454 resultados para 1G-GDGT-TEX86


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Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary conditions along continental margins. In this study, we present a new approach to regionalize the total organic carbon (TOC) content in surface sediments (<5 cm sediment depth). It is based on a compilation of more than 5500 single measurements from various sources. Global TOC distribution was determined by the application of a combined qualitative and quantitative-geostatistical method. Overall, 33 benthic TOC-based provinces were defined and used to process the global distribution pattern of the TOC content in surface sediments in a 1°x1° grid resolution. Regional dependencies of data points within each single province are expressed by modeled semi-variograms. Measured and estimated TOC values show good correlation, emphasizing the reasonable applicability of the method. The accumulation of organic carbon in marine surface sediments is a key parameter in the control of mineralization processes and the material exchange between the sediment and the ocean water. Our approach will help to improve global budgets of nutrient and carbon cycles.

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In ocean margin sediments both marine and terrestrial organic matter (OM) are buried but the factors governing their relative preservation and degradation are not well understood. In this study, we analysed the degree of preservation of marine isoprenoidal and soil-derived branched glycerol dialkyl glycerol tetraethers (GDGTs) upon long-term oxygen exposure in OM-rich turbidites from the Madeira Abyssal Plain by analyzing GDGT concentrations across oxidation fronts. Relative to the anoxic part of the turbidites ca. 7-20% of the soil-derived branched GDGTs were preserved in the oxidized part while only 0.2-3% of the marine isoprenoid GDGT crenarchaeol was preserved. Due to these different preservation factors the Branched Isoprenoid Tetraether (BIT) index, a ratio between crenarchaeol and the major branched GDGTs that is used as a tracer for soil-derived organic matter, substantially increases from 0.02 to 0.4. Split Flow Thin Cell (SPLITT) separation of turbidite sediments showed that the enhanced preservation of soil-derived carbon was a general phenomenon across the fine particle size ranges (<38 ?m). Calculations reveal that, despite their relatively similar chemical structures, degradation rates of crenarchaeol are 2-fold higher than those of soil-derived branched GDGTs, suggesting preferential soil OM preservation possibly due to matrix protection.

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The cores described in this report were taken on the SOUTHTOW Expedition in June 1972 to January 1973 by the Scripps Institution of Oceanography from the R/V Thomas Washington. A total of 105 cores and dredges were recovered and are available at Scripps for sampling and study.

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We reconstruct the latest Paleocene and early Eocene (~57-50 Ma) environmental trends in the Arctic Ocean and focus on the Paleocene-Eocene thermal maximum (PETM) (~55 Ma), using strata recovered from the Lomonosov Ridge by the Integrated Ocean Drilling Program Expedition 302. The Lomonosov Ridge was still partially subaerial during the latest Paleocene and earliest Eocene and gradually subsided during the early Eocene. Organic dinoflagellate cyst (dinocyst) assemblages point to brackish and productive surface waters throughout the latest Paleocene and early Eocene. Dinocyst assemblages are cosmopolitan during this time interval, suggesting warm conditions, which is corroborated by TEX86'-reconstructed temperatures of 15°-18°C. Inorganic geochemistry generally reflects reducing conditions within the sediment and euxinic conditions during the upper lower Eocene. Spectral analysis reveals that the cyclicity, recorded in X-ray fluorescence scanning Fe data from close to Eocene thermal maximum 2 (~53 Ma, presence confirmed by dinocyst stratigraphy), is related to precession. Within the lower part of the PETM, proxy records indicate enhanced weathering, runoff, anoxia, and productivity along with sea level rise. On the basis of total organic carbon content and variations in sediment accumulation rates, excess organic carbon burial in the Arctic Ocean appears to have contributed significantly to the sequestration of injected carbon during the PETM.

