Stone Age to recent land-use history at Pegrema, northern Lake Onega, Russian Karelia

The village of Pegrema in Karelia may be regarded as a Stone Age innovation centre in the large Lake Onega area. Two pollen and plant macrofossil diagrams are presented which represent the first contribution to the study of human impact in the area using anthropogenic pollen indicators. A continuous but sporadic human presence from the Mesolithic onwards is demonstrated. While there is no archaeological evidence relating to the period 4200–3000 B.P., the pollen data suggest continuous, though rather sparse human presence. The data do not support any natural catastrophes in Pegrema as has been suggested elsewhere. Cerealia pollen is recorded earlier than expected (c. 5000 B.P.=. In the Bronce Age and Iron Age, the settlement of the Zaonezhye peninsula is reflected by a slight increase in herb pollen representation, sporadic Cerealia pollen and several periods of regression in Picea. The long introductory period of agriculture to the area, as well as the similarities and discrepancies between different sources of evidence (palaeoecological, archaeological and historical) are discussed at some length. The start of land clearance for permanent cultivation in the profile Pegrema S was dated to the late 13^th century. The beginning of more intensive field cultivation in the 15^th century is clearly seen in the pollen succession at both localities. The fluctuation in anthropogenic indicators can be related to population density based on historical data. The village of Pegrema was depopulated in 1956 which is reflected in a distinct decline in settlement indicators. Received February 17 / Accepted May 19, 2000     

Paleoenvironmental study of the Carquefou site (Massif Armoricain, France) from the end of the Sub-boreal

The town of Carquefou, some 10 km northeast of Nantes on the left bank of the river Erdre, occupies a site long associated with human activity. During road construction east of the town, ditches, enclosures and post holes characteristic of the late la Tène were discovered at the locality of “Le Clouet”, which led us to obtain core samples from a nearby peat bog. These investigations indicated the changes in vegetation since 3915±95 uncal B.P., [2828 (2459) 2074 cal B.C.]. The slopes in the surroundings of the bog have been relatively treeless since the Bronze Age, but a very open woodland vegetation composed of Tilia, Corylus and Quercus has been maintained until the present day. In the area around the bog, and Alnus wood with an undergrowth of Cyperaceae was the dominant vegetation, despite some changes probably related to human occupation since the Bronze Age. Beginning at 955±35 uncal B.P. [1004 (1036, 1144, 1146) 1181 cal A.D.], in the Middle Ages, the alders disappeared almost totally, apparently because of clearance or an increase in water level. Human presence led to intensified cultivation of different crops including Cannabis and especially Cerealia. Finally, the presence of a variety of anthropogenic indicator plants (Cichorioideae, Asteraceae, Plantago lanceolata, etc.) suggests that cattle were reared in the vicinity of the site. Received May 22, 2000 / Accepted March 29, 2001     

Palaeoethnobotanical studies of the Neolithic settlement in Hidden Valley, Farafra Oasis, Egypt

The Neolithic site at Hidden Valley, Farafra Oasis, Egypt (6028±150 – 5163±374 cal B. C.) on the shores of a playa (dry lake basin in the desert), yielded a large quantity of carbonized plant remains from post-holes, hearths, querns and a corridor. The plant remains could have become carbonised during food preparation, or when fuel included seeds. Rich and diverse floras were retrieved from 40 soil samples, in all 534 seeds, grains, spikelets, culm fragments and leaflet fragments which were attributed to 30 taxa in the flora of Egypt. Wild grasses from almost all samples represent 83% of the plant remains. Quantitative correlation between plants remains and archaeological contexts is discussed. The highest density of plant remains was recorded from pot-holes (in which pots were stood), while sediments recovered near querns show the lowest. The economy of the site was apparently based mainly on herding associated with the gathering of grasses which suggests that the climate at Farafra during the middle Holocene (6077–4511 cal B. C.) was wetter than today's, with winter and summer rainfall. A reconstruction of the vegetation around the site comprises reed plant cover, aquatic and wetland plants and desert savanna. Received March 8, 2001 / Accepted June, 2001     

