Late Pleistocene and Holocene palaeoenvironmental changes in central Tierra del Fuego (~54°S) inferred from pollen analysis

A pollen record was obtained from a coring site at La Correntina mire (54°33′S, 66°59′W, 206 m a.s.l.) to the east of Lago Fagnano, centre of Tierra del Fuego. The results indicate that the valley bottom was free of ice shortly before 15,400 cal bp. Pioneer vegetation included dwarf shrub heaths, grasses and herbs with sparsely distributed Nothofagus trees, indicative of dry conditions. Nothofagus expanded by 10,000 cal bp and the forest-steppe ecotone was established by 9,400 cal bp, implying warm conditions and an increase in available moisture. After ca. 5,000 cal bp, the development of a closed-canopy forest is interpreted as the result of wetter and colder conditions. After 3,000 cal bp, Nothofagus forest became more open, and by about 400 cal bp there was a further decline of the forest. A closed-canopy Nothofagus forest re-established after 400 cal bp.     

Vegetation and fire history of coastal north-eastern Sardinia (Italy) under changing Holocene climates and land use

Little is known about the vegetation and fire history of Sardinia, and especially the long-term history of the thermo-Mediterranean belt that encompasses its entire coastal lowlands. A new sedimentary record from a coastal lake based on pollen, spores, macrofossils and microscopic charcoal analysis is used to reconstruct the vegetation and fire history in north-eastern Sardinia. During the mid-Holocene (c. 8,100–5,300 cal bp), the vegetation around Stagno di Sa Curcurica was characterised by dense Erica scoparia and E. arborea stands, which were favoured by high fire activity. Fire incidence declined and evergreen broadleaved forests of Quercus ilex expanded at the beginning of the late Holocene. We relate the observed vegetation and fire dynamics to climatic change, specifically moister and cooler summers and drier and milder winters after 5,300 cal bp. Agricultural activities occurred since the Neolithic and intensified after c. 7,000 cal bp. Around 2,750 cal bp, a further decline of fire incidence and Erica communities occurred, while Quercus ilex expanded and open-land communities became more abundant. This vegetation shift coincided with the historically documented beginning of Phoenician period, which was followed by Punic and Roman civilizations in Sardinia. The vegetational change at around 2,750 cal bp was possibly advantaged by a further shift to moister and cooler summers and drier and milder winters. Triggers for climate changes at 5,300 and 2,750 cal bp may have been gradual, orbitally-induced changes in summer and winter insolation, as well as centennial-scale atmospheric reorganizations. Open evergreen broadleaved forests persisted until the twentieth century, when they were partly substituted by widespread artificial pine plantations. Our results imply that highly flammable Erica vegetation, as reconstructed for the mid-Holocene, could re-emerge as a dominant vegetation type due to increasing drought and fire, as anticipated under global change conditions.     

18,000 years of grassland evolution in the summer rainfall region of South Africa: evidence from Mahwaqa Mountain,KwaZulu-Natal

A palynological and sedimentological record from the Mahwaqa Mountain in KwaZulu-Natal, South Africa, provides evidence of the vegetation dynamics in this part of the Grassland Biome during the last c. 18,000 years. The wetland is located at 1,850 m on an isolated outlier of the Ukhahlamba–Drakensberg Mountain range on an ecotone along a climatic gradient. The vegetation responded to humidity and temperature changes during the late Pleistocene and Holocene. The period c. 18,000–13,500 cal. bp is characterized by high Ericaceae and Restionaceae percentages and decreasing values of charred particles, indicating cool conditions. Around 13,500–8,500 cal. bp, Ericaceae were gradually replaced by Poaceae, signaling climate warming. Growing environmental wetness during the same time period is inferred from Phragmites-type and Cliffortia pollen percentages. Since c. 8,500 cal. bp, Cliffortia, Restionaceae, and Phragmites-type percentages have maintained low levels. Ericaceae were almost completely replaced by grasses and Asteraceae by c. 7,500 cal. bp. All indications are that warm and fluctuating moisture conditions followed until 4,600 cal. bp but they became driest between c. 4,600 and 3,500 cal. bp, when high Asteraceae, Pentzia-type and Scabiosa percentages were prominent. From c. 3,500–800 cal. bp, the increase of sedges, Aponogeton and grass pollen (including Phragmites-type) at the expense of Asteraceae pollen suggests the return of slightly more humid conditions. Since c. 1,000 cal. bp an increase of water demanding Podocarpus and Cliffortia occurred. Pine pollen indicates the recent introduction of alien plants in the 19th and 20th centuries.     