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Chondroitin sulfate (CS) is a naturally glycosaminoglycan found in the extracellular matrix of connective tissues and it may be extracted and purified those tissues. CS is involved in various biological functions, which may be related to the having structural variability, despite the simplicity of the linear chain structure from this molecule. Researches in biotechnology and pharmaceutical field with wastes from aquaculture has been developed in Brazil. In recent decades, tilapia (Oreochromis niloticus), native fish from Africa, has been one of the most cultivated species in various regions of the world, including Brazil. The tilapia farming is a cost-effective activity, however, it generates large amount of wastes that are discarded by producers. It is understood that waste from tilapia can be used in research as a source of molecules with important biotechnological applications, which also helps in reducing environmental impacts and promote the development of an ecofriendly activity. Thus, nile tilapia viscera were subjected to proteolysis, then the glycosaminoglycans were complexed with ion exchange resin (Lewatit), it was fractionated with increasing volumes of acetone and purified by ion exchange chromatography DEAE-Sephacel. Further, the fraction was analyzed by agarose gel electrophoresis and nuclear magnetic resonance (NMR). The electrophoretic profile of the compound together the analysis of 1H NMR spectra and the HSQC correlation allow to affirm that the compound corresponds to a molecule like chondroitin sulfate. MTT assay was used to assess cell viability in the presence of CS tilapia isolated and showed that the compound is not cytotoxic to normal cells such as cells from the mouse embryo fibroblast (3T3). Then, this compound was tested for the ability to reduce the influx of leukocytes in model of acute peritonitis (in vivo) induced by sodium thioglycolate. In this context, it was done total and differential leukocytes counting in the blood and peritoneal fluid collected respectively from vena cava and the peritoneal cavity of the animals subjected to the experiment. The chondroitin sulfate for the first time isolated from tilapia (CST ) was able to reduce the migration of leukocytes to the peritoneal cavity of inflamed mice until 80.4 per cent at a dose 10µg/kg. The results also show that there was a significant reduction (p<0.001) of the population of polymorphonuclear leukocytes from peritoneal cavity in the three tested doses (0.1µg/kg; 1µg/kg and 10µg/kg) when it was compared to the positive control (just thioglycolate). Therefore, since the CST structure and mechanism of action has been completely elucidated, this compound may have potential for therapeutic use in inflammatory diseases

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The uncontrolled disposal of wastewaters containing phenolic compounds by the industry has caused irreversible damage to the environment. Because of this, it is now mandatory to develop new methods to treat these effluents before they are disposed of. One of the most promising and low cost approaches is the degradation of phenolic compounds via photocatalysis. This work, in particular, has as the main goal, the customization of a bench scale photoreactor and the preparation of catalysts via utilization of char originated from the fast pyrolysis of sewage sludge. The experiments were carried out at constant temperature (50°C) under oxygen (410, 515, 650 and 750 ml min-1). The reaction took place in the liquid phase (3.4 liters), where the catalyst concentration was 1g L-1 and the initial concentration of phenol was 500 mg L-1 and the reaction time was set to 3 hours. A 400 W lamp was adapted to the reactor. The flow of oxygen was optimized to 650 ml min-1. The pH of the liquid and the nature of the catalyst (acidified and calcined palygorskite, palygorskite impregnated with 3.8% Fe and the pyrolysis char) were investigated. The catalytic materials were characterized by XRD, XRF, and BET. In the process of photocatalytic degradation of phenol, the results showed that the pH has a significant influence on the phenol conversion, with best results for pH equal to 5.5. The phenol conversion ranged from 51.78% for the char sewage sludge to 58.02% (for palygorskite acidified calcined). Liquid samples analyzed by liquid chromatography and the following compounds were identified: hydroquinone, catechol and maleic acid. A mechanism of the reaction was proposed, whereas the phenol is transformed into the homogeneous phase and the others react on the catalyst surface. For the latter, the Langmuir-Hinshelwood model was applied, whose mass balances led to a system of differential equations and these were solved using numerical methods in order to get estimates for the kinetic and adsorption parameters. The model was adjusted satisfactorily to the experimental results. From the proposed mechanism and the operating conditions used in this study, the most favored step, regardless of the catalyst, was the acid group (originated from quinone compounds), being transformed into CO2 and water, whose rate constant k4 presented value of 0.578 mol L-1 min-1 for acidified calcined palygorskite, 0.472 mol L-1 min-1 for Fe2O3/palygorskite and 1.276 mol L-1 min-1 for the sludge to char, the latter being the best catalyst for mineralization of acid to CO2 and water. The quinones were adsorbed to the acidic sites of the calcined palygorskite and Fe2O3/palygorskite whose adsorption constants were similar (~ 4.45 L mol-1) and higher than that of the sewage sludge char (3.77 L mol-1).