Archaeobotanical evidence for early agriculture at Ljubjansko barje (Ljubljana Moor), central Slovenia

Archaeobotanical evidence is presented for early agriculture at southwestern Ljubljansko barje (Ljubljana Moor), Slovenia. Archaeobotanical finds from the Eneolithic site at Hočevarica, and pollen records from an archaeological profile and from a nearby core were analysed. Numerous charred grains of cultivated cereals together with fossil seeds of Chenopodium sp. demonstrate that during the occupation of the settlement at Hočevarica, agriculture was well established. The majority of identified grains were of Hordeum vulgare (cultivated barley) and the rest were Triticum monococcum and T. turgidum ssp. dicoccum (cultivated wheats). Large amounts of cereal pollen and pollen of Chenopodiaceae also suggest strong human impact on the surrounding vegetation and landscape. Pollen and archaeobotanical data from Hočevarica show a large consistency in timing of the appearance of agriculture. In the pollen record from the core at Hočevarica a significant increase (up to 40%) in cereal pollen was detected at 4881 ± 50 B.P. (3770-3630 cal B.C.). Charred cereal grains were dated to 4800 ± 40 B.P. (3650-3520 cal B.C.). The grains of cultivated cereals from Hočevarica represent the oldest archaeobotanical evidence for agriculture in central Slovenia. Received February 18, 2002 / Accepted October 21, 2002     

On the Late Pleistocene and Holocene history of vegetation and human impact in the Ücker valley, north-eastern Germany

A high-resolution Late Pleistocene and Middle to Late Holocene pollen profile of regional significance is presented. The coring site is located in a mire between two lakes. Ober- and Unter-ückersee, in Brandenburg, north-eastern Germany. The study was carried out in an archaeological context. It provides information about the history of vegetation, climate and human impact in the ücker river valley and the surrounding hills, the Uckerm?rker Hügelland. Hence, it is an important contribution for the reconstruction of the past vegetation of this area of Brandenburg. Seven AMS ¹⁴C-dates based on pollen concentrates provide a chronology for the middle Holocene part of the profile. Phases of intensive human activity can be shown from the middle Neolithic times until the Roman Iron Age. Received February 1, 2000 / Accepted January 18, 2001     

Archaeobotany of capers (Capparis) (Capparaceae)

The origins of capers, their use and cultivation are discussed. Capers seeds and charcoal are often recovered from archaeological sites of the Mediterranean and West Asia. These are referred to as C. Spinosa L. This is mostly a group of cultivars restricted to localities surrounding the Western Mediterranean and some places in the Eastern Mediterranean. Identification of the findings is discussed in terms of seed morphology, present distribution and ancient uses of C. aegyptia Lam., C. sicula Veill., C. cartilaginea Decne, C. orientalis Veill., C. decidua (Forssk.) Edgew. and other species. Citations of Capparis in early Rabbinic, Mesopotamian and Greco-Roman texts are presented. Received June 3, 2002 / Accepted October 8, 2002 Correspondence to: D. Rivera     

Mangroves of Oman during the late Holocene; climatic implications and impact on human settlements

Pollen and micropalaeontological analyses carried out on mangrove swamp sediments of Suwayh, Oman (22°05.589'N, 50°40.033'E) reveal environmental changes linked both to climate (monsoon) and geomorphological (sea-level) variations during the Late Holocene. A Rhizophora mangrove developed at Suwayh around 6000 years B. P. under climate conditions marked by an increased tropical influence as compared to the modern situation, with dominant summer rains. The later extension of Prosopis cineraria at Suwayh provides evidence for a different rainfall pattern, with a winter rainy season. Pollen and micropalaeontological composition shows three episodes influenced by the sea water at Suwayh. The most important corresponded to the mangrove episode centred ca 6000 B. P. This was followed by two episodes of slight seawater incursion at ca. 5100 and 4500 B. P. responsible for the formation of a brackish laagon. Comparison based on ¹⁴C measurements on shell recovered from both the sedimentary sequence of Suwayh and the nearby archaeological sites demonstrates that close relations existed between man and mangroves during the Neolithic and the Early Bronze Age. Received October 31, 2001 / Accepted January 24, 2002 Correspondence to: Anne-Marie Lézine     

