Pollen record and age determiation of sediments from the Labaz Lake area

Pollen records from perennially frozen sequences provide vegetation and climate reconstruction for the last 48,000 14C years in the central part of Taymyr Peninsula. Open larch forest with Alnus fruticosa and Betula nana grew during the Kargin (Middle Weichselian) Interstade, ca. 48,000-25,000 14C yr B.P. The climate was generally warmer and wetter than today. Open steppe-like communities with Artemisia, Poaceae, Asteraceae, and herb tundralike communities with dwarf Betula and Salix dominated during the Sartan (Late Weichselian) Stade, ca. 24,000-10,300 14C yr B.P. The statistical information method used for climate reconstruction shows that the coldest climate was ca. 20,000-17,000 14C yr B.P. A warming (Allerød Interstade?) with mean July temperature ca. 1.5°C warmer than today occurred ca. 12,000 14C yr B.P. The following cooling with temperatures about 3°-4°C cooler than present and precipitation about 100 mm lower corresponds well with the Younger Dryas Stade. Tundra-steppe vegetation changed to Betula nana-Alnus fruticosa shrub tundra ca. 10,000 14C yr B.P. Larch appeared in the area ca. 9400 14C yr B.P. and disappeared after 2900 14C yr B.P. Cooling events ca. 10,500, 9600, and 8200 14C yr B.P. characterized the first half of the Holocene. A significant warming occurred ca. 8500 14C yr B.P., but the Holocene temperature maximum was at about 6000-4500 14C yr B.P. The vegetation cover approximated modern conditions ca. 2800 14C yr B.P. Late Holocene warming events occurred at ca. 3500, 2000, and 1000 14C yr B.P. A cooling (Little Ice Age?) took place between 500 and 200 14C yr ago.

Paleoclimate reconstruction from Miocene macroflora in Kazakhstan compiled from various publications

25 datasets (13 fossil leaf and pollen assemblages, 12 quantitative palaeoclimatic datasets) are provided in order to analyse Early Miocene palaeoclimate in Kazakhstan. The rich fossil record in Kazakhstan documents that during the Oligocene and Early Miocene this area in Central Eurasia was densely forested with warm-temperate deciduous trees and shrubs of the so-called "Turgayan flora". 29 fossil floras from 13 localities have been selected for a quantitative analysis of the Aquitanian (early Early Miocene) climate situation in Kazakhstan. The assessed mean annual temperatures generally place around 15 °C, while values of mean annual precipitation are of about 1000 mm. In combination with several other climate parameters estimated (temperatures of warmest and coldest months, precipitation rates of wettest, driest and warmest months), these data reflect uniform climatic conditions over several thousands of square kilometres. Data of temperature parameters show slight spatial differentiations, with generally cooler mean annual temperatures and higher seasonality (i.e. warmer summers and colder winters) in the north-eastern part of the study area compared with the south-western area around Lake Aral. As compared with palaeoclimate estimates for the European and East Asian Aquitanian, the central part of the Eurasian continent reveals evident signals of higher seasonality and slightly increased continentality.

Conversion of sub-tropical native vegetation to introduced conifer forest: Impacts on below-ground and above-ground carbon pools

