Late-Glacial and early Holocene marine 14C reservoir ages off North Iceland (16-9 cal kyr BP)

Tephrochronological age models and 48 14C age determinations on molluscs and foraminifera (planktonic and benthic) are applied for the calculation of marine 14C reservoir age variability during a time period covering the Heinrich event H1 to early Holocene (16–9 cal kyr BP). Our data source consists of four high-resolution marine sediment cores (HM107-04, HM107-05, MD99-2271, MD99-2275) from the North Icelandic shelf. The marine reservoir age (ΔR) is found to be extremely variable, ranging from 385 to 1065 14C years. Extreme ΔR values occur at the end of H1, with values around 1000 14C years (~15 cal kyr BP), probably due to reduced northward flow of well-ventilated subtropical surface waters and a southward expansion of polar waters, as well as an expansion of sea ice limiting air-sea gas exchange. With the onset of the Bølling-Allerød interstadial, the ΔR values decrease towards 0 14C years suggesting a more vigorous North Atlantic Current and an active meridional overturning circulation system. During the Younger Dryas stadial, ΔR values are consistently around 700 14C years suggesting e renewed expansion of polar waters and a weakened meridional overtuning circulation. Interestingly, ΔR values remain high (~200 14C years) at the onset of the Holocene suggesting continued high influence of polar waters. Subsequently, ΔR values rapidly decrease to ~¬ 250 14C years around 11 cal kyr BP, indicating increased air-sea CO2 exchange with the coeval atmosphere. The ΔR values average around 0 14C years from around 10.5 to 9.0 cal kyr BP.

The fate of 14C-naphthalene in soil microcosms containing Scots pine seedlings and enchytraeids

The fate of freshly spiked and aged ¹⁴C-naphthalene associated residues as investigated in the presence and absence of ectomycorrhizal Scots pine seedlings and enchytraeid worms, in a factorial experimental design. Microcosms were used which enabled the ¹⁴C-labelled naphthalene associated residues to be quantified, including plant lipids which acted as an additional naphthalene sink within the microcosms. The presence of plant roots altered the availability of the ¹⁴C-naphthalene and associated residues to degrading microbes. Mineralisation and volatilisation of ¹⁴C naphthalene in freshly spiked soil were lower in the presence of Scots pine. Conversely, in soil aged for 180 d, Scots pine increased mineralisation, and bioavailability of naphthalene. Root-mediated processes, microbial activity and enchytraeids interact with desorption, bioavailability and mineralisation of naphthalene. © 2006 Elsevier Ltd. All rights reserved.

Degradation of 4-fluorobiphenyl by mycorrhizal fungi as determined by 19F nuclear magnetic resonance spectroscopy and 14C radiolabelling analysis

The pathways of biotransformation of 4-fluorobiphenyl (4FBP) by the ectomycorrhizal fungus Tylospora fibrilosa and several other mycorrhizal fungi were investigated by using ¹⁹F nuclear magnetic resonance (NMR) spectroscopy in combination with ¹⁴C radioisotope-detected high-performance liquid chromatography (¹⁴C- HPLC). Under the conditions used in this study T. fibrillosa and some other species degraded 4FBP. ¹⁴C-HPLC profiles indicated that there were four major biotransformation products, whereas ¹⁹F NMR showed that there were six major fluorine-containing products. We confirmed that 4-fluorobiphen-4'-ol and 4-fluorobiphen-3'-ol were two of the major products formed, but no other products were conclusively identified. There was no evidence for the expected biotransformation pathway (namely, meta cleavage of the less halogenated ring), as none of the expected products of this route were found. To the best of our knowledge, this is the first report describing intermediates formed during mycorrhizal degradation of halogenated biphenyls.