The effects on plasma L-arginine levels of combined oral L-citrulline and L-arginine supplementation in healthy males

We investigated the effects of combining 1 g of l-citrulline and 1 g of l-arginine as oral supplementation on plasma l-arginine levels in healthy males. Oral l-citrulline plus l-arginine supplementation more efficiently increased plasma l-arginine levels than 2 g of l-citrulline or l-arginine, suggesting that oral l-citrulline and l-arginine increase plasma l-arginine levels more effectively in humans when combined.     

An 800 year record of mangrove dynamics and human activities in the upper Gulf of Thailand

A multiproxy record comprising pollen, charcoal, loss on ignition and particle size analyses from two radiocarbon dated sediment cores from Klong Kone subdistrict on the western coast of the Gulf of Thailand provides insights on mangrove dynamics, environmental changes and human activities during the last 800 years. The mangroves were dominated by Rhizophora which indicates that the area has been influenced by the sea level from at least 820 cal bp until 720 cal bp. An intertidal area may have formed that supported mangrove development as part of an old shoreline during 820–720 cal bp. After 720 cal bp, mangroves decreased and were replaced by grasses, suggesting that a lower sea level caused the mangroves to grow closer to the sea until around 140 cal bp. Cereal pollen increased from 720 cal bp suggesting probable use of the shoreline for intensive cultivation. The mangroves were characterised by Avicennia, which increased toward the top of the 2 cores, suggesting that the mangroves then grew further inland, probably due to recent sea-level rise. Intensive human activity is recorded during the 20th century, as indicated by increased particle size, charcoal and carbonate content. At present, human activity in the area includes dams and construction as well as aquaculture.     

Production of l-allose and d-talose from l-psicose and d-tagatose by l-ribose isomerase

l-ribose isomerase (L-RI) from Cellulomonas parahominis MB426 can convert l-psicose and d-tagatose to l-allose and d-talose, respectively. Partially purified recombinant L-RI from Escherichia coli JM109 was immobilized on DIAION HPA25L resin and then utilized to produce l-allose and d-talose. Conversion reaction was performed with the reaction mixture containing 10% l-psicose or d-tagatose and immobilized L-RI at 40 °C. At equilibrium state, the yield of l-allose and d-talose was 35.0% and 13.0%, respectively. Immobilized enzyme could convert l-psicose to l-allose without remarkable decrease in the enzyme activity over 7 times use and d-tagatose to d-talose over 37 times use. After separation and concentration, the mixture solution of l-allose and d-talose was concentrated up to 70% and crystallized by keeping at 4 °C. l-Allose and d-talose crystals were collected from the syrup by filtration. The final yield was 23.0% l-allose and 7.30% d-talose that were obtained from l-psicose and d-tagatose, respectively.     

Mid-Holocene vegetation dynamics with an early expansion of <Emphasis Type="Italic">Mauritia flexuosa</Emphasis> palm trees inferred from the Serra do Tepequém in the savannas of Roraima State in Amazonia,northwestern Brazil

Transition zones between forest and savanna in northern South America are important areas for improving our understanding of ecosystem dynamics and climate change. The uniquely available mid-Holocene sediment deposits from the Serra do Tepequém plateau in Roraima State, northwestern Brazil, were used to analyze past forest-savanna dynamics through pollen, spores, microcharcoal and loss on ignition (LOI). In this newly studied landscape, two distinct periods of vegetation, fire and climate dynamics have been recorded. The first phase from ca. 7,570 to 6,190 cal bp, with the dominance of savanna vegetation in particular with Poaceae and Cyperaceae and some small forest patches with Moraceae/Urticaceae, Alchornea and Schefflera, indicates a relatively dry period. Based on the microcharcoal concentration and influx data, frequent regional fires occurred at that time. The second phase from ca. 6,190 to 4,900 cal bp shows a change in the vegetation composition with an increase of Ilex, Schefflera and Fabaceae. In this period forest expanded, while savanna became reduced, reflecting an increase of wetter conditions. The fire frequency was markedly lower. The first occurrence of Mauritia flexuosa palm was at ca. 7,300 cal bp and an early expansion occurred at around 6,600 cal bp. This early expansion of M. flexuosa showed a development that was in opposition to the increase of fire and savanna expansion found in other regions in northern South America. The increase of wetter conditions in Serra do Tepequém in the mid-Holocene confirms other results found in savannas of Colombia and Venezuela between 7,000 and 6,600 cal bp.     

