Constituintes químicos e avaliação do potencial alelopático de Adiantum tetraphyllum Humb. & Bonpl. Ex. Willd (Pteridaceae)

Chemical studies of green leaves of A. tetraphyllum afforded beta-sitosterol, a mixture containing the ethyl esters of long chain carboxylic acids, 30-normethyl-lupan-20-one, hopan-22-ol, phytol, phyten-3(20)-1,2-diol, quercetin and quercetin-3-O-beta-D-glucoside. The structures of the compounds were elucidated by spectroscopic and GC analysis. The allelopathic potentials of the crude ethanolic extract and fractions were evaluated against Lactuca sativa (letuce) and Allium cepa (onion) seeds.

Entwicklungsstadien von Sprossen : Osterluzei - Aristolochia clematitis - Farne: Osmunda, Aspidium, Adiantum, Polypodium

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Adiantum-Blätter : Adiantum monochlamys - Adiantum macrophyllum - Adiantum formosum, vergrößerte Fiederchen - Adiantum trapeziforme - Adiantum formosum - Adiantum amabile - Adiantum tenerum - Adiantum tenerum, vergrößerte Fiederchen

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Farne : Asplenium ruta muraria - Trichomanes angustatum - Osmunda regalis - Adiantum reniforme - Polypodium urophyllum

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Entwicklungsstadien von Sprossen : Aristolochia clematitis - Farne: Osmunda, Aspidium, Adiantum, Polypodium

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A phytochrome from the fern Adiantum with features of the putative photoreceptor NPH1

In plant photomorphogenesis, it is well accepted that the perception of red/far-red and blue light is mediated by distinct photoreceptor families, i.e., the phytochromes and blue-light photoreceptors, respectively. Here we describe the discovery of a photoreceptor gene from the fern Adiantum that encodes a protein with features of both phytochrome and NPH1, the putative blue-light receptor for second-positive phototropism in seed plants. The fusion of a functional photosensory domain of phytochrome with a nearly full-length NPH1 homolog suggests that this polypeptide could mediate both red/far-red and blue-light responses in Adiantum normally ascribed to distinct photoreceptors.

Chloroplast-Avoidance Response Induced by High-Fluence Blue Light in Prothallial Cells of the Fern Adiantum capillus-veneris as Analyzed by Microbeam Irradiation1

Chloroplast movement was induced by partial cell illumination using a high-fluence blue microbeam in light-grown and dark-adapted prothallial cells of the fern Adiantum capillus-veneris. Chloroplasts inside the illuminated area moved out (high-fluence response [HFR]), whereas those outside moved toward the irradiated area (low-fluence response [LFR]), although they stopped moving when they reached the border. These results indicate that both HFR and LFR signals are generated by high-fluence blue light of the same area, and that an LFR signal can be transferred long-distance from the beam spot, although an HFR signal cannot. The lifetime of the HFR signal was calculated from the traces of chloroplast movement induced by a brief pulse from a high-fluence blue microbeam to be about 6 min. This is very short compared with that of the LFR (30–40 min; T. Kagawa, M. Wada [1994] J Plant Res 107: 389–398). These data indicate that the signal transduction pathways of the HFR and the LFR must be distinct.

Anatomia foliar das espécies de Pteridaceae do Parque Estadual do Rio Doce (PERD) - MG

O objetivo desse estudo foi selecionar caracteres que possam auxiliar na taxonomia das espécies de Pteridaceae ocorrentes no PERD. Durante levantamento preliminar realizado no PERD, foram coletadas 15 famílias, 27 gêneros e 57 espécies de Pteridophyta. A família que apresentou maior número de representantes foi Pteridaceae com 17 espécies, distribuídas em quatro gêneros (Adiantum, Hemionitis, Pityrogramma e Pteris). As folhas destas espécies apresentam pecíolo glabro, piloso ou escamoso cuja epiderme é uniestratificada, córtex constituído por esclerênquima e parênquima e o sistema vascular representado por um meristelo, em Pteris e Hemionitis, e dois ou três meristelos em Adiantum e Pityrogramma. Na região distal do pecíolo, esses meristelos são classificados como do tipo "Onoclea" e "Asterochlaena" em Adiantum, "Grammitis" em Hemionitis, "Onoclea" em Pityrogramma e "Loxsoma" e "Pteris podophylla" em Pteris. A lâmina foliar apresenta epiderme uniestratificada com idioblastos esclerenquimáticos paralelos, oblíquos ou restritos às nervuras, em Adiantum e Pityrogramma e reforçando as margens, em Pteris; os idioblastos estão ausentes em Hemionitis. Algumas espécies apresentam a lâmina foliar pilosa ou escamosa. Os estômatos ocorrem na face abaxial das pínulas sendo anomocíticos, às vezes associados a diacíticos, em Adiantum, Hemionitis e Pityrogramma e polocíticos, associados a copolocíticos, em Pteris. O mesofilo homogêneo é constituído por células braciformes, na maioria das espécies de Adiantum, ou por células lobadas, tendendo a isodiamétricas, nos demais gêneros. Os caracteres anatômicos mais relevantes para a identificação das Pteridaceae do PERD foram: presença de pêlos ou escamas; tipos de estômatos; presença e distribuição de idioblastos na epiderme e tipo e disposição do(s) feixe(s) vascular(es) no pecíolo.