The effect of nitrate fertilization on the distribution of exported 14c-photosynthate in nodulated soybean (Glycine max (L.) Merr.) plants

Soybean (Glycine ~ (L.) Merr. cv. Harosoy 63) plants inoculated with Rhizobium japonicum were grown in vermiculite in the presence or absence of nitrate fertilization for up to 6 weeks after planting. Overall growth of nodulated plants was enhanced in the presence of nitrate fertilization, while the extent of nodule development was reduced. Although the number of nodules was not affected by nitrate fertilization when plants were grown at a light intensity limiting for photosynthesis, at light intensities approaching or exceeding the light saturation point for photosynthesis, nitrate fertilization resulted in at least a 30% reduction in nodule numbers. The mature, first trifoliate leaf of 21 day old plants was allowed to photoassimi1ate 14C02. One hour after·· the initial exposure to 14C02, the , plants were harvested and the 14C radioactivity was determined in the 80% ethanol-soluble fraction: in. o:rider to assess· "the extent of photoassimilate export and the pattern of distribution of exported 14C. The magnitude of 14C export was not affected by the presence of nitrate fertilization. However, there was a significant effect on the distribution pattern, particularly with regard to the partitioning of 14C-photosynthate between the nodules and the root tissue. In the presence of nitrate fertilization, less than 6% of the exported 14C photosynthate was recovered from the nodules, with much larger amounts (approximately 37%) being recovered from the root tissue. In the absence of nitrate fertilization, recovery of exported 14C-photosynthate from the nodules (19 to 27%) was approximately equal to that from the root tissue (24 to 33%). By initiating- or terminating the applications of nitrate at 14 days of age, it was determined that the period from day 14 to day 21 after planting was particularly significant for the development of nodules initiated earlier. Addition of nitrate fertilization at this time inhibited further nodule development while stimulating plant growth, whereas removal of nitrate fertilization stimulated nodule development. The results obtained are consistent with the hypothesis that nodule development is inhibited by nitrate fertilization through a reduction in the availability of photosynthate to the nodules.

Der Einfluss von Neuropeptid Y auf die Glukoseaufnahme im dorsalen Tectum opticum während visueller Stimulation der Unke Bombina orientalis: Quantitative Analyse mit Hilfe der 14C-2-Desoxiglukose-Technik

