Produção e caracterização de biomateriais acelulares bioativos obtidos a partir da decelularização de placentas

A bioengenharia de tecidos baseia-se no uso de moléculas bioativas, células-tronco e biomateriais para reparação de tecidos e/ou órgãos. Biomateriais podem ser classificados de acordo com sua origem em sintéticos ou biológicos. Biomateriais biológicos podem ser produzidos por decelularização, que visa a remoção de células da matriz extracelular (MEC), a qual deve manter sua integridade química e física. Placentas são órgãos de grande interesse na bioengenharia de tecidos visto que são descartadas após o parto e possuem grande volume de matriz extracelular. Métodos de decelularização podem ser classificados em químicos, físicos e enzimáticos. Todos conhecidamente causam alterações na MEC, sendo que a associação deles é comumente utilizada. Este trabalho comparou diferentes protocolos e estabeleceu um método mais favorável para a decelularização de placentas caninas, visando a produção de um biomaterial para futuras aplicações clínicas. Inicialmente ambas as porções - materna e fetal - das placentas foram submetidas à 10 protocolos, que avaliaram variáveis como concentração e tempo de incubação em detergentes, diferentes gradientes de temperatura e a influência da perfusão versus imersão das soluções, na MEC remanescente. Com base na transparência do tecido e na ausência de núcleo celular em cortes histológicos, dois protocolos foram selecionados (I e II). Além dos critérios já mencionados, ambos os protocolos foram comparados quanto à quantidade de DNA remanescente na MEC decelularizada e à permanência e distribuição de algumas das proteínas da matriz. O detergente SDS foi o mais eficaz na remoção de células, embora não tenha sido suficiente para promover uma decelularização tecidual completa. O congelamento prévio das placentas requereu um maior tempo de incubação posterior das amostras nos distintos detergentes. Ambos métodos de perfusão e imersão foram eficazes na remoção das células, embora grande concentração de proteínas do citoesqueleto tenham permanecido retidas na matriz. As amostras processadas pelo protocolo I (SDS 1%, 5mM EDTA + 50mM TRIS + 0,5% antibiótico, e Triton X-100 1%) apresentaram maior preservação da organização estrutural da MEC quando comparadas àquelas processadas de acordo com o protocolo II (que diferiu do anterior pela utilização de solução contendo 0,05% tripsina ao invés de 50mM TRIS), esse último método entretanto foi o que melhor removeu as células das placentas, conforme observado em lâminas histológicas e demonstrado pela menor concentração de DNA. Tanto as porções materna quanto fetal submetidas à ambos protocolos, mantiveram as proteínas laminina, fibronectina e colágeno tipo I. O colágeno tipo III foi observado somente na porção fetal. Conclui-se que o protocolo II foi o mais eficaz no processo de decelularização de placentas caninas tendo promovido a remoção do conteúdo celular e diminuição da concentração de DNA na MEC remanescente. No entanto é necessário otimizar o tempo de incubação das placentas em soluções enzimáticas visando maior conservação do arranjo da matriz decelularizada. A análise da capacidade da MEC decelularizada por tal método para ser utilizada em bioengenharia de tecidos ainda deve ser avaliada in vitro e in vivo

Influência da densidade tubular em diferentes profundidades dentinárias na estabilidade de união de cimentos de iônomero de vidro

O objetivo do estudo foi avaliar a influência da densidade tubular em diferentes profundidades dentinárias na estabilidade de união de dois cimentos de ionômero de vidro (CIV) de alta viscosidade. Vinte terceiros molares foram alocados em 6 grupos experimentais, de acordo com a profundidade da dentina - proximal, oclusal superficial ou oclusal profunda, e os CIVs - Fuji IX (GC Corp.) e Ketac(TM) Molar Easy Mix (3M/ESPE). Inicialmente os dentes foram cortados a fim de se obter fatias de aproximadamente 1 mm de espessura de dentina proximal, oclusal superficial e profunda. Em seguida, foi realizado uma análise topográfica das secções das diferentes superfícies e profundidades em microscopia confocal a laser (100X) para obtenção das médias da densidade tubular em cada profundidade. Cânulas de polietileno foram então posicionadas sobre as secções de dentina pré-tratadas e preenchidas pelos CIVs. Os espécimes foram armazenados em água destilada por 24 h e 12 meses a 37°C, em seguida foram submetidos ao ensaio de microcisalhamento (0,5 mm/min). Após o ensaio, foi realizada a análise do padrão de fratura em estereomicroscópio (400X). Os dados obtidos foram submetidos à Análise de Variância para dados repetidos, seguido do teste de Tukey (?=5%). Verificamos que a densidade dos túbulos dentinários, em diferentes profundidades de molares permanentes, é inversamente proporcional a resistência de união de cimentos de ionômero de vidro de alta viscosidade. Foi ainda observado em todos os grupos que a resistência de união após 24 horas é maior do que em 12 meses, indicando degradação da interface adesiva ao longo do tempo.

