Coherence between solar activity and the East Asian winter monsoon variability in the past 8000 years from Yangtze River-derived mud in the East China Sea

AMS(14)C dating and grain-size analysis for Core PC-6, located in the middle of a mud area on the inner shelf of the East China Sea (ECS), were used to rebuild the Holocene history of the East Asian winter monsoon (EAWM). The 7.5-m core recorded the history of environmental changes during the postglacial transgression. The core's mud section (the upper 450 cm) has been formed mainly by suspended sediment delivered from the Yangtze River mouth by the ECS Winter Coastal Current (ECSWCC) since 7.6 kyr BP. Using a mathematical method called "grain size vs. standard deviatioW', we can divide the Core PC-6's grain-size distribution into two populations at about 28 mu m. The fine population (< 28 mu m) is considered to be transported by the ECSWCC as suspended loads. Content of the fine population changes little and represents a stable sedimentary environment in accord with the present situation. Thus, variation of mean grain-size from the fine population would reflect the strength of ECSWCC, which is mainly controlled by the East Asian winter monsoon. Abrupt increasing mean grain size in the mud section is inferred to be transported by sudden strengthened ECSWCC, which was caused by the strengthened EAWM. Thus, the high resolution mean grain-size variation might serve as a proxy for reconstruction of the EAWM. A good correlation between sunspot change and the mean grain-size of suspended fine population suggests that one of the primary controls on centennial- to decadal-scale changes of the EAWM in the past 8 ka is the variations of sun irradiance, i.e., the EAWM will increase in intensity when the number of sunspots decreases. Spectral analyses of the mean grain-size time series of Core PC-6 show statistically significant periodicities centering on 2463, 1368, 128, 106, 100, 88-91, 7678, and 70-72 years. The EAWM and the East Asian summer monsoon (EASM) agree with each other well on these cycles, and the East Asian Monsoon (EAM) and the Indian Monsoon also share in concurrent cycles in Holocene, which are in accord with the changes of the sun irradiance. (c) 2005 Elsevier B.V. All rights reserved.

Nutrient Dynamics in the Upwelling Area of Changjiang (Yangtze River) Estuary

Nutrient dynamics and its influence on the distribution of chlorophyll-a in the upwelling area of the Changjiang (Yangtze) River estuary were investigated in the spring (May) and summer (August) of 2004. In the spring, upwelling was apparent in the region of 122 degrees 20'-123 degrees 00' E, 31 degrees 00'-32 degrees 00' N and was associated with low temperature (16-21 degrees C), high salinity (24-33 practical salinity units [psu]), and low dissolved oxygen (2.5-6.0 mg L-1) in the upper 10 m of the water column. The spring upwelling increased the mixed-layer phosphate, nitrate, and silicate concentrations to roughly 1, 15, and 15 mu mol L-1, respectively, and improved the light transparency in the euphotic zone. This improvement in phytoplankton growing conditions was followed by an increase in chlorophyll-a concentrations. The summer upwelling was weaker and occurred over a smaller geographical area (122 degrees 20'-123 degrees 00' E, 31 degrees 15'-31 degrees 50' N). Strongly influenced by turbid Changjiang diluted water (CDW), it had little impact on the upper 10 m of the water column but instead increased nutrient concentrations at greater depths. The high concentration of particulates in the CDW reduced light transmission in the upper 10 m and, hence, limited phytoplankton growth throughout the water column. Chlorophyll-a concentrations in the summer upwelling area were roughly an order of magnitude lower than in the spring. Water clarity, as influenced by the CDW, appears to be the principal factor limiting the impact of upwelling on phytoplankton biomass in this area.