Punica granatum L. (pomegranates) from early Roman contexts in Vindonissa (Switzerland)

At the later legionary camp of Vindonissa, early Roman (Augustan-Claudian) structures were excavated during a rescue excavation between 1996 and 1998. In phase 2 (10 B.C. until 0), seven in situ carbonised wooden barrels, dug into the ground, were found. They belonged to a rather large building which was most probably used as storage facility. Two of the barrels contained, in the bottom layers, several hundred seeds and pericarp fragments of Punica granatum L. (pomegranates). A large number of other "exotic" plant taxa such as olive, walnut, pine, pistacio, peach, cherry (and probably date) were also found in rather large quantities. Above all, the finds of pomegranates are unique: they are the first finds of this Mediterranean fruit in regions north of the Alps. The origin, use, and other archaeological finds of the pomegranate in the Roman period are discussed. A comparison with other early Roman spectra shows that such large quantities of "exotic" useful plants are mainly present at larger military sites like the legionary camps of Novaesium or Oberaden. It must also be suggested that the pre-camp phases in Vindonissa already had a military charaeter, although this is not at all clear from the other archaeological finds. The precise role of the site is still a matter of debate. Received November 22, 2001 / Accepted February 19, 2002     

Continuity and changes in plant resources during the Neolithic period in western Switzerland

The Neolithic and Bronze Age (4400-1570 B.C.) pile dwellings of Concise-sous-Colachoz on the shore of Lake Neuchatel (Canton of Vaud, western Switzerland), known as an archaeological site for more than 140 years, were recently re-investigated due to rescue excavations. Plant macrofossil analyses were done for several Neolithic occupation phases (3868-2440 B.C. the Cortaillod classique, Cortaillod moyen, Cortaillod tardif and Auvernier periods) with a focus on cereal remains, and additionally, archaeological deposits dating to the Cortaillod moyen culture (3710-3677 B.C.) were studied in detail. The preliminary study of cereal macrofossil remains from all the mentioned Neolithic phases show that the most important cereals were Triticum aestivum/durum/turgidum (naked wheat), T. monococcum (einkorn) and Hordeum vulgare (barley). The preferences for specific crops did obviously not alter significantly through time, but, extraordinarily, significant amounts of einkorn continued to be grown for at least 1400 years during the Neolithic period. Other cultivated plants were Pisum sativum (pea), Linum usitatissimum (flax), and Papaver somniferum (opium poppy). Additionally to the seeds, capsule fragments of opium poppy were found in the Cortaillod moyen deposits. These represent the first finds of uncharred capsule fragments in Europe. Compared with other central European sites, opium poppy was very common during the 38th and 37th cent. B.C. and obviously less appreciated towards the end of the Neolithic in the western part of Switzerland. In central Switzerland the trends seem different: there opium poppy was mainly used during the Late Neolithic period. This may be due to cultural differences within contemporaneous human societies. Wild fruits which were collected as plant resources during the Cortaillod moyen period included Prunus spinosa (sloe), Cornus sanguinea (dogwood), Malus sylvestris (apple), Rubus idaeus/caesius/fruticosus (raspberry/dewberry/blackberry), Fragaria vesca (wild strawberry), Rosa sp. (hip), Quercus sp. (acorn), Corylus avellana (hazelnut), and Fagus sylvatica (beechnut), among others. Compared with other Neolithic sites in westem and central Switzerland the local population of Concise-sous-Colachoz used few sloes, while dogwood fruits were in use throughout the Neolithic period at Lake Neuchatel. Received September 4, 2001 / Accepted May 13, 2002     

