally forced variations in monsoon strength and have been implicated in the regulation of atmospheric trace gas concentrations on millenial timescales. Models that omit biogeophysical feedback, however, are unable to account for the full magnitude of African monsoon amplification and extension during the early to middle Holocene (˜9500–5000 years B.P.). A data set describing land-surface conditions 6000 years B.P. on a 1° × 1° grid across northern Africa and the Arabian Peninsula has been prepared from published maps and other sources of palaeoenvironmental data, with the primary aim of providing a realistic lower boundary condition for atmospheric general circulation model experiments similar to those performed in the Palaeoclimate Modelling Intercomparison Project. The data set includes information on the percentage of each grid cell occupied by specific vegetation types (steppe, savanna, xerophytic woods/scrub, tropical deciduous forest, and tropical montane evergreen forest), open water (lakes), and wetlands, plus information on the flow direction of major drainage channels for use in large-scale palaeohydrological modeling.

The greening of Arabia: multiple opportunities for human occupation of the Arabian peninsula during the Late Pleistocene inferred from an ensemble of climate model simulations

Climate models are potentially useful tools for addressing human dispersals and demographic change. The Arabian Peninsula is becoming increasingly significant in the story of human dispersals out of Africa during the Late Pleistocene. Although characterised largely by arid environments today, emerging climate records indicate that the peninsula was wetter many times in the past, suggesting that the region may have been inhabited considerably more than hitherto thought. Explaining the origins and spatial distribution of increased rainfall is challenging because palaeoenvironmental research in the region is in an early developmental stage. We address environmental oscillations by assembling and analysing an ensemble of five global climate models (CCSM3, COSMOS, HadCM3, KCM, and NorESM). We focus on precipitation, as the variable is key for the development of lakes, rivers and savannas. The climate models generated here were compared with published palaeoenvironmental data such as palaeolakes, speleothems and alluvial fan records as a means of validation. All five models showed, to varying degrees, that the Arabia Peninsula was significantly wetter than today during the Last Interglacial (130 ka and 126/125 ka timeslices), and that the main source of increased rainfall was from the North African summer monsoon rather than the Indian Ocean monsoon or from Mediterranean climate patterns. Where available, 104 ka (MIS 5c), 56 ka (early MIS 3) and 21 ka (LGM) timeslices showed rainfall was present but not as extensive as during the Last Interglacial. The results favour the hypothesis that humans potentially moved out of Africa and into Arabia on multiple occasions during pluvial phases of the Late Pleistocene.

Population structure and sexual maturity of the calico box crab Hepatus epheliticus Linnaeus (Brachyura, Hepatidae) from Yucatan Peninsula, Mexico

The calico box crab Hepatus epheliticus is an abundant species from shallow and continental shelf waters of the Atlantic coast of USA and Mexico. Information about population structure and sexual maturity is absent, even though this crab is caught to be used as bait for the octopus fishery in the Campeche Bank, Mexico. In order to achieve such information, a total of 768 individuals were collected from January to March 2010 through baited traps installed in the Yucatan Peninsula, Mexico. Our results showed that sex ratio is biased towards more males than females (1:0.55), contradicting to that reported in other brachyuran crabs. The absence of ovigerous females suggests that they did not enter into the traps during embryogenesis. Males reached a larger maximum size than females (64.0 +/- 6.15 and 58.4 +/- 5.60 mm carapace width, respectively). The general scheme of growth being positive allometric throughout ontogeny of both sexes. Males presented a transition phase from juveniles to adult corresponding to the puberty moult. The estimation of the onset of functional sexual maturity revealed a steady situation for the population, with 21.5 and 13.8% of males and females, respectively, morphologically immature at the time of catch. This study constitutes the first report on population structure and sexual maturity in a population of the calico box crab H. epheliticus.

Efeitos do ethephon sobre a produção da uva 'Niagara Rosada' (Vitis labrusca L.), produzida na entressafra na região de Jales-SP

A produção de 'Niagara Rosada' na entressafra, embora sendo uma excelente opção para os viticultores de Jales-SP, é problemática devido à dificuldade de emissão e desenvolvimento das brotações após a poda, realizada nos meses de ocorrência de temperaturas inferiores a 10ºC, o que tem causado pequenas produções e desestímulo entre os viticultores. Visando a solucionar este problema, foram conduzidos seis experimentos nos anos de 2001 e 2002, cujo objetivo foi verificar o efeito do ethephon aplicado antes da poda sobre o número de cachos, a produção e a qualidade da uva. Foram testadas as doses 0; 3; 6 e 9L.ha-1 de ethephon aplicado via foliar. Concluiu-se que o uso de ethephon proporcionou aumento do número de cachos e da produtividade de 'Niagara Rosada', especialmente quando da ocorrência de condições climáticas desfavoráveis e com satisfatório grau de enfolhamento. A utilização de ethephon na dose de 9L.ha-1 proporcionou aumento da produtividade da uva 'Niagara Rosada' na entressafra.