Polypodiaceae e Pteridaceae da Estação Ecológica do Panga, Uberlândia, Estado de Minas Gerais, Brasil

O presente trabalho apresenta o tratamento taxonômico das espécies de Polypodiaceae e Pteridaceae da Estação Ecológica do Panga. A Estação Ecológica do Panga abrange 409,5 ha e está situada a 30 km ao sul do centro da cidade de Uberlândia, MG, entre as coordenadas 19°09'20"-19°11'10" S e 48°23'20"-48°24'35" W, a 740-840 m de altitude. A área apresenta grande importância ecológica por ser uma das poucas formações de vegetação natural da região e por possuir diferentes fisionomias comuns do bioma Cerrado como campestres, savânicas e florestais. Polypodiaceae está representada por quatro gêneros e sete espécies (Campyloneurum centrobrasilianum Lellinger, C. phyllitidis (L.) C. Presl, C. repens (Aubl.) C. Presl, Microgramma lindbergii (Mett. ex Kuhn) de la Sota, M. persicariifolia (Schrad.) C. Presl, Pecluma robusta (Fée) M. Kessler & A.R. Sm. e Phlebodium areolatum (Humb. & Bonpl. ex Willd.) J. Sm.) e Pteridaceae por quatro gêneros e oito espécies (Adiantopsis chlorophylla (Sw.) Fée, Adiantum deflectens Mart., A. intermedium Sw., A. serratodentatum Humb. & Bonpl. ex Willd., Pityrogramma calomelanos (L.) Link, P. trifoliata (L.) R.M. Tryon, Pteris quadriaurita Retz. e P. vittata L.). São apresentadas chaves para gêneros e espécies, bem como ilustrações e comentários da distribuição geográfica de todos os táxons.

Licófitas e monilófitas das Unidades de Conservação da Usina Hidroelétrica - UHE de Tucuruí, Pará, Brasil

O presente estudo refere-se às espécies de licófitas e monilófitas ocorrentes nas Zonas de Preservação da Vida Silvestre da Usina Hidroelétrica de Tucuruí, Estado do Pará, Brasil. A área de estudo localiza-se na região sudeste do Pará, com cerca de 29.700 hectares, composta, predominantemente, por floresta ombrófila aberta. Os dados obtidos demonstraram a ocorrência de 18 famílias, 37 gêneros e 82 espécies. A família com maior riqueza de espécies é Pteridaceae (21 spp.) e o gênero mais representativo é Adiantum com 14 espécies. Três espécies são novas referências para o Pará: Didymoglossum ovale, Danaea nodosa e Pecluma hygrometrica. Além disso, duas espécies novas foram identificados, uma delas já descrita, Thyelypteris amazonica. A outra espécie pertence a Adiantum e será publicada em breve. A riqueza florística da área, associada com as novidades taxonômicas, atesta a sua importância biológica e aponta para a necessidade de aumentar os esforços em pesquisa e conservação da área estudada.

Early - Late Miocene palaeoclimate data and palaefloras of 48 samples from Southern China

Southern China, especially Yunnan, has undergone high tectonic activity caused by the uplift of Himalayan Mountains during the Neogene, which led to a fast changing palaeogeography. Previous study shows that Southern China has been influenced by the Asian Monsoon since at least the Early Miocene. However, it is yet not well understood how intense the Miocene monsoon system was. In the present study, 63 fossil floras of 16 localities from Southern China are compiled and evaluated for obtaining available information concerning floristic composition, stratigraphic age, sedimentology, etc. Based on such reliable information, selected mega- and micro-floras have been analysed with the coexistence approach to obtain quantitative palaeoclimate data. Visualization of climate results in maps shows a distinct spatial differentiation in Southern China during the Miocene. Higher seasonalities of temperature and precipitation occur in the north and south parts of Southern China, respectively. During the Miocene, most regions of Southern China and Europe were both warm and humid. Central Eurasia was likely to be an arid center, which gradually spread westward and eastward. Our data provide information about Miocene climate patterns in Southern China and about the evolution of these patterns throughout the Miocene, and is also crucial to unravel and understand the climatic signals of global cooling and tectonic uplift.