Structure of a self-assembled single nanotube of cyclo[(-d-Ala-l-Ala)4-]

Diameter and wall thickness of self-assembled peptide nanotube of cyclo[(-d-Ala-l-Ala)₄-] were characterised by molecular simulation. In order to verify the existence of peptide nanotube of cyclo[(-d-Ala-l-Ala)₄-], cyclo[(-d-Ala-l-Ala)₄-] was firstly synthesised through Fmoc solid-phase synthesis method and then self-assembled in trifluoroacetic acid. Based on the results of experiment, the single nanotube structure was further characterised by molecular dynamics (MD) employing the COMPASS force field. The results indicate that cyclo[(-d-Ala-l-Ala)₄-] is self-assembled into nanotube bundles of about 0.5 μm in diameter and 10 μm in length; the inner and outer diameter of the single nanotube is 8.5 and 15.9 Å, respectively, and the nanotube wall thickness is 3.3 Å.     

Kinetic and Equilibrium Studies on d-Mannose-d-Fructose Isomerization Catalyzed by Mannose Isomerase from Streptomyces aerocolorigenes

The equilibrium constant of the isomerization reaction between d-mannose and d-fructose which is catalyzed by a mannose isomerase from Streptomyces aerocolorigenes was obtained by using three methods over the temperature range from 1 to 40°C.

It was found that the equilibrium constant was scarcely dependent on temperature, ΔH, the heat of the formation of d-fructose from d-mannose, being approximately zero.

The standard free energy change, ΔG, and the standard entropy change, ΔS, of the reaction were calculated from the equilibrium constants at various temperatures and ΔH. The values of ΔG and ΔS at 25°C were ?650 cal/mole and + 2.2 cal/deg·mole, respectively.

By combining these thermodynamic data with those obtained for the isomerization reaction between d-glucose and d-fructose reported in the previous paper, ΔH, ΔG and ΔS for the isomerization between d-mannose and d-glucose were indirectly obtained to be +2220 cal/mole, +830 cal/mole and +4.6 cal/deg·mole at 25°C, respectively.     

Purification and Crystallization of d-Arabinose (l-Fucose) Isomerase from Aerobacter aerogenes by Polyethylene Glycol

d-Arabinose(l-fucose) isomerase (d-arabinose ketol-isomerase, EC 5.3.1.3) was purified from the extracts of d-arabinose-grown cells of Aerobacter aerogenes, strain M-7 by the procedure of repeated fractional precipitation with polyethylene glycol 6000 and isolating the crystalline state. The crystalline enzyme was homogeneous in ultracentrifugal analysis and polyacrylamide gel electrophoresis. Sedimentation constant obtained was 15.4s and the molecular weight was estimated as being approximately 2.5 × 10⁵ by gel filtration on Sephadex G-200.

Optimum pH for isomerization of d-arabinose and of l-fucose was identical at pH 9.3, and the Michaelis constants were 51 mm for l-fucose and 160 mm for d-arabinose. Both of these activities decreased at the same rate with thermal inactivation at 45 and 50°C. All four pentitols inhibited two pentose isomerase activities competitively with same Ki values: 1.3–1.5 mm for d-arabitol, 2.2–2.7 mm for ribitol, 2.9–3.2 mm for l-arabitol, and 10–10.5 mm for xylitol. It is confirmed that the single enzyme is responsible for the isomerization of d-arabinose and l-fucose.     

Identification and characterization of d-arabinose reductase and d-arabinose transporters from Pichia stipitis

d-xylose and l-arabinose are the major constituents of plant lignocelluloses, and the related fungal metabolic pathways have been extensively examined. Although Pichia stipitis CBS 6054 grows using d-arabinose as the sole carbon source, the hypothetical pathway has not yet been clarified at the molecular level. We herein purified NAD(P)H-dependent d-arabinose reductase from cells grown on d-arabinose, and found that the enzyme was identical to the known d-xylose reductase (XR). The enzyme activity of XR with d-arabinose was previously reported to be only 1% that with d-xylose. The k_cat/K_m value with d-arabinose (1.27 min^?1 mM^?1), which was determined using the recombinant enzyme, was 13.6- and 10.5-fold lower than those with l-arabinose and d-xylose, respectively. Among the 34 putative sugar transporters from P. stipitis, only seven genes exhibited uptake ability not only for d-arabinose, but also for d-glucose and other pentose sugars including d-xylose and l-arabinose in Saccharomyces cerevisiae.     