Infrared microspectroscopy of inflammatory process and colon tumors.

According to the last global burden of disease published by the World Health Organization, tumors were the third leading cause of death worldwide in 2004. Among the different types of tumors, colorectal cancer ranks as the fourth most lethal. To date, tumor diagnosis is based mainly on the identification of morphological changes in tissues. Considering that these changes appears after many biochemical reactions, the development of vibrational techniques may contribute to the early detection of tumors, since they are able to detect such reactions. The present study aimed to develop a methodology based on infrared microspectroscopy to characterize colon samples, providing complementary information to the pathologist and facilitating the early diagnosis of tumors. The study groups were composed by human colon samples obtained from paraffin-embedded biopsies. The groups are divided in normal (n=20), inflammation (n=17) and tumor (n=18). Two adjacent slices were acquired from each block. The first one was subjected to chemical dewaxing and H&E staining. The infrared imaging was performed on the second slice, which was not dewaxed or stained. A computational preprocessing methodology was employed to identify the paraffin in the images and to perform spectral baseline correction. Such methodology was adapted to include two types of spectral quality control. Afterwards the preprocessing step, spectra belonging to the same image were analyzed and grouped according to their biochemical similarities. One pathologist associated each obtained group with some histological structure based on the H&E stained slice. Such analysis highlighted the biochemical differences between the three studied groups. Results showed that severe inflammation presents biochemical features similar to the tumors ones, indicating that tumors can develop from inflammatory process. A spectral database was constructed containing the biochemical information identified in the previous step. Spectra obtained from new samples were confronted with the database information, leading to their classification into one of the three groups: normal, inflammation or tumor. Internal and external validation were performed based on the classification sensitivity, specificity and accuracy. Comparison between the classification results and H&E stained sections revealed some discrepancies. Some regions histologically normal were identified as inflammation by the classification algorithm. Similarly, some regions presenting inflammatory lesions in the stained section were classified into the tumor group. Such differences were considered as misclassification, but they may actually evidence that biochemical changes are in course in the analyzed sample. In the latter case, the method developed throughout this thesis would have proved able to identify early stages of inflammatory and tumor lesions. It is necessary to perform additional experiments to elucidate this discrepancy between the classification results and the morphological features. One solution would be the use of immunohistochemistry techniques with specific markers for tumor and inflammation. Another option includes the recovering of the medical records of patients who participated in this study in order to check, in later times to the biopsy collection, whether they actually developed the lesions supposedly detected in this research.

Snakes based tracking and texture analysis of microscopic images

Comunicación presentada en el VII Symposium Nacional de Reconocimiento de Formas y Análisis de Imágenes, SNRFAI, Barcelona, abril 1997.

BDNF impairs recovery of synaptic transmission after hypoxia even with blockage of adenosine A2A receptors

Trabalho Final do Curso de Mestrado Integrado em Medicina, Faculdade de Medicina, Universidade de Lisboa, 2014

Homeostatic plasticity induced by brief activity deprivation enhances long-term potentiation in the mature rat hippocampus

Trabalho Final do Curso de Mestrado Integrado em Medicina, Faculdade de Medicina, Universidade de Lisboa, 2014

Bases moléculaires et cellulaires d’un trouble neurodéveloppemental causé par l’haploinsuffisance de SYNGAP1