Pollen and non-pollen palynomorph records of the Holocene part of the composite sediment core TMD from lake Tso Moriri (NW India) and of modern surface samples from the Tso Moriri region

The high-altitude lake Tso Moriri (32°55'46'' N, 78°19'24'' E; 4522 m a.s.l.) is situated at the margin of the ISM and westerly influences in the Trans-Himalayan region of Ladakh. Human settlements are rare and domestic and wild animals are concentrating at the alpine meadows. A set of modern surface samples and fossil pollen from deep-water TMD core was evaluated with a focus on indicator types revealing human impact, grazing activities and lake system development during the last ca. 12 cal ka BP. Furthermore, the non-pollen palynomorph (NPP) record, comprising remains of limnic algae and invertebrates as well as fungal spores and charred plant tissue fragments, were examined in order to attest palaeolimnic phases and human impact, respectively. Changes in the early and middle Holocene limnic environment are mainly influenced by regional climatic conditions and glacier-fed meltwater flow in the catchment area. The NPP record indicates low lake productivity with high influx of freshwater between ca. 11.5 and 4.5 cal ka BP which is in agreement with the regional monsoon dynamics and published climate reconstructions. Geomorphologic observations suggest that during this period of enhanced precipitation the lake had a regular outflow and contributed large amounts of water to the Sutlej River, the lower reaches of which were integral part of the Indus Civilization area. The inferred minimum fresh water input and maximum lake productivity between ca. 4.5-1.8 cal ka BP coincides with the reconstruction of greatest aridity and glaciation in the Korzong valley resulting in significantly reduced or even ceased outflow. We suggest that lowered lake levels and river discharge on a larger regional scale may have caused irrigation problems and harvest losses in the Indus valley and lowlands occupied by sedentary agricultural communities. This scenario, in turn, supports the theory that, Mature Harappan urbanism (ca. 4.5-3.9 cal ka BP) emerged in order to facilitate storage, protection, administration, and redistribution of crop yields and secondly, the eventual collapse of the Harappan Culture (ca. 3.5-3 cal ka BP) was promoted by prolonged aridity. There is no clear evidence for human impact around Tso Moriri prior to ca. 3.7 cal ka BP, with a more distinct record since ca. 2.7 cal ka BP. This suggests that the sedimentary record from Tso Moriri primarily archives the regional climate history.

Fossil pollen record of composite sediment core TMD from Tso Moriri, analysis of modern surface pollen samples, mean annual precipitation reconstruction, and digitisation and recalibration of different discussed palaeoclimate proxy records

This paper presents a new fossil pollen record from Tso Moriri (32°54'N, 78°19'E, 4512 m a.s.l.) and seeks to reconstruct changes in mean annual precipitation (MAP) during the last 12,000 years. This high-alpine lake occupies an area of 140 km**2 in a glacial-tectonic valley in the northwestern Himalaya. The region has a cold climate, with a MAP <300 mm, and open vegetation. The hydrology is controlled by the Indian Summer Monsoon (ISM), but winter westerly-associated precipitation also affects the regional water balance. Results indicate that precipitation levels varied significantly during the Holocene. After a rapid increase in MAP, a phase of maximum humidity was reached between ca. 11 to 9.6 cal ka BP, followed by a gradual decline in MAP. This trend parallels the reduction in the Northern Hemisphere summer insolation. Comparison of different palaeoclimate proxy records reveal evidence for a stronger Holocene decrease in precipitation in the northern versus the southern parts of the ISM domain. The long-term trend of ISM weakening is overlaid with several short periods of greater dryness, which are broadly synchronous with the North Atlantic cold spells, suggesting reduced amounts of westerly-associated winter precipitation. Compared to the mid and late Holocene, it appears that westerlies had a greater influence on the western parts of the ISM domain during the early Holocene. During this period, the westerly-associated summer precipitation belt was positioned at Mediterranean latitudes and amplified the ISM-derived precipitation. The Tso Moriri pollen record and moisture reconstructions also suggest that changes in climatic conditions affected the ancient Harappan Civilisation, which flourished in the greater Indus Valley from approximately 5.2 to 3 cal ka BP. The prolonged Holocene trend towards aridity, punctuated by an interval of increased dryness (between ca. 4.5 to 4.3 cal ka BP), may have pushed the Mature Harappan urban settlements (between ca. 4.5 to 3.9 cal ka BP) to develop more efficient agricultural practices to deal with the increasingly acute water shortages. The amplified aridity associated with North Atlantic cooling between ca. 4 to 3.6 and around 3.2 cal ka BP further hindered local agriculture, possibly causing the deurbanisation that occurred from ca. 3.9 cal ka BP and eventual collapse of the Harappan Civilisation between ca. 3.5 to 3 cal ka BP.