Size-fractionated phytoplankton biomass in autumn of the Changjiang (Yangtze) River Estuary and its adjacent waters after the Three Gorges Dam construction

A cruise was undertaken from 3rd to 8th November 2004 in Changjiang (Yangtze) River Estuary and its adjacent waters to investigate the spatial biomass distribution and size composition of phytoplankton. Chlorophyll-a (Chl-a) concentration ranged 0.42-1.17 mu g L-1 and 0.41-10.43 mu g L-1 inside and outside the river mouth, with the mean value 0.73 mu g L-1 and 1.86 mu g L-1, respectively. Compared with the Chl-a concentration in summer of 2004, the mean value was much lower inside, and a little higher outside the river mouth. The maximal Chl-a was 10.43 mu g L-1 at station 18 (122.67 degrees E, 31.25 degrees N), and the region of high Chl-a concentration was observed in the central survey area between 122.5 degrees E and 123.0 degrees E. In the stations located east of 122.5 degrees E, Chl-a concentration was generally high in the upper layers above 5 m due to water stratification. In the survey area, the average Chl-a in sizes of > 20 mu m and < 20 mu m was 0.28 mu g L-1 and 1.40 mu g L-1, respectively. High Chl-a concentration of < 20 mu m size-fraction indicated that the nanophytoplankton and picophytoplankton contributed the most to the biomass of phytoplankton. Skeletonema costatum, Prorocentrum micans and Scrippsiella trochoidea were the dominant species in surface water. The spatial distribution of cell abundance of phytoplankton was patchy and did not agree well with that of Chl-a, as the cell abundance could not distinguish the differences in shape and size of phytoplankton cells. Nitrate and silicate behaved conservatively, but the former could probably be the limitation factor to algal biomass at offshore stations. The distribution of phosphate scattered considerably, and its relation to the phytoplankton biomass was complicated.

Inorganic carbon of sediments in the Yangtze River Estuary and Jiaozhou Bay

JGOFS results showed that the ocean is a major sink for the increasing atmospheric carbon dioxide resulting from human activity. However, the role of the coastal seas in the global carbon cycling is poorly understood. In the present work, the inorganic carbon (IC) in the Yangtze River Estuary and Jiaozhou Bay are studied as examples of offshore sediments. Sequential extraction was used to divide inorganic carbon in the sediments into five forms, NaCl form, NH3 H2O form, NaOH form, NH2OH HCl form and HCl form. Studied of their content and influencing factors were also showed that NaCl form < NH3 H2O form < NaOH form < NH2OH HCl form < HCl form, and that their influencing factors of pH, Eh, Es, water content, organic carbon, organic nitrogen, inorganic nitrogen, organic phosphorus and inorganic phosphorus on inorganic carbon can be divided into two groups, and that every factor has different influence on different form or on the same form in different environment. Different IC form may transform into each other in the early diagenetic process of sediment, but NaCl form, NH3 H2O form, NaOH form and NH2OH HCl form may convert to HCl form ultimately. So every IC form has different contribution to carbon cycling. This study showed that the contribution of various form of IC to the carbon cycle is in the order of NaOH form > NH2OH HCl form > NH3 H2O form > NaCl form > HCl form, and that the contribution of HCl form contributes little to carbon cycling, HCl form may be one of end-result of atmospheric CO2. So Yangtze River estuary sediment may absorb at least about 40.96x10(11) g atmospheric CO2 every year, which indicated that offshore sediment play an important role in absorbing atmospheric CO2.

Miniatures for Horn Trio.

This three movement work was first performed by members of the Research Ensemble at the Peninsula Arts Contemporary Music Festival, 26 February 2010. Material from the first movement reappears in the second and third in various guises. The second movement is dedicated to the choreographer, Merce Cunningham, and the constant piano part with pedal sustained throughout is a reference to the fluidity of dance. As a contrast to this there are passages of imitation between the horn and violin, some more audible than others, which are included as an acknowledgement of the intimate relationship which exists between co-dancers on stage. The third movement is dedicated to John Cage (Cunningham's partner) and, while the piano sustains chords (reworking content from the first movement), the gestures in the other parts loosely follow the outline of sections of one of Cage's watercolours, River Rocks and Smoke no.6. Much of my music is inspired by visual art and, having admired Cage's music and writings since by student days, it seemed appropriate after dedicating the second movement to Cunningham, to turn to Cage's art work in the final part of the composition.