La déficience intellectuelle est la cause d’handicap la plus fréquente chez l’enfant. De nombreuses évidences convergent vers l’idée selon laquelle des altérations dans les gènes synaptiques puissent expliquer une fraction significative des affections neurodéveloppementales telles que la déficience intellectuelle ou encore l’autisme. Jusqu’à récemment, la majorité des mutations associées à la déficience intellectuelle a été liée au chromosome X ou à la transmission autosomique récessive. D’un autre côté, plusieurs études récentes suggèrent que des mutations de novo dans des gènes à transmission autosomique dominante, requis dans les processus de la plasticité synaptique peuvent être à la source d’une importante fraction des cas de déficience intellectuelle non syndromique. Par des techniques permettant la capture de l’exome et le séquençage de l’ADN génomique, notre laboratoire a précédemment reporté les premières mutations pathogéniques dans le gène à transmission autosomique dominante SYNGAP1. Ces dernières ont été associées à des troubles comportementaux tels que la déficience intellectuelle, l’inattention, des problèmes d’humeur, d’impulsivité et d’agressions physiques. D’autres patients sont diagnostiqués avec des troubles autistiques et/ou des formes particulières d’épilepsie généralisée. Chez la souris, le knock-out constitutif de Syngap1 (souris Syngap1+/-) résulte en des déficits comme l’hyperactivité locomotrice, une réduction du comportement associée à l’anxiété, une augmentation du réflexe de sursaut, une propension à l’isolation, des problèmes dans le conditionnement à la peur, des troubles dans les mémoires de travail, de référence et social. Ainsi, la souris Syngap1+/- représente un modèle approprié pour l’étude des effets délétères causés par l’haploinsuffisance de SYNGAP1 sur le développement de circuits neuronaux. D’autre part, il est de première importance de statuer si les mutations humaines aboutissent à l’haploinsuffisance de la protéine. SYNGAP1 encode pour une protéine à activité GTPase pour Ras. Son haploinsuffisance entraîne l’augmentation des niveaux d’activité de Ras, de phosphorylation de ERK, cause une morphogenèse anormale des épines dendritiques et un excès dans la concentration des récepteurs AMPA à la membrane postsynaptique des neurones excitateurs. Plusieurs études suggèrent que l’augmentation précoce de l’insertion des récepteurs AMPA au sein des synapses glutamatergiques contribue à certains phénotypes observés chez la souris Syngap1+/-. En revanche, les conséquences de l’haploinsuffisance de SYNGAP1 sur les circuits neuronaux GABAergiques restent inconnues. Les enjeux de mon projet de PhD sont: 1) d’identifier l’impact de mutations humaines dans la fonction de SYNGAP1; 2) de déterminer si SYNGAP1 contribue au développement et à la fonction des circuits GABAergiques; 3) de révéler comment l’haploinsuffisance de Syngap1 restreinte aux circuits GABAergiques affecte le comportement et la cognition. Nous avons publié les premières mutations humaines de type faux-sens dans le gène SYNGAP1 (c.1084T>C [p.W362R]; c.1685C>T [p.P562L]) ainsi que deux nouvelles mutations tronquantes (c.2212_2213del [p.S738X]; c.283dupC [p.H95PfsX5]). Ces dernières sont toutes de novo à l’exception de c.283dupC, héritée d’un père mosaïque pour la même mutation. Dans cette étude, nous avons confirmé que les patients pourvus de mutations dans