Postglacial vegetation history in Luxembourg: new charcoal data from the cave of la Karelslé (Waldbillig, eastern Gutland)

The archaeological site of La Karelslé (Waldbillig, Luxembourg) provides the first important charcoal sequence in Luxembourg for the development of Holocene plant cover. During the Pre-boreal, the results show open woodland vegetation dominated by Pinus sylvestris type in association with Betula sp. and Rosaceae. After an important gap covering the Boreal and the early Atlantic, the data reveal the dominance of a deciduous Quercus woodland with Tilia sp., Fraxinus excelsior and Corylus avellana. Finally during the sub-Boreal, the assemblages indicate a cooler and wetter climate and Quercus woods with Fagus sylvatica and Taxus baccata. There is no clear evidence for human impact. Received June 5, 2001 / Accepted December 3, 2001     

New evidence for the use of root foods in pre-agrarian subsistence recovered from the late Mesolithic site at Halsskov, Denmark

Roots and tubers, together with other plant storage organs such as rhizomes, bulbs, corms, etc. are known to be a source of human food. Until very recently, however, remains of root foods were rarely identified from archaeological contexts in temperate Europe. New evidence for the use of root foods has been recently recovered from the early Erteb?lle settlement at Halsskov in Denmark. Remains included charred bulbs of Allium cf. ursinum and tubers of Conopodium majus. They were accompanied by charred remains of parenchymatous tissues derived from underground parts of other plants. All parenchymatous remains were recovered from features that could be interpreted as pit-cooking depressions. A minimum of two periods of root food gathering can be assumed, spring to early summer and autumn. The presence of charred seeds of Nuphar pumilum suggests that either the seeds or rhizomes (or both) were use as food. Received September 4, 2001 / Accepted February 27, 2002     

The relationship between albumin, other plasma proteins and variables, and age in the acute phase response after liver resection in man

Summary. A large series of plasma albumin (ALB, g/dl) and simultaneous blood and clinical measurements were prospectively performed on 92 liver resection patients, and processed to assess the correlations between ALB, other plasma proteins, additional variables and clinical events. The measurements were performed preoperatively and at postoperative day 1, 3 and 7 in all patients, and subsequently only in those who developed complications or died. In patients who recovered normally ALB was 4.3 ± 0.4 g/dl (mean ± SD) preoperatively, 3.7 ± 0.7 at day 1 and 3, and 3.9 ± 0.4 at day 7. In patients with complications its decrease was more prolonged. In non-survivors it was 3.4 ± 0.4 preoperatively, 3.0 ± 0.4 at day 1, and then decreased further. Regression analysis showed direct correlations between ALB and pseudo-cholinesterase (CHE, U/l, nv 5300-13000), cholesterol (CHOL, mg/dl), iron binding capacity (IBC, mg/dl), prothrombin activity (PA, % of standard reference) and fibrinogen, an inverse correlation with blood urea nitrogen (BUN, mg/dl) for any given creatinine level (CREAT, mg/dl), and weaker direct correlations with hematocrit, other variables and dose of exogenous albumin. An inverse relationship found between ALB and age (AGE, years) became postoperatively (POSTOP) also a function of outcome, showing larger age-related decreases in ALB associated with complications (COMPL: sepsis, liver insufficiency) or death (DEATH). Main overall correlations: CHE = 287.4(2.014)^ALB, r = 0.73; CHOL = 16.5(1.610)^ALB (1.001)^ALKPH, r = 0.71; IBC = 68.6(1.391)^ALB, r = 0.64; PA = 13.8 + 16.0(ALB), r = 0.51; BUN = 21.3 + 20.2(CREAT) – 6.2(ALB), r = 0.91; ALB = 5.0–0.013(AGE) – {0.5 + 0.003(AGE) _COMPL + 0.012(AGE) _DEATH } _POSTOP , r = 0.74 [p < 0.001 for each regression and each coefficient; ALKPH = alkaline phosphatase, U/l, nv 98-279, independent determinant of CHOL; discontinuous variables in italics label the change in regression slope or intercept associated with the corresponding condition]. These results suggest that altered albumin synthesis (or altered synthesis unable to compensate for albumin loss, catabolism or redistribution) is an important determinant of hypoalbuminemia after hepatectomy. The correlations with age and postoperative outcome support the concept that hypoalbuminemia is a marker of pathophysiologic frailty associated with increasing age, and amplified by the challenges of postoperative illness.     