(1) Neuropeptid Y (NPY), einer der häufigsten peptidergen Neurotransmitter im zentralen und peripheren Nervensystem der Säuger, ist an der Steuerung zahlreicher physiologischer Prozesse beteiligt. Auch Amphibien weisen eine verstärkte NPY-Immunreaktivität im Zentralnervensystem auf. Im Hinblick auf bereits gewonnene Erkenntnisse sollte in der vorliegenden Arbeit eine Modulierbarkeit retino-tectaler Aktivität durch Neuropeptid Y an der chinesischen Rotbauchunke (Bombina orientalis) überprüft und erstmals mit Hilfe der 14[C]-2-Desoxiglukose-Methode (14C-2DG) (Sokoloff et al. 1977) quantitativ analysiert werden. Als Vergleichstier diente die Agakröte (Bufo marinus). Zur Darstellung eines möglichen Effektes auf das Tectum opticum wurde NPY lokal auf die tectale Oberfläche visuell stimulierter Rotbauchunken appliziert. Mit Hilfe der 14C-2DG-Methode und den daraus autoradiographisch ermittelten Daten konnten die zerebralen Aktivitäten visualisiert, quantitativ ausgewertet und miteinander verglichen werden. In einer weiteren Versuchsreihe wurde hinterfragt, welche inhibitorische Wirkung NPY entwickeln kann, wenn zuvor der retinale Input pharmakologisch durch systemische Gabe von Apomorphin (APO) signifikant erhöht wurde. (2) Die 14C-2DG-Methode erlaubt einen Blick in die funktionale Aktivität des Gehirns und ermöglicht es, regional ablaufende physiologische und biochemische Energiestoffwechselprozesse innerhalb des Gehirns quantitativ zu erfassen. Mit Hilfe der 14C-2DG-Methode werden die neuromodulatorischen Wirkungen von NPY kartiert und analysiert. (3) Versuchstiergruppe 1 – Bombina orientalis – unbehandelt Zur Beurteilung pharmakologischer Effekte durch NPY bzw. APO auf den Hirnmetabolismus war es zunächst erforderlich, die Gehirnaktivitäten pharmakologisch unbeeinflusster Tiere nach visueller Reizgabe zu untersuchen. Im Bereich des medialen Mesencephalon wurden die tectalen 14C-2DG-Konzentrationen über zehn Messreihen pro Einzeltier sowohl an der rechten als auch an der linken tectalen Hälfte auf Höhe des ventrolateralen Tectum opticum ermittelt. Beim rechts-links Vergleich zeigen sich gleich verteilte Strahlungsintensitäten. Basierend auf dieser Aussage konnte NPY unilateral auf die tectale Oberfläche aufgebracht und auf seine Wirkung geprüft werden. (4) Versuchstiergruppe 2 – Bombina orientalis – NPY-Applikation Der unilaterale Einsatz von NPY auf die tectale Oberfläche des Versuchstieres bewirkt, dass die unter dem Einfluss von NPY stehende tectale Hälfte, im Gegensatz zur unbehandelten tectalen Hälfte, einen deutlich niedrigeren 14C-2DG-Gebrauch aufweist. Besonders in den oberen Schichten des Tectum opticum (Layer 9) zeigt die 14C-2DG-Methode qualitativ und quantitativ auswertbare Aktivitätsminderungen an. (5) Verhalten unter NPY: Durchschnittlich nach 10 min Versuchsdauer zeigt Bombina orientalis eine deutliche Abnahme in der Beutefangaktivität, die sich gegen Ende der Versuchszeit noch weiter reduziert. (6) Versuchstiergruppe 3 – Bombina orientalis – APO-Applikation Systemisch verabreichtes APO führt bei Bombina orientalis zu einer Verstärkung des retinalen Ausganges in die retino-tectalen Projektionsfelder. Die neuronalen Aktivitäten im Tectum opticum erhöhen sich unter dem Einfluss von APO im Durchschnitt um 40% im Vergleich zu APO-unbehandelten Tieren. (7) Verhalten unter APO: Bombina orientalis zeigt nach systemischer Applikation von APO keine verstärkten stereotypen Schnappreaktionen. Die Tiere reagieren ausschließlich mit Akinese, d.h. einem Ausfall gerichteter Lokomotionen und Orientierungsbewegungen. (8) Versuchstiergruppe 4 – Bombina orientalis – APO/NPY-Applikation Die durch systemisch verabreichtes APO erhöhten retino-tectalen Aktivitäten im Tectum opticum werden unter dem unilateralen Einsatz von NPY deutlich abgeschwächt. Eindeutig niedrigere 14C-2DG-Aufnahmen sind in den oberen Schichten des Tectum opticum messbar, was die starke Wirkung von NPY quantitativ belegt. (9) Versuchstiergruppe 2 – Bufo marinus – NPY-Applikation Der unilaterale Einsatz von NPY auf die tectale Oberfläche von Bufo marinus zeigt ebenfalls, dass die unter dem Einfluss von NPY stehende tectale Hälfte, im Gegensatz zur unbehandelten tectalen Hälfte, einen deutlich niedrigeren 14C-2DG-Gebrauch aufweist. Bufo marinus zeigt aber aufgrund erweiterter Versuchsbedingungen (On-Off-Beleuchtungswechsel) anders verteilte Strahlungsintensitäten über dem Tectum-Querschnitt als Bombina orientalis. Stärkere [14C]-Akkumulationen zeigen sich in den tieferen zentralen Schichten des Tectum opticum. (10) Versuchstiergruppe 4 – Bufo marinus – APO/NPY-Applikation Auch die durch systemisch verabreichtes APO erhöhten retino-tectalen Aktivitäten im Tectum opticum von Bufo marinus werden unter dem unilateralen Einsatz von NPY deutlich abgeschwächt. (11) Die Ergebnisse der vorliegenden Arbeit leisten einen Beitrag zum Einfluss von NPY auf den retino-tectalen Informationstransfer bei Anuren im Sinne einer praetecto-tectalen inhibitorischen Modulation. Im Einklang mit früheren neuroanatomischen, immuncytochemischen und elektro-physiologischen Befunden liefern diese Ergebnisse erstmals ein biochemisches Korrelat auf der Basis des tectalen Energiestoffwechsels. (12) Es ist hervorzuheben, dass NPY-vermittelte inhibitorische Modulationen visuellen Informationstransfers in der vorliegenden Arbeit an Bombina orientalis nachgewiesen wurden, die phylogenetisch zu den ältesten Anuren (Anamnioten) gehört. Vergleichbares ist an verschiedenen Amnioten – einschließlich Primaten – beschrieben worden, was darauf hinweist, dass solche NPY-vermittelten Prozesse sich innerhalb der Tetrapoden relativ früh herausgebildet haben und in der Evolution konserviert worden sind.