Land-use change can have a major influence on soil organic carbon (SOC) and above-ground C pools. We assessed a change from native vegetation to introduced Pinus species plantations on C pools using eight paired sites. At each site we determined the impacts on 0–50 cm below-ground (SOC, charcoal C, organic matter C, particulate organic C, humic organic C, resistant organic C) and above-ground (litter, coarse woody debris, standing trees and woody understorey plants) C pools. In an analysis across the different study sites there was no significant difference (P > 0.05) in SOC or above-ground tree C stocks between paired native vegetation and pine plantations, although significant differences did exist at specific sites. SOC (calculated based on an equivalent soil mass basis) was higher in the pine plantations at two sites, higher in the native vegetation at two sites and did not differ for the other four sites. The site to site variation in SOC across the landscape was far greater than the variation observed with a change from native vegetation to introduced Pinus plantation. Differences between sites were not explained by soil type, although tree basal area was positively correlated with 0–50 cm SOC. In fact, in the native vegetation there was a significant linear relationship between above-ground biomass and SOC that explained 88.8% of the variation in the data. Fine litter C (0–25 mm diameter) tended to be higher in the pine forest than in the adjacent native vegetation and was significantly higher in the pine forest at five of the eight paired sites. Total litter C (0–100 mm diameter) increased significantly with plantation age (R2 = 0.64). Carbon stored in understorey woody plants (2.5–10 cm DBH) was higher in the native vegetation than in the adjacent pine forest. Total site C varied greatly across the study area from 58.8 Mg ha−1 at a native heathland site to 497.8 Mg ha−1 at a native eucalypt forest site. Our findings suggest that the effects of change from native vegetation to introduced Pinus sp. forest are highly site-specific and may be positive, negative, or have no influence on various C pools, depending on local site characteristics (e.g. plantation age and type of native vegetation).

Crescimento in vitro de isolados de Armillaria sp. obtidos de Pinus elliottii var: elliottii sob várias temperaturas

A armilariose tem sido considerada a principal doença em Pinus no Brasil. Os sintomas e danos consistem no amarelecimento de acículas, declínio, podridão de raízes, exsudação de resina e morte. A temperatura é um dos fatores ambientais que influencia patógenos, doença de plantas ou ambos. Este trabalho avaliou o comportamento de três isolados de Armillaria sp. obtidos de P. elliottii var. elliottii, submetidos a uma faixa de temperatura de 16 a 26 ºC, utilizando a biomassa seca produzida em meio líquido como parâmetro de análise. Verificou-se que todos os isolados apresentaram máxima produção de biomassa a 22 ºC. Utilizando-se de regressão cúbica encontrou-se temperaturas de máximo crescimento entre 21,79 e 23,19 ºC. De acordo com os resultados, a melhor temperatura para crescimento dos isolados testados situou-se em 22 ºC.

Suficiência amostral para coletas de serapilheira acumulada sobre o solo em Pinus elliottii Engelm, Eucalyptus sp. E floresta estacional decidual

O presente estudo objetivou determinar a suficiência amostral para coletas de serapilheira acumulada sobre o solo em povoamentos de Pinus elliottii, Eucalyptus sp., ambos plantados no Campus da Universidade Federal de Santa Maria e em uma área de Floresta Estacional Decidual (FED) localizada no Morro do Elefante, Santa Maria, RS. Para a realização do estudo, foram coletadas 100 amostras de serapilheira por floresta, com o auxílio de uma moldura quadrada de 25 cm de lado, totalizando 300 amostras, as quais foram separadas nas seguintes frações: acículas ou folhas, galhos, estruturas reprodutivas, cascas e resíduos. Com base nos pesos de matéria seca de cada fração, realizou-se a análise estatística dos dados, visando à estabilização dos valores do coeficiente de variação (CV%). Para Pinus elliottii, a maior contribuição na formação da serapilheira foi dada pelas acículas, com 57,2%; em Eucalyptus sp., isso ocorreu com os galhos (38,8%) e na FED, novamente com as folhas, que representaram 49,6% da serapilheira. No Pinus elliottii, o maior CV% se deu nos resíduos, seguido de estruturas reprodutivas. Em Eucalyptus sp., o maior CV% foi encontrado em cascas, seguido de galhos. Na FED, as cascas tiveram o maior CV%. A suficiência amostral necessária para Pinus elliottii foi de 40, sendo esse o povoamento que necessitou de menos amostras para estabilizar o CV%. Em Eucalyptus sp., a suficiência amostral foi de 70, enquanto na FED foram necessárias 80 amostras.

Análise técnica e econômica da resinagem de Pinus elliottii Engelm. var. elliottii na região de Manduri, SP

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)