Late Quaternary environmental changes in the Lagoa da Curuça region (eastern Amazonia, Brazil) and evidence of Podocarpus in the Amazon lowland

Late-glacial and Holocene vegetational and climate dynamics and human impact of the eastern Amazon rain forest in the coastal region of eastern Pará State in northern Brazil have been studied in two sedimentary recores from Lagoa da Curu?a. Seven radiocarbon dates provide the chronology for two pollen and charcoal records starting from 11,700 and 9440 uncal B. P. to present. Dense and high diverse terra firme Amazon rain forest in the coastal area shows that there was no savanna during the Late-glacial period. The occurrence of Podocarpus trees in the coastal region during the Late-glacial indicate wet and markedly colder conditions at that time. A possible habitat for Pleistocene populations of Podocarpus trees which are now also evident from several other Amazon regions is discussed. There were no rain forest fires between 11,700 and 10,840 uncal B. P. The increase of charcoal particles in the lake deposits after this period suggest an early Amerindian occupation of the coastal region. Received March 26, 2001 / Accepted August 8, 2001     

The effect of taurine depletion on the contractile properties and fatigue in fast-twitch skeletal muscle of the mouse

Summary. Taurine as well as tauret (retinyliden taurine) levels were measured in locust Locusta migratoria compound eyes. HPLC measurements revealed relatively low taurine levels (1.9 ± 0.16 mM) in dark-adapted eyes. Glutamate, aspartate and glycine levels were 2.0 ± 0.2, 2.7 ± 0.4 and 3.0 ± 0.37 mM, respectively, while GABA was present only in trace amounts. After about 4 h of light adaptation at 1500–2000 lx, amino acid levels in the compound eye were as follows: taurine, 1.8 ± 0.17 mM; glutamate, no change at 2.1 ± 0.2 mM; aspartate sharply increased to 4.7 ± 0.7 mM; glycine slightly decreased to 2.8 ± 0.3 mM; and GABA trace levels. In the compound eye of locust Locusta migratoria, the existence of endogenous tauret in micro-molar range was established. In the dark, levels were several times higher compared with compound eye after light adaptation 1500 lx for 3 h, as estimated by TLC in combination with spectral measurements. Existence of tauret in compound eye is of special interest because in the compound eye, rhodopsin regeneration is based on photoregeneration.     

Extending the chronology of deposits at Blombos Cave, South Africa, back to 140 ka using optical dating of single and multiple grains of quartz

Optically stimulated luminescence (OSL) measurements are reported for both single aliquots (of two different sizes) and single grains of quartz from deposits within Blombos Cave. Ages have been obtained for six sediments from the Middle Stone Age (MSA) occupation levels and for two sterile sands, one underlying the archaeological sediment and one overlying the Later Stone Age occupation levels. The ages for the archaeological sediments were obtained from single-grain measurements that enabled unrepresentative grains to be rejected. The MSA occupation levels have ages that, within error limits, are in stratigraphic order and fall between the OSL age for the oldest dune sand (143.2+/-5.5 ka) and a previously published OSL age for the sterile sand ( approximately 70 ka) that separates the Middle and Later Stone Age deposits. The earliest MSA archaeological phase, M3, from where fragments of ochre were found as well as human teeth, is dated to 98.9+/-4.5 ka, coinciding with the sea-level high of oxygen isotope substage 5c. The cave then appears to be unoccupied until oxygen isotope substage 5a on the basis of four OSL ages for archaeological phase M2, ranging from 84.6+/-5.8 to 76.8+/-3.1 ka; these levels contained large hearths and bone tools. An age of 72.7+/-3.1 ka was obtained for the final MSA archaeological phase, M1, from which deliberately engraved ochre and shell beads were recovered along with bifacial stone points. We conclude that the periods of occupation were determined by changes in sea level, with abundant sources of seafood available in times of high sea level and with the cave being closed by the accumulation of large dunes during periods of low sea level, such as during oxygen isotope stages 4 and 6.     