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The uncontrolled disposal of wastewaters containing phenolic compounds by the industry has caused irreversible damage to the environment. Because of this, it is now mandatory to develop new methods to treat these effluents before they are disposed of. One of the most promising and low cost approaches is the degradation of phenolic compounds via photocatalysis. This work, in particular, has as the main goal, the customization of a bench scale photoreactor and the preparation of catalysts via utilization of char originated from the fast pyrolysis of sewage sludge. The experiments were carried out at constant temperature (50°C) under oxygen (410, 515, 650 and 750 ml min-1). The reaction took place in the liquid phase (3.4 liters), where the catalyst concentration was 1g L-1 and the initial concentration of phenol was 500 mg L-1 and the reaction time was set to 3 hours. A 400 W lamp was adapted to the reactor. The flow of oxygen was optimized to 650 ml min-1. The pH of the liquid and the nature of the catalyst (acidified and calcined palygorskite, palygorskite impregnated with 3.8% Fe and the pyrolysis char) were investigated. The catalytic materials were characterized by XRD, XRF, and BET. In the process of photocatalytic degradation of phenol, the results showed that the pH has a significant influence on the phenol conversion, with best results for pH equal to 5.5. The phenol conversion ranged from 51.78% for the char sewage sludge to 58.02% (for palygorskite acidified calcined). Liquid samples analyzed by liquid chromatography and the following compounds were identified: hydroquinone, catechol and maleic acid. A mechanism of the reaction was proposed, whereas the phenol is transformed into the homogeneous phase and the others react on the catalyst surface. For the latter, the Langmuir-Hinshelwood model was applied, whose mass balances led to a system of differential equations and these were solved using numerical methods in order to get estimates for the kinetic and adsorption parameters. The model was adjusted satisfactorily to the experimental results. From the proposed mechanism and the operating conditions used in this study, the most favored step, regardless of the catalyst, was the acid group (originated from quinone compounds), being transformed into CO2 and water, whose rate constant k4 presented value of 0.578 mol L-1 min-1 for acidified calcined palygorskite, 0.472 mol L-1 min-1 for Fe2O3/palygorskite and 1.276 mol L-1 min-1 for the sludge to char, the latter being the best catalyst for mineralization of acid to CO2 and water. The quinones were adsorbed to the acidic sites of the calcined palygorskite and Fe2O3/palygorskite whose adsorption constants were similar (~ 4.45 L mol-1) and higher than that of the sewage sludge char (3.77 L mol-1).

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CARD-FISH was performed as previously described in Ruff et al., (2013; doi:10.1371/journal.pone.0072627) with the following modifications. 4-6 µl of 25-fold diluted sediment were used for filtration. Archaeal cell walls were permeabilized with 0.1M HCl for 2 min to detect ANME-3 cells, or Proteinase K solution (15 µg ml-1 (Merck, Darmstadt, Germany) in 0.05 M EDTA (pH 8), 0.1 M Tris-HCl (pH 8), 0.5 M NaCl) for 2-4 min at room temperature for all other archaea. Bacterial cell walls were permeabilized with lysozyme solution (1000kU/ml) for 60 min at 37°. Cells were stained with DAPI (1µg/ml), embedded in mounting medium and counted in 40-60 independent microscopic fields using an Axiophot II epifluorescence microscope (Carl Zeiss, Jena, Germany).