Pollen-based reconstructions of biome distributions for Australia, Southeast Asia and the Pacific (SEAPAC region) at 0,6000 and 18,000 14C yr B.P.

Aim  This paper documents reconstructions of the vegetation patterns in Australia, Southeast Asia and the Pacific (SEAPAC region) in the mid-Holocene and at the last glacial maximum (LGM). Methods  Vegetation patterns were reconstructed from pollen data using an objective biomization scheme based on plant functional types. The biomization scheme was first tested using 535 modern pollen samples from 377 sites, and then applied unchanged to fossil pollen samples dating to 6000 ± 500 or 18,000 ± 1000 14C yr bp. Results  1. Tests using surface pollen sample sites showed that the biomization scheme is capable of reproducing the modern broad-scale patterns of vegetation distribution. The north–south gradient in temperature, reflected in transitions from cool evergreen needleleaf forest in the extreme south through temperate rain forest or wet sclerophyll forest (WSFW) and into tropical forests, is well reconstructed. The transitions from xerophytic through sclerophyll woodlands and open forests to closed-canopy forests, which reflect the gradient in plant available moisture from the continental interior towards the coast, are reconstructed with less geographical precision but nevertheless the broad-scale pattern emerges. 2. Differences between the modern and mid-Holocene vegetation patterns in mainland Australia are comparatively small and reflect changes in moisture availability rather than temperature. In south-eastern Australia some sites show a shift towards more moisture-stressed vegetation in the mid-Holocene with xerophytic woods/scrub and temperate sclerophyll woodland and shrubland at sites characterized today by WSFW or warm-temperate rain forest (WTRF). However, sites in the Snowy Mountains, on the Southern Tablelands and east of the Great Dividing Range have more moisture-demanding vegetation in the mid-Holocene than today. South-western Australia was slightly drier than today. The single site in north-western Australia also shows conditions drier than today in the mid-Holocene. Changes in the tropics are also comparatively small, but the presence of WTRF and tropical deciduous broadleaf forest and woodland in the mid-Holocene, in sites occupied today by cool-temperate rain forest, indicate warmer conditions. 3. Expansion of xerophytic vegetation in the south and tropical deciduous broadleaf forest and woodland in the north indicate drier conditions across mainland Australia at the LGM. None of these changes are informative about the degree of cooling. However the evidence from the tropics, showing lowering of the treeline and forest belts, indicates that conditions were between 1 and 9 °C (depending on elevation) colder. The encroachment of tropical deciduous broadleaf forest and woodland into lowland evergreen broadleaf forest implies greater aridity. Main conclusions  This study provides the first continental-scale reconstruction of mid-Holocene and LGM vegetation patterns from Australia, Southeast Asia and the Pacific (SEAPAC region) using an objective biomization scheme. These data will provide a benchmark for evaluation of palaeoclimate simulations within the framework of the Palaeoclimate Modelling Intercomparison Project.

Pollen-based reconstructions of Japanese biomes at 0, 6000 and 18,000 14C yr bp

A biomization method, which objectively assigns individual pollen assemblages to biomes ( Prentice et al., 1996 ), was tested using modern pollen data from Japan and applied to fossil pollen data to reconstruct palaeovegetation patterns 6000 and 18,000 14C yr bp Biomization started with the assignment of 135 pollen taxa to plant functional types (PFTs), and nine possible biomes were defined by specific combinations of PFTs. Biomes were correctly assigned to 54% of the 94 modern sites. Incorrect assignments occur near the altitudinal limits of individual biomes, where pollen transport from lower altitudes blurs the local pollen signals or continuous changes in species composition characterizes the range limits of biomes. As a result, the reconstructed changes in the altitudinal limits of biomes at 6000 and 18,000 14C yr bp are likely to be conservative estimates of the actual changes. The biome distribution at 6000 14C yr bp was rather similar to today, suggesting that changes in the bioclimate of Japan have been small since the mid-Holocene. At 18,000 14C yr bp the Japanese lowlands were covered by taiga and cool mixed forests. The southward expansion of these forests and the absence of broadleaved evergreen/warm mixed forests reflect a pronounced year-round cooling.