SYNGAP1 présentent, entre autre, des phénotypes associés à des troubles comportementaux relatifs à la déficience intellectuelle. En culture organotypique, la transfection biolistique de l’ADNc de Syngap1 wild-type dans des cellules pyramidales corticales réduit significativement les niveaux de pERK, en fonction de l’activité neuronale. Au contraire les constructions plasmidiques exprimant les mutations W362R, P562L, ou celle précédemment répertoriée R579X, n’engendre aucun effet significatif sur les niveaux de pERK. Ces résultats suggèrent que ces mutations faux-sens et tronquante résultent en la perte de la fonction de SYNGAP1 ayant fort probablement pour conséquences d’affecter la régulation du développement cérébral. Plusieurs études publiées suggèrent que les déficits cognitifs associés à l’haploinsuffisance de SYNGAP1 peuvent émerger d’altérations dans le développement des neurones excitateurs glutamatergiques. Toutefois, si, et auquel cas, de quelle manière ces mutations affectent le développement des interneurones GABAergiques résultant en un déséquilibre entre l’excitation et l’inhibition et aux déficits cognitifs restent sujet de controverses. Par conséquent, nous avons examiné la contribution de Syngap1 dans le développement des circuits GABAergiques. A cette fin, nous avons généré une souris mutante knockout conditionnelle dans laquelle un allèle de Syngap1 est spécifiquement excisé dans les interneurones GABAergiques issus de l’éminence ganglionnaire médiale (souris Tg(Nkx2.1-Cre);Syngap1flox/+). En culture organotypique, nous avons démontré que la réduction de Syngap1 restreinte aux interneurones inhibiteurs résulte en des altérations au niveau de leur arborisation axonale et dans leur densité synaptique. De plus, réalisés sur des coupes de cerveau de souris Tg(Nkx2.1-Cre);Syngap1flox/+, les enregistrements des courants inhibiteurs postsynaptiques miniatures (mIPSC) ou encore de ceux évoqués au moyen de l’optogénétique (oIPSC) dévoilent une réduction significative de la neurotransmission inhibitrice corticale. Enfin, nous avons comparé les performances de souris jeunes adultes Syngap1+/-, Tg(Nkx2.1-Cre);Syngap1flox/+ à celles de leurs congénères contrôles dans une batterie de tests comportementaux. À l’inverse des souris Syngap1+/-, les souris Tg(Nkx2.1-Cre);Syngap1flox/+ ne présentent pas d’hyperactivité locomotrice, ni de comportement associé à l’anxiété. Cependant, elles démontrent des déficits similaires dans la mémoire de travail et de reconnaissance sociale, suggérant que l’haploinsuffisance de Syngap1 restreinte aux interneurones GABAergiques dérivés de l’éminence ganglionnaire médiale récapitule en partie certains des phénotypes cognitifs observés chez la souris Syngap1+/-. Mes travaux de PhD établissent pour la première fois que les mutations humaines dans le gène SYNGAP1 associés à la déficience intellectuelle causent la perte de fonction de la protéine. Mes études dévoilent, également pour la première fois, l’influence significative de ce gène dans la régulation du développement et de la fonction des interneurones. D’admettre l’atteinte des cellules GABAergiques illustre plus réalistement la complexité de la déficience intellectuelle non syndromique causée par l’haploinsuffisance de SYNGAP1. Ainsi, seule une compréhension raffinée de cette condition neurodéveloppementale pourra mener à une approche thérapeutique adéquate.