Isolation of Radiosensitive Mutants of Micrococcus radiodurans

Sulfated polysaccharides (SP) isolated from freshwater green algae, Spirogyra neglecta (Hassall) Kützing, and fractionated SPs were examined to investigate their molecular characteristics and immunomodulatory activity. The crude and fractionated SPs (F₁, F₂, and F₃) consisted mostly of carbohydrates (68.5–85.3%), uronic acids (3.2–4.9%), and sulfates (2.2–12.2%) with various amounts of proteins (2.6–17.1%). d-galactose (23.5–27.3%), d-glucose (11.5–24.8%), l-fucose (19.0–26.7%), and l-rhamnose (16.4–18.3%) were the major monosaccharide units of these SPs with different levels of l-arabinose (3.0–9.4%), d-xylose (4.6–9.8%), and d-mannose (0.4–2.3%). The SPs contained two sub-fractions with molecular weights (M_w) ranging from 164 × 10³ to 1460 × 10³ g/mol. The crude and fractionated SPs strongly stimulated murine macrophages, producing considerable amounts of nitric oxide and various cytokines via up-regulation of their mRNA expression by activation of nuclear factor-kappa B and mitogen-activated protein kinases pathways. The main backbone of the most immunoenhancing SP was (1→3)-l-Fucopyranoside, (1→4,6)-d-Glucopyranoside, and (1→4)-d-Galactopyranoside.     

Investigation of peat sediments from Daiyun Mountain in southeast China: late Holocene vegetation,climate and human impact

In this study, late Holocene vegetation, climate and human impacts were investigated using multiproxy data-pollen percentages, pollen accumulation rates (PAR), humification and loss-on-ignition (LOI)—measured from peat sediments from Daiyun Mountain, southeast China. A stratigraphic chronology was established on the basis of four radiocarbon dates. The 4,350 year sequence of vegetation history and climate change exhibits three distinctive stages: (1) 4,350–1,000 cal bp, during which the vegetation was dominated by evergreen forests mainly composed of broad-leaf trees, indicating a warm and wet climate; (2) 1,000–550 cal bp, during which the climate was thought to be cool and dry, based on a decrease in pollen percentages and the PARs of trees, shrubs and wetland herbs, and an increase in the pollen percentage and PAR of dry land herbs, as well as high overall LOI values; and (3) 550 cal bp to modern times, during which higher pollen percentages of dry land and wetland herbs, along with low pollen percentage and PAR of trees and shrubs, as well as low absorbance and LOI values, suggest relatively cooler but wetter climate conditions. In addition, major climatic events, such as the warm period from ad 670–960, the Medieval Warm Period (ad 1050–1520) and the Little Ice Age (ad 1580–1850), could be identified within the peat sediments in this study, with climatic conditions at these times being characteristically warm and wet, warm and dry, and cold and wet, respectively. Pollen signals indicate significant human impact since 1,000 cal bp, which may be linked to the development of the local porcelain industry and a rapid increase in the population in the study region.     

Two novel pyrrolooxazole pigments formed by the Maillard reaction between glucose and threonine or serine

Pyrrolothiazolate formed by the Maillard reaction between l-cysteine and d-glucose has a pyrrolothiazole skeleton as a chromophore. We searched for a Maillard pigment having a pyrrolooxazole skeleton formed from l-threonine or l-serine instead of l-cysteine in the presence of d-glucose. As a result, two novel yellow pigments, named pyrrolooxazolates A and B, were isolated from model solutions of the Maillard reaction containing l-threonine and d-glucose, and l-serine and d-glucose, respectively, and identified as (2R,3S,7aS)-2,3,7,7a-tetrahydro-6-hydroxy-2,5,7a-trimethyl-7-oxo-pyrrolo[2,1-b]oxazole-3-calboxylic acid and (3S,7aS)-2,3,7,7a-tetrahydro-6-hydroxy-5,7a-dimethyl-7-oxo-pyrrolo[2,1-b]oxazole-3-calboxylic acid by instrumental analyses. These compounds were pyrrolooxazole derivatives carrying a carboxy group, and showed the absorption maxima at 300–360 nm under acidic and neutral conditions and at 320–390 nm under alkaline conditions.     

Production of l-rhamnulose,a rare sugar,from l-rhamnose using commercial immobilized glucose isomerase

Abstract

A commercial immobilized d-glucose isomerase from Streptomyces murines (Sweetzyme) was used to produce l-rhamnulose from l-rhamnose in a packed-bed reactor. The optimal conditions for l-rhamnulose production from l-rhamnose were determined as pH 8.0, 60?°C, 300?g L^?1 l-rhamnose as a substrate, and 0.6?h^?1 dilution rate. The half-life of the immobilized enzyme at 60?°C was 809?h. Under the optimal conditions, the immobilized enzyme produced an average of 135?g L^?1 l-rhamnulose from 300?g L^?1 l-rhamnose after 16 days at pH 8.0, 60?°C, and 0.6?h^?1 dilution rate, with a productivity of 81?g/L/h and a conversion yield of 45% in a packed-bed reactor.     