Micromorphology of lamellae formed in an alluvial soil, Big Pine Tree Archeological Site, South Carolina

The formation of lamellae in soils is not clearly understood. The objectives of this study are to examine the microscopical characteristics of selected well developed lamellae inorder to identify the major processes involved in their formation at the Big Pine Tree Archaeological site on the Savannah River, South Carolina. Well developed lamellae have formed in a fine sandy alluvial soil that is about 11,000 to 12,000 years old. In the field, these lamellae are observed as 1 to 4.2 cm thick horizontal layers having a smooth upper and a wavy, sometimes irregular, lower boundary with adjacent interlamellae horizons. Soil thin sections reveal denser accumulations of brown fine silt and clay coatings in the upper and lower sections of the lamellae. The center of the lamellae has mainly orange highly oriented discontinuous clay coatings bridging quartz grains and some silt accumulations. Although, horizontal layering of denser areas (accumulations of fine silt and clay coatings) is also observed in the middle of the lamellae. The interlamellae horizons are mainly loose quartz grains. Low total carbon values (

A PRELIMINARY ASSESSMENT OF THE DISTRIBUTION OF THE SEA LAMPREY (PETROMYZON MARINUS L.), RIVER LAMPREY (LAMPETRA FLUVIATILIS (L.)) AND BROOK LAMPREY (LAMPETRA PLANERI (BLOCH)) IN NORTHERN IRELAND

Lampreys are endangered in Europe, and European states are legally required to take measures to ensure their protection. However, there is currently little information on the distribution of the three species present in Northern Ireland. Anecdotal records of adult lampreys were collated from anglers and other sources, and a systematic electrofishing survey was undertaken to establish the distribution of lamprey ammocoetes. Lampreys were found in seven of the nine Northern Irish river catchments. Brook lampreys (Lampetra planeri (Bloch)) were widely distributed, but the two anadromous species, sea lamprey (Petromyzon marinus L.) and river lamprey (Lampetra fluviatilis (L.)), were more limited in their distribution, possibly due to barriers restricting migration.

Complex pattern of genetic structuring in the Atlantic salmon (Salmo salar L.) of the River Foyle system in northwest Ireland: disentangling the evolutionary signal from population stochasticity

Little is known about the microevolutionary processes shaping within river population genetic structure of aquatic organisms characterized by high levels of homing and spawning site fidelity. Using a microsatellite panel, we observed complex and highly significant levels of intrariver population genetic substructure and Isolation-by-Distance, in the Atlantic salmon stock of a large river system. Two evolutionary models have been considered explaining mechanisms promoting genetic substructuring in Atlantic salmon, the member-vagrant and metapopulation models. We show that both models can be simultaneously used to explain patterns and levels of population structuring within the Foyle system. We show that anthropogenic factors have had a large influence on contemporary population structure observed. In an analytical development, we found that the frequently used estimator of genetic differentiation, F-ST, routinely underestimated genetic differentiation by a factor three to four compared to the equivalent statistic Jost's D-est (Jost 2008). These statistics also showed a near-perfect correlation. Despite ongoing discussions regarding the usefulness of "adjusted" F-ST statistics, we argue that these could be useful to identify and quantify qualitative differences between populations, which are important from management and conservation perspectives as an indicator of existence of biologically significant variation among tributary populations or a warning of critical environmental damage.

Genome analysis of a simultaneously predatory and prey-independent, novel Bdellovibrio bacteriovorus from the River Tiber, supports in silico predictions of both ancient and recent lateral gene transfer from diverse bacteria

BACKGROUND: Evolution equipped Bdellovibrio bacteriovorus predatory bacteria to invade other bacteria, digesting and replicating, sealed within them thus preventing nutrient-sharing with organisms in the surrounding environment. Bdellovibrio were previously described as "obligate predators" because only by mutations, often in gene bd0108, are 1 in ~1x10(7) of predatory lab strains of Bdellovibrio converted to prey-independent growth. A previous genomic analysis of B. bacteriovorus strain HD100 suggested that predatory consumption of prey DNA by lytic enzymes made Bdellovibrio less likely than other bacteria to acquire DNA by lateral gene transfer (LGT). However the Doolittle and Pan groups predicted, in silico, both ancient and recent lateral gene transfer into the B. bacteriovorus HD100 genome.