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Campomanesia adamantium and Campomanesia pubescens are morphologically similar, occur in the same regions of the Cerrado, are difficult to differentiate and exhibit naturally slow growth and development. The objectives of this study were to analyze fruit and seed biometric data, emergence capacity and seedling growth characteristics. Fruit from both species was collected and used to measure biometric data of the fruit and seeds and to set up two emergence and two seedling growth experiments. C. adamantium fruit is round and has wider, pale yellow seeds while C. pubescens fruit is ellipsoidal to pyriform with yellow gold seeds. C. adamantium’s greater fresh fruit mass and biometric variability favors selection of promising material for commercialization. Seed drying reduced the speed and rate of seedling emergence of C. adamantium, but had no effect on C. pubescens. Leaf number, height, shoot dry weight and the ratio of shoot dry weight to root dry weight were greater in C. adamantium than in the slower growing C. pubescens. Increases in substrate volume favor seedling development. Slow-release fertilizer application at 1g per 115 cm3 substrate increased leaf formation, plant height and shoot dry weight of seedlings of both species and lateral budding in C. adamantium. Until 120 days after transplant, lateral budding was not observed in C. pubescens seedlings. For all traits evaluated in this experiment, C. adamantium seedling growth was greater than that of C. pubescens.

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Toneladas de pescado são desperdiçadas diariamente aquando do processamento do peixe e o hambúrguer de pata-roxa foi desenvolvido para reaproveitar esse pescado subvalorizado e para ser uma fonte nutricional rica em antioxidantes. No presente trabalho, pretendeu-se comprovar o potencial antioxidante antes e após o tratamento térmico do hambúrguer de pata-roxa, e o potencial citotóxico e antiproliferativo sobre um modelo celular do cancro da mama (MCF-7). Foi também observada a estabilidade do hambúrguer de pata-roxa embalado a vácuo e refrigerado. A extração dos compostos fitoquímicos foi realizada com solventes de polaridade distinta (água, metanol e diclorometano) e com diferentes durações do processo (12h e 24h). O tratamento térmico aplicado foi vinte minutos a 180ºC. O potencial antioxidante foi avaliado pela capacidade de redução do radical livre 1,1-difenil-2-picrilhidrazil (DPPH) e pela capacidade de redução de radicais de oxigénio (ORAC), e através da quantificação total de polifenóis (QTP) pelo método de Folin-Ciocalteu (FC). O potencial citotóxico e antiproliferativo foi avaliado na linha celular MCF-7, cujos resultados foram revelados por ensaios espectrofotométricos (método do brometo de 3- (4,5-dimetiltiazol-2-il)-2,5-difenil tetrazólio (MTT)) e fluorimétricos (método de acetoxi-metil éster de calceína (calceína-AM)). A estabilidade do hambúrguer de pataroxa em vácuo e refrigerado foi avaliada através do estudo microbiológico com metodologias de referência (contagens de “totais” e produtores de sulfureto de hidrogénio (H2S) aeróbios e anaeróbios, esporos de Clostridium sulfitos-redutores, enterobactérias, Escherichia coli e pesquisa de Salmonella spp.), da determinação do índice de ácido tiobarbitúrico (TBA) e da avaliação da cor do hambúrguer pelo sistema CIE-L*a*b*. Os ensaios de DPPH e ORAC comprovaram a atividade antioxidante do extrato de hambúrguer de pata-roxa (metanol, 12h) com 79,5% de redução do DPPH e 8603,01μmol ET/100g para amostras sem tratamento térmico, e 87,4% de redução do DPPH e 2567,27μmol ET/100g para amostras com tratamento térmico. Quanto ao conteúdo fenólico, os extratos (metanol, 12h) revelaram 17,13mg EAG/100g do hambúrguer cru e 31,81mg EAG/100g do hambúrguer cozinhado. A extração de 24 horas não aumentou a quantidade de compostos fitoquímicos presentes no extrato. O hambúrguer apenas revelou ainda um potencial citotóxico in vitro relevante na linha celular MCF-7 (1mg/mL, 24h).Apesar do abuso observado na temperatura de armazenamento em refrigeração (temperatura média de 10,3ºC), o hambúrguer de pata-roxa cru, quando submetido ao embalamento a vácuo, apresentou um aumento no período de vida útil de prateleira de 4 dias relativamente à pata-roxa. Foi detetada a presença de esporos de Clostridium sulfito-redutores e 1,0x101ufc E. coli por 1g de hambúrguer de pata-roxa. Não foi detetada a presença de Salmonella spp. O índice de TBA manteve-se estável, mas o hambúrguer de pata-roxa sofreu uma perda na vivacidade (Cab) e na tonalidade (hab) da cor ao fim de 6 dias em refrigeração. É necessário continuar o estudo para melhorar o novo produto alimentar funcional, mas o presente trabalho permitiu concluir que o hambúrguer de pata-roxa reúne as condições para ter um elevado potencial antioxidante, apresentar maior estabilidade em armazenamento e, em simultâneo, constituir uma solução para o desperdício de pescado.