Prodigiosin-25 C

The equilibrium constant of the isomerization reaction between d-glucose and d-fructose which is catalyzed by a. glucose isomerase from Streptomyces sp. was obtained by both methods of chemical analysis and of kinetic study over the temperature range of 25° to 70°C.

It was found that the formation of d-fructose from d-glucose was an endothermic reaction with the heat of the reaction, ΔH, of +2220 cal/mole. The standard free energy change, ΔG, and the standard entropy change, ΔS, associated with the isomeric change were found to be +180 cal/mole and + 6.8 cal/deg. mole at 25°C, respectively. The values of these thermodynamic quantities at other temperature are also summarized.     

Studies on the Acid-Protease of Paecilomyces varioti Bainier TPR-220

The acid-protease of Paecilomyces varioti Bainier TPR-220 can hydrolyze carbobenzoxy-l-glutamyl-l-tyrosine, which is the substrate for pepsin, the acid-protease of Aspegillus saitoi by Yoshida and of Asp. oryzae by Nunokawa, and the trypsinogenkinase by Nakanishi, and benzoyl-l-argininamide, which is the substrate for trypsin, papain, and above two acid-proteases, optimally at pH 3.5 and 5.5 at 45°C, respectively. The Michaelis constant and activation energy of the enzyme are 4.08 × 10^-3m and 9.17 × 10³ cal/mol for the former, and 6.58 × 10^-3m and 6.86 × 10³ cal/mol for the latter, respectively.

Other substrates for papain, chymotrypsin, and various exopeptidases are hardly hydrolyzed by the enzyme.     

Crystalline d-Mannitol:NAD Oxidoreductase from Leuconostoc mesenteroides

The crystalline d-mannitol dehyrogenase (d-mannitol:NAD oxidoreductase, EC 1.1.1.67) catalyzed the reversible reduction of d-fructose to d-mannitol. d-Sorbitol was oxidized only at the rate of 4% of the activity for d-mannitol. The enzyme was inactive for all of four pentitols and their corresponding 2-ketopentoses. The apparent optimal pH for the reduction of d-fructose or the oxidation of d-mannitol was 5.35 or 8.6, respectively. The Michaelis constants were 0.035 m for d-fructose and 0.020 m for d-mannitol. The enzyme was also found to be specific for NAD. The Michaelis constans were 1 × 10^?5 m for NADH₂ and 2.7 × 10^?4 m for NAD.     

Optimal Conditions for the Enzymatic Production of l-Aromatic Amino Acids from the Corresponding 5-Substituted Hydantoins

The reaction conditions for the production of l-tryptophan from dl-5-indolyl- methylhydantoin by Flavobacterium sp. AJ-3940, and the cultural conditions for the formation of the enzyme involved by this bacterium were investigated. The optimal pH of this reaction was around 8.5 and the optimal temperature was between 45 to 55°C. The amount of l-tryptophan produced was remarkably increased by the addition of inosine, which formed a water insoluble adduct with l-tryptophan, to the reaction mixture because of the release of end-product inhibition by l-tryptophan. This enzyme was inducibly and intracellularly produced by Flavobacterium sp. AJ-3940 in proportion to the increase in cell growth. Cells showing high activity were obtained using a medium containing 5 g glucose, 5 g (NH₄)₂SO₄, 1 g KH₂PO₄, 3 g K₂HPO₄, 0.1 g MgSO₄ · 7H₂O, 0.01 g CaCl₂ · 2H₂O, 50 ml corn steep liquor and 3.5 g dl-5-indolylmethylhydantoin in a total volume of 1 liter (pH 7.0). Under the best conditions, 43 mg/ml of l-tryptophan was produced from 50 mg/ml of dl-5-indolylmethylhydantoin with a molar yield of 97% in the presence of cells of Flavobacterium sp. AJ-3940. In addition, other l-aromatic amino acids such as l-phenylalanine, l-tyrosine, l-DOPA and related l-amino acids were also produced from the corresponding 5-substituted hydantoins by this bacterium containing the l-tryptophan-producing enzyme induced by dl-5-indolylmethylhydantoin.