Pollen-based biomes for Beringia 18,000, 6000 and 0 14C yr B.P.

The objective biomization method developed by Prentice et al. (1996) for Europe was extended using modern pollen samples from Beringia and then applied to fossil pollen data to reconstruct palaeovegetation patterns at 6000 and 18,000 14C yr bp. The predicted modern distribution of tundra, taiga and cool conifer forests in Alaska and north-western Canada generally corresponds well to actual vegetation patterns, although sites in regions characterized today by a mosaic of forest and tundra vegetation tend to be preferentially assigned to tundra. Siberian larch forests are delimited less well, probably due to the extreme under-representation of Larix in pollen spectra. The biome distribution across Beringia at 6000 14C yr bp was broadly similar to today, with little change in the northern forest limit, except for a possible northward advance in the Mackenzie delta region. The western forest limit in Alaska was probably east of its modern position. At 18,000 14C yr bp the whole of Beringia was covered by tundra. However, the importance of the various plant functional types varied from site to site, supporting the idea that the vegetation cover was a mosaic of different tundra types.

Inverse modeling of the 14C bomb pulse in stalagmites to constrain the dynamics of soil carbon cycling at selected European cave sites

The decomposition of soil organic matter (SOM) is temperature dependent, but its response to a future warmer climate remains equivocal. Enhanced rates of decomposition of SOM under increased global temperatures might cause higher CO2 emissions to the atmosphere, and could therefore constitute a strong positive feedback. The magnitude of this feedback however remains poorly understood, primarily because of the difficulty in quantifying the temperature sensitivity of stored, recalcitrant carbon that comprises the bulk (>90%) of SOM in most soils. In this study we investigated the effects of climatic conditions on soil carbon dynamics using the attenuation of the 14C ‘bomb’ pulse as recorded in selected modern European speleothems. These new data were combined with published results to further examine soil carbon dynamics, and to explore the sensitivity of labile and recalcitrant organic matter decomposition to different climatic conditions. Temporal changes in 14C activity inferred from each speleothem was modelled using a three pool soil carbon inverse model (applying a Monte Carlo method) to constrain soil carbon turnover rates at each site. Speleothems from sites that are characterised by semi-arid conditions, sparse vegetation, thin soil cover and high mean annual air temperatures (MAATs), exhibit weak attenuation of atmospheric 14C ‘bomb’ peak (a low damping effect, D in the range: 55–77%) and low modelled mean respired carbon ages (MRCA), indicating that decomposition is dominated by young, recently fixed soil carbon. By contrast, humid and high MAAT sites that are characterised by a thick soil cover and dense, well developed vegetation, display the highest damping effect (D = c. 90%), and the highest MRCA values (in the range from 350 ± 126 years to 571 ± 128 years). This suggests that carbon incorporated into these stalagmites originates predominantly from decomposition of old, recalcitrant organic matter. SOM turnover rates cannot be ascribed to a single climate variable, e.g. (MAAT) but instead reflect a complex interplay of climate (e.g. MAAT and moisture budget) and vegetation development.