Analysis of analogue models by helical X-ray computed tomography

The aim of analogue model experiments in geology is to simulate structures in nature under specific imposed boundary conditions using materials whose rheological properties are similar to those of rocks in nature. In the late 1980s, X-ray computed tomography (CT) was first applied to the analysis of such models. In early studies only a limited number of cross-sectional slices could be recorded because of the time involved in CT data acquisition, the long cooling periods for the X-ray source and computational capacity. Technological improvements presently allow an almost unlimited number of closely spaced serial cross-sections to be acquired and calculated. Computer visualization software allows a full 3D analysis of every recorded stage. Such analyses are especially valuable when trying to understand complex geological structures, commonly with lateral changes in 3D geometry. Periodic acquisition of volumetric data sets in the course of the experiment makes it possible to carry out a 4D analysis of the model, i.e. 3D analysis through time. Examples are shown of 4D analysis of analogue models that tested the influence of lateral rheological changes on the structures obtained in contractional and extensional settings.

Tropical climate and vegetation simulations during the Heinrich event 1 using an Earth System Model of Intermediate Complexity (EMIC) - the University of Victoria Earth System-Climate Model (UVic ESCM)

Abrupt climate changes from 18 to 15 thousand years before present (kyr BP) associated with Heinrich Event 1 (HE1) had a strong impact on vegetation patterns not only at high latitudes of the Northern Hemisphere, but also in the tropical regions around the Atlantic Ocean. To gain a better understanding of the linkage between high and low latitudes, we used the University of Victoria (UVic) Earth System-Climate Model (ESCM) with dynamical vegetation and land surface components to simulate four scenarios of climate-vegetation interaction: the pre-industrial era, the Last Glacial Maximum (LGM), and a Heinrich-like event with two different climate backgrounds (interglacial and glacial). We calculated mega-biomes from the plant-functional types (PFTs) generated by the model to allow for a direct comparison between model results and palynological vegetation reconstructions. Our calculated mega-biomes for the pre-industrial period and the LGM corresponded well with biome reconstructions of the modern and LGM time slices, respectively, except that our pre-industrial simulation predicted the dominance of grassland in southern Europe and our LGM simulation resulted in more forest cover in tropical and sub-tropical South America. The HE1-like simulation with a glacial climate background produced sea-surface temperature patterns and enhanced inter-hemispheric thermal gradients in accordance with the "bipolar seesaw" hypothesis. We found that the cooling of the Northern Hemisphere caused a southward shift of those PFTs that are indicative of an increased desertification and a retreat of broadleaf forests in West Africa and northern South America. The mega-biomes from our HE1 simulation agreed well with paleovegetation data from tropical Africa and northern South America. Thus, according to our model-data comparison, the reconstructed vegetation changes for the tropical regions around the Atlantic Ocean were physically consistent with the remote effects of a Heinrich event under a glacial climate background.

Stable carbon and oxygen isotope composition of benthic foraminifera

Seventeen surface sediment samples from the North Atlantic Ocean off NE-Greenland between 76° and 81°N, and nine samples from the South Atlantic Ocean close to Bouvet Island between 48° and 55°S were taken with the aid of a Multiple Corer and investigated for their live (Rose Bengal stained) benthic foraminiferal content within the upper 15 cm of sediment. Preferentially endobenthic Melonis barleeanum, Melonis zaandami, and Bulimina aculeata as well as preferentially epibenthic Lobatula lobatula were counted from 1-cm-thick sediment slices each and analyzed for stable carbon and oxygen isotopic compositions of their calcareous tests. Live and dead specimens were counted and measured separately. The carbon isotopic composition of the foraminifera was compared to that of the dissolved inorganic carbon (DIC) of simultaneously sampled bottom water. During a period of one month, one station off NE-Greenland was replicately sampled once every week and samples were processed as above. Live specimens of Lobatula lobatula are confined to the uppermost two centimeters of sediment. Live specimens of Melonis spp. are found down to 8 cm within the sediment but with a distinct sub-surface maximum between 2 and 5 cm. The down-core distribution of live Bulimina aculeata shows a distinct surface maximum in the top centimeter and constant but low numbers down to 11-cm subbottom depth. The average stable carbon isotopic composition (d13C versus per mil PDB) of live Lobatula lobatula off NE-Greenland is by 0.4±0.1 per mil higher than the d13CDIC of the ambient bottom water at the time of sampling. There is evidence that this species calcify before the ice-free season, when bottom water d13CDIC is supposed to be higher. This would reconfirm the one-to-one relationship between d13C of ambient water DIC and cibicids, widely used by paleoceanographers. Live Melonis barleeanum show a negative offset from bottom water DIC of -1.7±0.6 per mil in the uppermost sediment and of -2.2±0.5 per mil in 3-4-cm subbottom depth. All d13C values of live Melonis spp. decrease within the upper four centimeters, regardless of the time of sampling and site investigated. The offset of live Bulimina aculeata from bottom water d13CDIC values of 8 stations rather constantly amounts to -0.6±0.1 per mil, no matter what subbottom depth the specimens are from. At one station however, where is strong indication of elevated organic carbon flux, the negative offset averaged over all sub-bottom depths increases to -1.5±0.2 per mil. Buliminids actively move within the sediment and by this either record an average isotope signal of the pore water or the signal of one specific calcification depth. The recorded signal, however, depends on the organic carbon flux and reflects general but site-specific pore water d13CDIC values. If compared with epibenthic d13C values from the same site, not influenced by pore water and related phytodetritus layer effects, Buliminad13C values bear some potential as a paleoproductivity proxy. Specimens of Melonis spp. seem to prefer a more static way of life and calcify at different but individually fix depths within the sediment. Although live specimens thus record a stratified pore water d13C signal, there is no means yet to correct for bioturbational and early diagenetic effects in fossil faunas.