RESULTS: To test these predictions, we isolated a predatory bacterium from the River Tiber- a good potential source of LGT as it is rich in diverse bacteria and organic pollutants- by enrichment culturing with E. coli prey cells. The isolate was identified as B. bacteriovorus and named as strain Tiberius. Unusually, this Tiberius strain showed simultaneous prey-independent growth on organic nutrients and predatory growth on live prey. Despite the prey-independent growth, the homolog of bd0108 did not have typical prey-independent-type mutations. The dual growth mode may reflect the high carbon content of the river, and gives B. bacteriovorus Tiberius extended non-predatory contact with the other bacteria present. The HD100 and Tiberius genomes were extensively syntenic despite their different cultured-terrestrial/freshly-isolated aquatic histories; but there were significant differences in gene content indicative of genomic flux and LGT. Gene content comparisons support previously published in silico predictions for LGT in strain HD100 with substantial conservation of genes predicted to have ancient LGT origins but little conservation of AT-rich genes predicted to be recently acquired.

CONCLUSIONS: The natural niche and dual predatory, and prey-independent growth of the B. bacteriovorus Tiberius strain afforded it extensive non-predatory contact with other marine and freshwater bacteria from which LGT is evident in its genome. Thus despite their arsenal of DNA-lytic enzymes; Bdellovibrio are not always predatory in natural niches and their genomes are shaped by acquiring whole genes from other bacteria.

Towards a budget approach to Pleistocene terraces: preliminary studies using the River Exe in South West England, UK

This paper presents a first approach to using a sediment budget methodology for paired terrace staircase sediments in SW England. Although a budget approach has become firmly established in Holocene fluvial studies, it has not been used in Pleistocene sequences due to the problems of temporal resolution, catchment changes and downstream loss from the system. However, this paper uses a budget approach in a paired non-glaciated basin, primarily as a method of interrogating the terrace record concerning the degree of reworking and new sediment input required to produce the reconstructed terrace sequences. In order to apply a budget approach a number of assumptions have to be made and these are justified in the paper. The results suggest that the Exe system can most parsimoniously be explained principally by the reworking of a Middle Pleistocene floodplain system with relatively little input of new resistant clasts required and a cascade-type model in geomorphological terms. Whilst this maybe partially a result of the specific geology of the catchment, it is likely to be representative of many Pleistocene terrace systems in NW Europe due to their litho-tectonic similarities. This cascade-type model of terrace formation has archaeological implications and sets the context for the Palaeolithic terrace record in the UK. Future work will involve the testing of this and similar budget models using a combination of landscape modelling and chronometric dating. ?? 2009 The Geologists' Association.

Effects of fluvial and marine processes on nearshore suspended sediment concentrations off the Elwha River

Senior thesis written for Oceanography 444

Ermittlung geeigneter Methoden zur Differenzierung und Qualitätsbeurteilung unterschiedlicher Milchqualitäten aus verschiedenen on-farm-Experimenten