Efeito do ethephon na qualidade da uva 'Niagara Rosada' (Vitis labrusca L.), produzida na entressafra, na região de Jales-SP

Na região de Jales (SP), a produção de uva 'Niagara Rosada' obtida de videiras podadas em períodos de ocorrência de baixas temperaturas é, em geral, insatisfatória, apresentando pequena produtividade e cachos com qualidade inadequada à comercialização. Essa qualidade da produção está intimamente relacionada à efetiva brotação. Assim, este trabalho teve o objetivo de avaliar a aplicação do ethephon em diferentes doses antes da poda, visando a melhorar a brotação e a qualidade dos cachos, em seis experimentos, durante os anos de 2001 e 2002. Foram testadas as doses de 0; 3; 6 e 9 L.ha-1 de ethephon aplicado via foliar. Concluiu-se que o uso de ethephon, na dose de 9 L.ha-1, proporcionou cachos e bagas maiores e com maiores pesos, comprimento e largura, melhorando o aspecto dos mesmos. A aplicação de ethephon não afetou os teores de sólidos solúveis totais e a acidez total titulável, não alterando o sabor da uva 'Niagara Rosada'.

Efeito do ethephon sobre a brotação e vigor dos ramos da videira 'Niagara Rosada' (Vitis labrusca L.)

A produção da videira 'Niagara Rosada' em regiões tropicais e subtropicais do Brasil tem sido freqüentemente prejudicada, principalmente devido à dificuldade de emissão e desenvolvimento das brotações após a poda de produção, realizada nos meses de ocorrência de temperaturas mais baixas, o que tem causado redução nas produções e desestímulo aos viticultores. Para solucionar esse problema, foram conduzidos três experimentos, em pomares comerciais localizados na região Noroeste do Estado de São Paulo, com o objetivo de estudar o efeito do Ethephon, aplicado antes da poda de produção, na emissão e desenvolvimento das novas brotações e na duração do período da poda até a floração. Foram testadas quatro doses de ethephon (0 mg.L-1; 720 mg.L-1; 1.440 mg.L-1; 2.160 mg.L-1) aplicadas via foliar antes da poda de produção, nos meses de junho e julho de 2002. Observou-se que a aplicação de Ethephon proporcionou maior número de gemas brotadas, maior comprimento e diâmetro do ramo e não alterou o período da poda à floração. Especialmente quando da ocorrência de condições climáticas desfavoráveis e quando as plantas apresentaram satisfatório grau de enfolhamento, a aplicação de ethephon, na dose de 2.160 mg.L-1, foi a mais efetiva.

Características físicas e acúmulo de nutrientes pelos cachos de 'niagara rosada' em vinhedos na região de Jundiaí

Este trabalho teve por objetivo realizar um levantamento em 40 vinhedos de 'Niagara Rosada' nos municípios de Jundiaí e Louveira-SP, sendo metade sobre o porta-enxerto 'Ripária do Traviú' e outra sobre o 'IAC 766'. Determinaram-se, em cada vinhedo, a produtividade, a duração do ciclo, o número de cachos e de ramos produtivos por planta, as características físicas dos cachos e bagas, e o acúmulo de nutrientes pelos cachos. Avaliaram-se nos cachos amostrados a massa da matéria fresca, o comprimento e a largura dos cachos e baga, e diâmetro do pedicelo. Os cachos de cada vinhedo amostrado foram secos em estufa e posteriormente submetidos à análise química para determinar os teores de macro e micronutrientes, visando a estimar o acúmulo de nutrientes por tonelada de uva. Constatou-se um comportamento semelhante entre os porta-enxertos para os dados de produtividade, duração do ciclo, número de cachos e ramos produtivos, sendo de, respectivamente, 11.100kg ha-1, 134 dias, 13 cachos e 9 ramos produtivos. Quanto às características físicas, os valores médios da massa da matéria fresca, comprimento e largura dos cachos foram de, respectivamente, 209g, 12 e 6,8cm; massa da matéria fresca, comprimento e largura das bagas, e diâmetro do pedicelo de, respectivamente, 4,3g; 19,9; 18,2 e 3,2mm. Quanto ao acúmulo de nutrientes, concluiu-se que a cultivar Niagara Rosada enxertada sobre 'Ripária do Traviú' apresentou maior acúmulo de P, Fe e Zn, enquanto sobre o porta-enxerto 'IAC 766' houve maior acúmulo de Mn. em ambos os porta-enxertos, a 'Niagara Rosada' apresentou a seguinte escala de acúmulo de nutrientes em ordem decrescente: K>N>P>Ca>S>Mg>B>Fe>Mn>Cu>Zn.

Correlação entre a produtividade e os resultados de análise foliar e de solo em vinhedos de Niagara Rosada

Realizou-se nos municípios de Jundiaí e Louveira-SP um levantamento do estado nutricional e de produtividade de 20 vinhedos de 'Niagara Rosada' enxertada sobre o porta-enxerto IAC 766 e outros 20 enxertadas sobre o 'Ripária do Traviú'. Coletaram-se amostras de solo a 0-20 e 20-40 cm de profundidade na linha e na entrelinha de plantio e amostras de folha completa, limbo e pecíolo nas épocas de pleno florescimento e no início da maturação das bagas, visando correlacionar com os dados de produtividade. Verificou-se para o porta-enxerto IAC 766 correlações significativas entre a produtividade com os resultados das análises de solo e de folhas. A baixa produtividade verificada esteve relacionada ao excesso de nutrientes no solo, especialmente cálcio e magnésio, em função da calagem e adubação serem realizadas sem levarem em consideração a análise do solo. A produtividade correlacionou-se positivamente com os teores de potássio no solo, a relação K/Mg nas folhas e os teores de potássio nas folhas; e negativamente com a relação (Ca+Mg)/K no solo e os teores de cálcio e magnésio nas folhas, exibindo o antagonismo entre o magnésio e o potássio.