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O chá é a bebida mais consumida no mundo depois da água, no entanto, é no continente Asiático que é mais consumido. Existem vários tipos diferentes de chá “descendentes” da planta Camellia sinensis. É uma bebida multifacetada e benéfica para o próprio consumidor, devido às suas propriedades organoléticas e propriedades benéficas para a saúde (presença de antioxidantes). Hoje em dia existe uma crescente procura por produtos inovadores, de elevada qualidade nutricional, nomeadamente produtos alimentares com propriedades diuréticas ou dietéticas. Por outro lado, os organismos marinhos têm-se revelado como fonte de compostos bioativos com elevado potencial. Nomeadamente as algas que têm demonstrado produzir moléculas, pelo seu metabolismo secundário, com aplicação alimentar, farmacológica, entre outras. Desta forma, o principal objetivo do trabalho foi avaliar a capacidade da alga Fucus Spiralis, uma alga edível com elevado poder antioxidante, na transferência de antioxidantes durante a preparação de uma tisana, para o desenvolvimento de uma bebida inovadora “chá de alga”. Por outro lado, este trabalho teve também como objetivo fazer uma nova tisana “variante” do chá verde alga Fucus Spiralis. De modo a estudar o melhor processo para a secagem da alga, esta foi seca através de três métodos: liofilização, em estufa e no secador Tray-drier. Para os três métodos foram avaliados vários parâmetros químicos, como a quantificação de polifenóis totais, cor, aW e teor de humidade. As análises foram realizadas logo após a secagem. Ao longo do tempo (60 dias), foi também medido a quantificação de polifenóis com a alga embalada a vácuo e sem estar embalada a vácuo. Finalmente, adicionando a alga, o chá verde e aditivos alimentares, procederam-se a três diferentes processos de conservação: esterilização, pasteurização e filtração (filtro 0,22μm). Após estes tratamentos foi realizado um estudo microbiológico, a variação de cor e a quantificação de polifenóis totais ao longo de 30 dias. O menor valor obtido de aW foi observado para a alga liofilizada. Por outro lado os menores valores de humidade foram obtidos pela secagem por liofilização e pela utilização da estufa ventilada. A realização da tisana de Fucus spiralis revelou a libertação de antioxidantes em todos os processos de secagem e para todas as concentrações testadas (0,1g; 0,5g e 1g/300mL). No entanto, a libertação de polifenóis revelou-se apenas dependente do processo de secagem para a concentração de 0,5 g/300 mL, onde a quantificação total de polifenóis foi superior para o processo de liofilização (0,246 ± 0,049 mg equivalentes de ácido gálico/mL). Este valor não apresentou diferenças estatisticamente significativas com os polifenóis quantificados para a concentração de 1g/300mL. O armazenamento da alga Fucus spiralis ao longo de 60 dias em vácuo ou na ausência de vácuo não provocaram alterações na quantificação total de polifenóis e foi independente do processo de secagem. Durante os 60 dias ocorreu uma diminuição dependente do tempo dos polifenóis libertados para a tisana de alga. Esta diminuição foi particularmente acentuada até aos 15 dias. A formulação de uma tisana com 0,5g da alga Fucus spiralis e 0,5g de chá verde revelou-se, tendencialmente, com maior concentração de polifenóis de que uma tisana com 1 g de chá verde ou 1 g. Para a tisana com 0,5g da alga Fucus spiralis e 0,5g de chá verde o processo de esterilização e pasteurização não impediram o crescimento de microrganismo ao final de 30 dias de armazenamento da tisana. Contrariamente, o processo de filtração garantiu ausência de carga bacteriana durante os 30 dias de armazenamento. Por outro lado os níveis de polifenóis diminuíram ligeiramente ao longo do tempo de armazenamento, mas de um modo independente do processo de conservação. Desta forma, as tisanas de alga (Fucus spiralis) e chá verde desenvolvidas no presente trabalho, quando liofilizadas e filtradas, apresentaram um elevado potencial antioxidante, apresentando-se como um produto inovador para a indústria alimentar.