Zusammenfassung: Ziel der Arbeit war ein Methodenvergleich zur Beurteilung der Milchqualität unterschiedlicher Herkünfte. Am Beispiel von Milchproben aus unterschiedlicher Fütterung sowie an Milchproben von enthornten bzw. horntragenden Kühen wurde geprüft, welche der angewendeten Methoden geeignet ist, die Vergleichsproben zu unterscheiden (Differenzierungsfähigkeit der Methoden) und inwieweit eine Qualitätsbeurteilung möglich ist (hinsichtlich Milchleistung, Fett-, Eiweiß-, Lactose- (=F,E,L), Harnstoff-gehalt und Zellzahl (=SCC), Säuerungseigenschaften (=SE), Fettsäuremuster (=FS-Muster), Protein- und Metabolit-Zusammensetzung (=Pr&M), Fluoreszenz-Anregungs-Spektroskopie-Eigenschaften (=FAS) und Steigbild-Merkmalen). Zusätzlich wurde vorab die Steigbildmethode (=SB-M) für das Produkt Rohmilch standardisiert und charakterisiert, um die Reproduzierbarkei der Ergebnisse sicherzustellen. Die Untersuchungen zur SB-M zeigten, dass es Faktoren gibt, die einen deutlichen Einfluß auf die Bildmerkmals-Ausprägung aufweisen. Dazu gehören laborseitig die Klimabedingungen in der Kammer, die Verdünnungsstufe der Probe, die Standzeiten der Vorverdünnung (Reaktionen mit der Luft, Alterung usw.), und tagesspezifisch auftretende Effekte, deren Ursache unbekannt ist. Probenseitig sind sehr starke tierindividuelle Effekte auf die Bildmerkmals-Ausprägung festzustellen, die unabhängig von Fütterung, Alter, Laktationsstadium und Genetik auftreten, aber auch Fütterungsbedingungen der Kühe lassen sich in der Bildmerkmals-Ausprägung wiederfinden. Die Art der Bildauswertung und die dabei berücksichtigten Bildmerkmale ist von großer Bedeutung für das Ergebnis. Die im Rahmen dieser Arbeit untersuchten 46 Probenpaare (aus den Fütterungsvergleichen (=FV) und zur Thematik der Hörner) konnten in 91% der Fälle korrekt gruppiert werden. Die Unterschiede konnten benannt werden. Drei FV wurden auf drei biologisch-dynamischen Höfen unter Praxis-Bedingungen durchgeführt (on-farm-Experimente). Es wurden jeweils zwei vergleichbare Gruppen à mindestens 11 Kühen gebildet, die im Cross-Over-Design gefüttert wurden, mit Probennahme am 14. und 21. Tag je Periode. Es wurden folgende FV untersucht: A: Wiesenheu vs. Kleegrasheu (=KG-Heu), B: Futterrüben (=FuR) vs. Weizen (Ergänzung zu Luzernegrasheu ad lib.), C: Grassilage vs. Grasheu. Bei Versuch A sind die Futtereffekte am deutlichsten, Gruppeneffekte sind gering. Die Milch der Wiesenheu-Variante hat weniger CLA’s und n3- FS und mehr mittellangkettige FS (MCT-FS), das Pr&M-Muster weist auf „Gewebereifung und Ausdifferenzierung“ vs. bei KG-Heu „Nährstoff-fülle, Wachstum und Substanz-Einlagerung und die SB zeigen fein ausdifferenzierte Bildmerkmale. Bei Versuch B sind die Futtereffekte ähnlich groß wie die Gruppeneffekte. Bei vergleichbarer Milchleistung weist die Milch der FuR-Variante höhere F- und E-Gehalte auf, sie säuert schneller und mehr, das FS-Muster weist auf eine „intensive“ Fütterung mit vermehrt MCT- FS, und die Pr&M-Untersuchungen charakterisieren sie mit „Eisentransport und Fetttröpfchenbildung“ vs. bei Weizen „mehr Abwehr-, Regulations- und Transportfunktion“ /. „mehr Lipidsynthese“. Die SB charakterisieren mit „große, kräftige Formen, verwaschen“ vs. „kleine, ausdifferenzierte Bildmerkmal“ für FuR vs. Weizen. Die FAS charakterisiert sie mit „Saftfutter-typisch“ vs. „Samentypisch“. Versuch C weist die geringsten Futtereffekt auf, und deutliche Gruppen- und Zeiteffekte. Milchleistung und F,E,L-Gehalte zeigen keinen Futtereffekt. Die Milch der Heu-Variante säuert schneller, und sie weist mehr SCT und MCT- FS auf. Pr&M-Untersuchungen wurden nicht durchgeführt. Die SB charakterisieren bei Heumilch mit „fein, zart, durchgestaltet, hell“, bei Silagemilch mit „kräftig, wäßrig-verwaschen, dunkler“. Die FAS kann keine konsistenten Unterschiede ermitteln. Der Horn-Einfluß auf die Milchprobe wurde an 34 Probenpaaren untersucht. Von 11 Höfen wurden je zwei möglichst vergleichbare Gruppen zusammengestellt, die sich nur im Faktor „Horn“ unterscheiden, und im wöchentlichen Abstand drei mal beprobt. F,E,L, SCC und SE der Proben sowie die FAS-Messungen weisen keine konsistenten signifikanten Unterschiede zwischen den Horn-Varianten auf. Pr&M weisen bei den untersuchten Proben (von zwei Höfen) auf Horneffekte hin: bei Eh eine Erhöhung von Immun-Abwehr-Funktionen, sowie einer Abnahme phosphorylierter C3- und C6-Metabolite und Beta-Lactoglobulin. Mit den SB ließen sich für die gewählten Merkmale (S-Größe und g.B.-Intensität) keine Horneffekte feststellen. FS, Pr&M-Muster sowie Harnstoffgehalt und SB (und z.T. Milchleistung) zeigten je FV ähnliche Effekt-Intensitäten für Futter-, Gruppen- und Zeiteffekte, und konnten die Cross-Over-Effekte gut wiedergeben. F- und E-Gehalte konnten neben tierindividuellen Effekten nur in FV B auch Futtereffekte aufzeigen. In FV C zeigten die SE der Proben den deutlichsten Futtereffekt, die anderen Methoden zeigten hier vorrangig Gruppen-Effekte, gefolgt von Futter- und Zeiteffekten. Die FAS zeigte den SB vergleichbare Ergebnisse, jedoch weniger sensibel reagierend. Die Interpretation von Qualitätsaspekten war bei konsistent differenzierbaren Proben (FV A, B, C) am fundiertesten mit Hilfe der FS möglich, da über die Synthese von FS und beeinflussende Faktoren schon vielfältige Erkenntnisse vorliegen. Das Pr&M-Muster war nach einer weiteren Methodenentwicklung bei der Deutung von Stoffwechselprozessen sehr hilfreich. Die FAS konnte z.T. eine zu der Fütterungsvariante passende Charakterisierung liefern. Für die SB-M fehlt es noch an Referenzmaterial, um Angaben zu Qualitätsaspekten zu machen, wenngleich Probenunterschiede aufgezeigt und Proben-Eigenschaften charakterisiert werden konnten.