Raw-data to morphometric investigations about the Neogene planktonic foraminifer Globorotalia menardii and related forms from ODP Hole 154-925B (Céara Rise, western tropical Atlantic)

Evolutionary prospection is the study of morphological evolution and speciation in calcareous plankton from selected time-slices and key sites in the world oceans. In this context, the Neogene menardiform globorotalids serve as study objects for morphological speciation in planktic foraminifera. A downcore investigation of test morphology of the lineage of G. menardii-limbata-multicamerata during the past 8 million years was carried out in the western tropical Atlantic ODP Hole 925B. A total of 4669 specimens were measured and analyzed from 38 stratigraphic levels and compared to previous studies from DSDP Sites 502 and 503. Collection of digital images and morphometric measurements from digitized outlines were achieved using a microfossil orientation and imaging robot called AMOR and software, which was especially developed for this purpose. Most attention was given to the evolution of spiral height versus axial length of tests in keel view, but other parameters were investigated as well. The variability of morphological parameters in G. menardii, G. limbata, and G. multicamerata through time are visualized by volume density diagrams. At Hole 925B results show gradual test size increase in G. menardii until about 3.2 Ma. The combination of taxonomic determination in the light microscope with morphometric investigations shows strong morphological overlap and evolutionary continuity from ancestral to extant G. menardii (4-6 chambers in the final whorl) to the descendent but extinct G. limbata (seven chambers in the final whorl) and to G. multicamerata (>=8 chambers in the final whorl). In the morphospace defined by spiral height (dX) and axial length (dY) Globorotalia limbata and G. multicamerata strongly overlap with G. menardii. Distinction of G. limbata from G. menardii is only possible by slight differences in the number of chambers of the final whorl, nuances in spiral convexity, upper keel angles, radii of osculating circles, or by differences in reflectance of their tests. Globorotalia multicamerata can be distinguished from the other two forms by more than eight chambers in the final whorl. It appeared as two stratigraphically separate clusters during the Pliocene. Between 2.88 and 2.3 Ma G. menardii was severely restricted in size and abundance. Thereafter, it showed a rapid and prominent expansion of the upper test size extremes between 2.3 and 1.95 Ma persisting until present. The size-frequency distributions at Hole 925B are surprisingly similar to trends of menardiform globorotalids from Caribbean DSDP Site 502. There, the observations were explained as an adaptation to changes in the upper water column due to the emergence of the Isthmus of Panama. In light of more recent paleontological and geological investigations about the completion of the permanent land connection between North and South America since about 3 Ma the present study gives reason to suspect the sudden test size increase of G. menardii to reflect immigration of extra-large G. menardii from the Indian Ocean or the Pacific. It is hypothesized that during the Late Pliocene dispersal of large G. menardii into the southern to tropical Atlantic occurred during an intermittent episode of intense Agulhas Current leakage around the Cape of Good Hope and from there via warm eddy transport to the tropical Atlantic (Agulhas dispersal hypothesis).

Spectral analysis of seabed elevation from the Danish Wadden Sea

Bedforms both reflect and influence shallow water hydrodynamics and sediment dynamics. A correct characterization of their spatial distribution and dimensions is required for the understanding, assessment and prediction of numerous coastal processes. A method to parameterize geometrical characteristics using two-dimensional (2D) spectral analysis is presented and tested on seabed elevation data from the Knudedyb tidal inlet in the Danish Wadden Sea, where large compound bedforms are found. The bathymetric data were divided into 20x20 m areas on which a 2D spectral analysis was applied. The most energetic peak of the 2D spectrum was found and its energy, frequency and direction were calculated. A power-law was fitted to the average of slices taken through the 2D spectrum; its slope and y-intercept were calculated. Using these results the test area was morphologically classified into 4 distinct morphological regions. The most energetic peak and the slope and intercept of the power-law showed high values above the crest of the primary bedforms and scour holes, low values in areas without bedforms, and intermediate values in areas with secondary bedforms. The secondary bedform dimensions and orientations were calculated. An area of 700x700 m was used to determine the characteristics of the primary bedforms. However, they were less distinctively characterized compared to the secondary bedforms due to relatively large variations in their orientations and wavelengths. The method is thus appropriate for morphological classification of the seabed and for bedform characterization, being most efficient in areas characterized by bedforms with regular dimensions and directions.