Decrease of plasma taurine in Gaucher disease and its sustained correction during enzyme replacement therapy

Summary. Gaucher disease is caused by an autosomal-recessive deficiency of glucocerebrosidase. Cells of monocytic/macrophagic origin accumulate glucosylceramide. This leads to hepatosplenomegaly, bone destruction, thrombocytopenia and anemia. Enzyme replacement therapy (ERT) with macrophage-targeted glucocerebrosidase leads to normalization of these parameters. The way of macrophage activation in Gaucher disease is not known. Recently, the osmolytes taurine, betaine and inositol were identified as important regulators of macrophage function in liver. Therefore, the role of plasma taurine in Gaucher disease as a primarily macrophage-derived disease was studied. Fasting plasma levels were measured from blood samples of healthy control subjects (n = 29, m : f = 11 : 18, mean age 37 ± 3 years), from un-treated Gaucher patients (n = 16, m : f = 7 : 9, mean age 44 ± 4 years) and those treated for 37 ± 2 months (n = 54, m : f = 19 : 35, mean age 47 ± 2 years). Amino acid analysis was carried out in a BioChrom amino acid analyzer. In the untreated patients, plasma taurine was 45 ± 3 μM, as compared to the controls with a plasma taurine of 63 ± 4 μM (p < 0.01). The aver-age increase of plasma taurine during the first year of ERT was 18 ± 8 μM (n = 10). Patients treated for an average of 37 months (range 1–9 years of ERT) had a plasma taurine of 65 ± 4 μM (n = 54), which was not different from the controls. It is concluded that Gaucher patients show decreased plasma taurine levels and that therapy of Gaucher disease might correct this. It has to be established, whether decreased taurine availability is a cofactor of the permanent activation of glucosylceramide-storing monocytes/macrophages in this disease. Received January 25, 2000/Accepted January 31, 2000     

The time-profile of the PBMC HSP70 response to in vitro heat shock appears temperature-dependent

Summary. Heat shock proteins (HSPs) are synthesised by cells subsequent to a stress exposure and are known to confer protection to the cell in response to a second challenge. HSP induction and decay are correlated to thermotolerance and may therefore be used as a biomarker of thermal history. The current study tested the temperature-dependent nature of the heat shock response and characterised its time profile of induction. Whole blood from 6 healthy males (Age: 26 ± (SD) 2 yrs; Body mass 74.2 ± 3.8 kgs; VO_2max: 49.1 ± 4.0 ml·kg⁻¹·min⁻¹) were isolated and exposed to in vitro heat shock (HS) at 37, 38, 39, 40, and 41 °C for a period of 90 min. After HS the temperature was returned to 37 °C and intracellular HSP70 was quantified from the leukocytes at 0, 2, 4, and 6 h after heat treatment. The concentration of HSP70 was not different between temperatures (P > 0.05), but the time-profile of HSP70 synthesis appeared temperature-dependent. At control (37 °C) and lower temperatures (38–39 °C) the mean HSP70 concentration increased up to 4 h post HS (P < 0.05) and then returned towards baseline values by 6 h post HS. With in vitro hyperthermic conditions (40–41 °C), the time-profile was characterised by a sharp rise in HSP70 levels immediately after treatment (P < 0.05 for 40 °C at 0 h), followed by a progressive decline over time. The results suggest a temperature-dependent time-profile of HSP70 synthesis. In addition, the temperature at which HSP70 is inducted might be lower than 37 °C.     