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In this study we reconstruct sea surface temperatures (SSTs) using two lipid-based biomarker proxies (alkenone unsaturation index UK'37 and TEX86 index based on glycerol dibiphytanyl glycerol tetraethers) in 36 surface sediment samples from the Indonesian continental margin off west Sumatra and south of Java and the Lesser Sunda Islands. Comparison of measured temperatures (World Ocean Atlas 09) to reconstructed temperatures suggests that SST-UK'37 reflects the SE monsoon SST in the upwelling area south of Java and the Lesser Sunda Islands, whereas Temp-TEXH86 estimates are up to 2°C lower than SST-UK'37. This offset is possibly related to either one or a combination of two factors: i) the depth habitats of the source organisms; ii) different seasonal production and/ or seasonality of export associated with phytoplankton blooming triggered by primary productivity. In the non-upwelling area off west Sumatra, the alkenone-based SSTs are cooler than measured temperatures during the entire year, likely due to the reduced sensitivity of the UK'37 proxy beyond 28°C. However, reconstructed temperatures based on TEXH86 are consistent with mean annual SST, implying that the Temp-TEXH86 reflects the mean annual SST in the non-upwelling area of the tropical Eastern Indian Ocean.

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Membrane lipids of marine planktonic archaea have provided unique insights into archaeal ecology and paleoceanography. However, past studies of archaeal lipids in suspended particulate matter (SPM) and sediments mainly focused on a small class of fully saturated glycerol dibiphytanyl glycerol tetraether (GDGT) homologues identified decades ago. The apparent low structural diversity of GDGTs is in strong contrast to the high diversity of metabolism and taxonomy among planktonic archaea. Furthermore, adaptation of archaeal lipids in the deep ocean remains poorly constrained. We report the archaeal lipidome in SPM from diverse oceanic regimes. We extend the known inventory of planktonic archaeal lipids to include numerous unsaturated archaeal ether lipids (uns-AELs). We further reveal i) different thermal regulations and polar headgroup compositions of membrane lipids between the epipelagic (<= 100 m) and deep (> 100 m) populations of archaea; ii) stratification of unsaturated GDGTs with varying redox conditions; and iii) enrichment of tetra-unsaturated archaeol and fully saturated GDGTs in epipelagic and deep oxygenated waters, respectively. Such stratified lipid patterns are consistent with the typical distribution of archaeal phylotypes in marine environments. We thus provide an ecological context for GDGT-based paleoclimatology and bring about the potential use of uns-AELs as biomarkers for planktonic Euryarchaeota. This article is protected by copyright. All rights reserved.

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In this study we utilize two organic geochemical proxies, the Uk'37 index and TEX86, to examine past sea surface temperatures (SST) from a site located near the Nile River Delta in the eastern Mediterranean (EM) Sea. The Uk'37 and TEX86 records generally are in agreement and indicate SST ranges of 14°C-26°C and 14°C-28°C, respectively, during the last 27 cal ka. During the Holocene, TEX86-based SST estimates are usually higher than Uk'37-based SST estimates, which is likely due to seasonal differences between the timing of the haptophyte and crenarchaeota blooms in the EM and is related to the onset of the modern flow regime of the Nile River. Both records show that SST varied on centennial to millennial timescales in response to global climate events, i.e., cooling during the Last Glacial Maximum (LGM), Heinrich event 1 (H1), and the Younger Dryas (YD) and warming during the Bølling-Allerød and in the early Holocene during deposition of sapropel S1. The H1 cooling was particularly severe and is marked by a drop in SST of ~4.5°C in comparison to pre-H1 SST, with temperatures >1°C cooler than during the LGM. In contrast to high-latitude and western Mediterranean records, which indicate both an abrupt onset and termination of the YD event, the transition from the YD to the Holocene was much more gradual in the EM.