Degradação de 14C-atrazina em solo sob condições semicontroladas

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Efeito da idade sobre a fertilidade de éguas inseminadas com sêmen diluído, resfriado a 14ºC e transportado

Para estudar o efeito da idade sobre características ovulatórias e de fertilidade, 147 ciclos estrais de 99 éguas foram agrupados em classes por idade (1 - 3-6 anos; 2 - 7-10 anos; 3 - 11-14 anos; e 4 - 15-19 anos), de acordo com o ano do nascimento. As éguas foram inseminadas com sêmen diluído, resfriado e transportado de apenas um garanhão, três vezes por semana (segundas, quartas e sextas-feiras).O controle folicular, por meio da palpação retal, e a rufiação foram realizados diariamente, durante todo o período experimental. Utilizou-se, para o transporte, o sêmen diluído no diluidor de leite desnatado-glicose no conteiner Celle modificado, sendo a dose inseminante de 400 x 10(6) espermatozóides móveis, no momento da diluição final, pré-resfriamento. O tempo médio da coleta do sêmen à inseminação artificial foi de 3,5 horas e a temperatura final do sêmen, no momento da inseminação, de 14ºC. Não houve influência da idade sobre a velocidade de crescimento folicular e o tamanho do folículo ovulatório. A fertilidade decaiu após os 15 anos de idade, traduzida pela diminuição da taxa de concepção/ciclo e eficiência de prenhez, entretanto, não foram observadas características indicativas de senescência até os 19 anos de idade.

Efeito do número de inseminações artificiais sobre a fertilidade de éguas inseminadas com sêmen diluído, resfriado a 14ºC e transportado

Estudou-se o efeito do número de inseminações sobre a fertilidade de éguas inseminadas, três vezes/semana (segundas, quartas e sextas-feiras), com sêmen diluído, resfriado e transportado, de apenas um garanhão. As éguas foram inseminadas a partir da detecção, pela palpação retal, de um folículo de 3,0 a 3,5 cm de diâmetro, em um dos ovários, até a ovulação. Utilizaram-se para o transporte o sêmen diluído no diluidor leite desnatado-glicose e o conteiner Celle modificado, sendo a dose inseminante de 400 x 10(6) espermatozóides móveis, no momento da diluição final, pré-resfriamento. de acordo com o número de inseminações artificiais (IA) utilizadas/ciclo, os resultados de 148 ciclos, de 100 éguas, foram agrupados em: 1 IA, 2IA, 3 IA e 4 ou mais IA. A eficiência de prenhez foi de 4,29; 5,04; 5,67; e 3,43, para 1, 2, 3 e 4 ou mais IA, respectivamente. As características foliculares diferiram em relação à freqüência de inseminações com os maiores valores observados no grupo de éguas inseminadas quatro ou mais vezes. Concluiu-se que menor velocidade de crescimento folicular e maior diâmetro do folículo ovulatório estiveram associados a maior número de inseminações artificiais/ciclo. Na presença de uma concentração espermática adequada, o número de inseminações/ciclo não exerceu influência sobre a fertilidade.

Datação por luminescência opticamente estimulada (Loe) e por 14C de materiais de uma topossequência de solos na Serra do Espinhaço Meridional - MG: abordagem paleoambiental

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Hydromorphic Soil, Topographic Depression and Vegetation Development History by Using 13c and 14c In Rondônia State (sw Brazilian Amazon)

13C e 14C obtidos da matéria orgânica do solo foram usados para diferenciar fases de flutuação da vegetação em transição floresta-savana. A região apresenta baixos platôs com depressões topográficas imperfeitamente drenadas na superfície. Na topossequência estudada foram analisados solos de cinco perfis localizados sob floresta (F), transição floresta-savana (S1), borda da depressão sob savana (S2) e centro da depressão sob savana (S3). Os valores de 13C e idades evidenciam que a ~ 200cm de profundidade, com idades entre ~ 12.000 e 10.000 A.P., valores de -27‰ a -27,7‰ indicam vegetação de floresta (C3) em todos os perfis. Na profundidade de 100 cm, com idades entre ~ 6.000 e 5.000 A.P., houve enriquecimento de – 20,2‰ a -22,3‰, indicando regressão da floresta e expansão da savana. Valores entre -15,9 e -18,7‰ a 50-60 cm, estimado entre ~ 4.700 a 3.800 A.P., sugere máxima expansão da vegetação C4 em resposta às condições climáticas mais secas, exceto no perfil S3 com valores mais empobrecidos (-20,9‰), sugerindo que na depressão, o desenvolvimento da hidromorfia possibilitou a presença de espécies de gramíneas C3 e C4 da savana em resposta as mudanças das condições ambientais.