Food remains from Bronze Age-Archondiko and Mesimeriani Toumba in northern Greece?

Finds of fragmented cereal grain from the sites of Mesimeriani Toumba and Archondiko in Macedonia, northern Greece, dated to 2100-1900 cal. B.C. provide the basis for the experimental investigation of the effects of a) fragmentation before and after charring, b) treatment of grain with water and c) charring conditions, on the morphology of the fracture surface. The experiments indicate that it is possible to distinguish fragmentation before and after charring and, with low charring temperatures, it is possible to distinguish prior treatment of grain with hot water. Comparison of the archaeological grain with the grain produced experimentally suggests that both archaeologieal finds represent ground grain, and at least those from Mesimeriani correspond to some type of wheat bulgur, probably intended for human consumption. These finds mark the prehistoric origins of a foodstuff widely used in Mediterranean cuisine. Further experimentation along the lines followed here would be desirable. Received January 8, 2002 / Accepted April 1, 2002     

Manifold decrease of sialic acid synthase in fetal Down syndrome brain

Summary. Background: Down syndrome (DS, trisomy 21) is the most common genetic cause of mental retardation. A large series of biochemical defects have been observed in fetal and adult DS brain that help in unraveling the molecular mechanisms underlying mental retardation. Aims: As sialylation of glycoconjugates plays an important role in brain development, this study aimed to look at the sialic acid metabolism by measuring sialic acid synthase (SAS; N-acetylneuraminate synthase) in early second trimester fetal control and DS brain. Results: In this regard, protein profiling was performed by two-dimensional gel electrophoresis coupled to matrix-assisted laser desorption/ionization mass-spectrometry followed by database search and subsequent quantification of spot using specific software. SAS, the enzyme catalyzing synthesis of N-acetyl-neuraminic acid (syn: sialic acid) was represented as a single spot and found to be significantly and manifold reduced (P < 0.01) in cortex of fetuses with DS (control vs. DS, 0.052 ± 0.025 vs. 0.012 ± 0.006). Conclusion: The intriguing finding of the manifold decrease of SAS in DS fetal cerebral cortex as early as in the second trimester of pregnancy may help to explain the brain deficit observed in DS. Decreased SAS may well lead to altered sialic acid metabolism, required for brain development and, more specifically, for sialylation of key brain proteins, including neuronal cell adhesion molecule and myelin associated glycoprotein.     

Enhancement of transglutaminase activity and polyamine depletion in B16-F10 melanoma cells by flavonoids naringenin and hesperitin correlate to reduction of the <Emphasis Type="Italic">in vivo</Emphasis> metastatic potential

Summary. The in vitro and in vivo effects of two flavonons, naringenin (NG) and hesperitin (HP) on the proliferation rate of highly metastatic murine B16-F10 melanoma cell were investigated. NG or HP treatment of melanoma cells produced a remarkable reduction of cell proliferation, paralleled with both the lowering of the intracellular levels of polyamine, spermidine and spermine and the enhancement of transglutaminase (TGase, EC 2.3.2.13) activity. Orally administered NG or HP in C57BL6/N mice inoculated with B16-F10 cells affected the pulmonary invasion of melanoma cells in an in vivo metastatic assay. The number of lung metastases detected by a computerized image analyzer was reduced, compared to untreated animals, by about 69% in NG-treated mice and by about 36% in HP-treated mice. Survival studies showed that 50% of the NG-treated animals died 38 ± 3.1 days after tumor cell injection (control group: 18 ± 1.5 days) and HP-treated mice died 27 ± 2.3 days after cell inoculation. Taken together, these findings provide further evidences for the potential anticancer properties of dietary flavonoids as chemopreventive agents against malignant melanoma.