Clay mineralogy of sediment cores from the Arctic Ocean

This study focuses on sedimentological investigations of sediment cores recovered during the international Arctic'91, expeditions with the German research ice breaker RV "Polarstern" to the European sector of the Arctic Ocean. Here, we deduce the last glacial/interglacial changes in transport mechanism and sedimentation from the clay mineral group smectite. We choose the smectites as an example of how sediment mineralogy can be linked with particular source regions (the Kara and Laptev seas), distinct transport mechanism (sea ice and surface currents) and sedimentation processes. Smectite contents in Arctic sediments discussed for two time slices, including the Last Glacial Maximum (LGM), and the last deglaciation (Termination I), reveal the highest variability subsequent to the retreat of the Eurasian ice sheets. Our results show that smectite anomalies in the Eurasian Basin are associated with distinct meltwater pulses and occurred around 13.5-13.0 14C ka B.P. Compelling evidence is provided that these anomalies are deduced from sea-ice entrained sediments from the eastern Kara Sea that entered the Arctic Ocean after ice-sheet break-up and eventually flooding of the Kara Sea. We propose that smectite anomalies in sediments of the eastern Arctic Ocean can be utilized to identify deglacial events and to help decipher configurations of the Eurasian ice sheets. The identification of smectite maxima along the modern sea-ice edge in the Eurasian Basin further indicates biologically enhanced sedimentation from melting sea ice allowing the reconstruction of seasonally open water in the region. Hence, considering the poor preservation conditions of primary paleoceanographic proxies in the Arctic Ocean, the clay mineral contents, particularly the smectite group, may be one alternative tool for paleoclimatic reconstruction in the Eurasian Basin.

Short-term variations in radiolarian faunal dsitribution in the eastern equatorial Pacific

Two short time intervals centered at 2.3 and 4.7 Ma were studied to investigate short-term variations in surface-ocean processes as indicated by changes in the radiolarian microfossil population. These time intervals represent two different settings of late Neogene climate. The older interval represents a time when tropical circulation between the Pacific and Atlantic oceans was not blocked by the Isthmus of Panama, whereas the younger interval represents a time when Northern Hemisphere glaciation was present but did not display the dominance of the 100,000-yr cycle that characterizes the late Pleistocene. The younger time slice at 2.3 Ma was sampled at all Leg 138 sites except Site 844, where significant reworking was evident. All sites except 844, 853, and 854 were sampled for the older time slice. Samples were taken at 10- to 20-cm intervals at each site and spanned a GRAPE density maximum and minimum. Thus, it was possible to investigate whether the changes in carbonate content (as indicated by GRAPE density) were associated with changes in surface-ocean conditions (indicated by radiolarian assemblage variations). For both time slices, the radiolarian data indicate that intervals of decreased carbonate content are periods of cooler water conditions and possibly enhanced biogenic production. Times of increased carbonate content are associated with inferred warmer oceanographic conditions, as indicated by the dominance of tropical assemblages at 2.3 Ma and tropical and western Pacific assemblages during the time slice centered at 4.8 Ma. However, the spatial patterns of change during each time slice show a distinct difference in the mapped patterns of radiolarian assemblage dominance. The older time slice, representing a period before the closing of the Isthmus of Panama, shows more zonal patterns presumably associated with a more zonal character of equatorial circulation. After the closing of the isthmus, the shifts in faunal patterns between times of high and low carbonates are characterized by shifts in the dominance of the tropical and transitional assemblages, respectively, throughout the region.

Results of calculated surface air temperature anomaly of COSMOS Pliocene experiment 2 in NetCDF format

In this manuscript we describe the experimental procedure employed at the Alfred Wegener Institute in Germany in the preparation of the simulations for the Pliocene Model Intercomparison Project (PlioMIP). We present a description of the utilized Community Earth System Models (COSMOS, version: COSMOS-landveg r2413, 2009) and document the procedures that we applied to transfer the Pliocene Research, Interpretation and Synoptic Mapping (PRISM) Project mid-Pliocene reconstruction into model forcing fields. The model setup and spin-up procedure are described for both the paleo- and preindustrial (PI) time slices of PlioMIP experiments 1 and 2, and general results that depict the performance of our model setup for mid-Pliocene conditions are presented. The mid-Pliocene, as simulated with our COSMOS setup and PRISM boundary conditions, is both warmer and wetter in the global mean than the PI. The globally averaged annual mean surface air temperature in the mid-Pliocene standalone atmosphere (fully coupled atmosphere-ocean) simulation is 17.35 °C (17.82 °C), which implies a warming of 2.23 °C (3.40 °C) relative to the respective PI control simulation.