You and me, little bear.

Little Bear desea jugar con Big Bear, pero éste siempre tiene cosas que hacer. Cuando no ayuda a Big Bear en los menesteres caseros, él juega solo a saltar, a deslizarse, a balancearse de la rama de un árbol, a hacer el pino. Pero Big Bear si encuentra un rato para cumplir el deseo de Little Bear.

Can't you sleep, little bear?

El osito no puede dormir pues tiene miedo a la oscuridad aunque el papa Oso le ha colocado un gran farol encendido sobre la cama para que no se asuste. El Gran Oso encuentra una ingeniosa manera de tranquilizarlo. Existe un libro para el alumno con el mismo título en formato pequeño. .

Flow controls on lowland river macrophytes: A review

We review the current status of knowledge regarding the role that flow parameters play in controlling the macrophyte communities of temperate lowland rivers. We consider both direct and indirect effects and the interaction with other factors known to control macrophyte communities. Knowledge gaps are identified and implications for the management of river systems considered. The main factors and processes controlling the status of macrophytes in lowland rivers are velocity (hence also discharge), light, substrate, competition, nutrient status and river management practices. We suggest that whilst the characteristics of any particular macrophyte community reflect the integral effects of a combination of the factors, fundamental importance can be attributed to the role of discharge and velocity in controlling instream macrophyte colonisation, establishment and persistence. Velocity and discharge also appear to control the relative influence of some of the other controlling factors. Despite the apparent importance of velocity in determining the status of macrophyte communities in lowland rivers, relatively little is understood about the nature of the processes controlling this relationship. Quantitative knowledge is particularly lacking. Consequently, the ability to predict macrophyte abundance and distribution in rivers is still limited. This is further complicated by the likely existence of feedback effects between the growth of macrophytes and velocity. Demand for water resources increases the pressure on lowland aquatic ecosystems. Despite growing recognition of the need to allocate water for the needs of instream biota, the inability to assess the flow requirements of macrophyte communities limits the scope to achieve this. This increases the likelihood of overexploitation of the water resource as other users, whose demands are quantifiable, are prioritised. (C) 2008 Elsevier B.V. All rights reserved.