Estimating estuarine residence times in the Westerschelde (The Netherlands) using a box model with fixed dispersion coefficients

The residence time of the water masses in the Westerschelde estuary was determined using a simple compartment-model that simulates the advective-diffusive transport of a conservative dissolved substance (chlorinity). The residence time of a water parcel in the upstream part of the estuary (i.e. the time needed for this water parcel to leave the estuary) varied from about 50 days in winter to about 70 days in summer. The most seaward compartment had residence times of about 10-15 days.Dispersive coefficients that are fixed in time were able to reproduce the observed salinity distributions very well in the Westerschelde. They were obtained by calibration on observed chlorinities. It is argued that the apparent relationship of dispersive coefficients with freshwater flow, which is observed in certain studies, could (partly) reflect the deviation from steady state conditions which are required assumptions to calculate these dispersive coefficients directly from salinity profiles.     

Carbon flows in the Westerschelde estuary (The Netherlands) evaluated by means of an ecosystem model (MOSES)

The autotrophic production and heterotrophic consumption of organic matter in the Westerschelde, a highly turbid and eutrophic estuary in the Southwest Netherlands is examined by means of a dynamic simulation model. The model describes the ecologically relevant processes in thirteen spatial compartments and adequately fits most observed data.Three autotrophic processes are included in the model. Net pelagic photosynthetic production is relatively low (average 41 gC m^–2 yr^–1) and three spatial compartments near the turbidity maximum zone are respiratory sinks of phytoplankton biomass. According to the model, net phytobenthic primary production is more important than pelagic primary production in the upstream half of the Westerschelde. On the scale of the entire estuary, benthic primary production amounts to about 60% of pelagic primary production. Water-column nitrification, which is very important in the nitrogen cycle, is most pronounced near the turbidity zone where it accounts for the major autotrophic fixation of carbon (up to 27 g C m^–2 yr^–1). Viewed on the scale of the total estuary, however, the process is not very important.Less than 20% of total organic carbon input to the estuary is primary produced, the remainder is imported from waste discharges and from the river.The degree of heterotrophy of the Westerschelde estuary proved to be one of the highest yet reported. On average 380 g carbon per square metre is net lost per year (range 200–1200 gC m^–2 yr^–1). The yearly community respiration (bacterial mineralization, respiration of higher trophic levels and sedimentation) is 4 to 35 times (estuarine mean of 6) higher than the net production. This degree of heterotrophy is highest near the turbidity maximum and generally decreases from the freshwater to the seaward boundary. About 75% of all carbon losses can be ascribed to pelagic heterotrophic processes; the sediment is only locally important.Mineralisation rates are highest in the turbidity region, but as only a fraction of total carbon resides here, less than 20% of all organic carbon is lost in this part of the estuary. This result is in contradiction with a previous budget of the estuary, based on data of the early seventies, where more than 80% of all carbon was estimated to be lost in the turbidity zone. Part of this discrepancy is probably caused by changes that have occurred in the estuary since that time.Due to the high heterotrophic activity, nearly all imported and in situ produced carbon is lost in the estuary itself and the Westerschelde is an insignificant source of organic matter to the coastal zone.The model estuary acts as a trap for reactive organic matter, both from the land, from the sea or in situ produced. Internal cycling, mainly in the water column, results in the removal of most of the carbon while the more refractory part is exported to the sea.     

Insulin-like growth factor-1 stimulates amino acid uptake by the cultured human placental trophoblast

Amino acid uptake by the human placenta is known to occur via several transport mechanisms. However, regulation by extracellular factors has received relatively little attention. A recent report by this laboratory characterized the uptake of α-aminoisobutyric acid (AIB) stimulated by insulin in the cultured human placental trophoblast The current study evaluated the effect of insulin-like growth factor-1 (IGF-1) on AIB uptake in cultured human placental trophoblasts. Na⁺-dependent AIB uptake was significantly stimulated by IGF-l in a time-dependent manner, as early as 30 min after hormone exposure. The maximum effect was at 2–4 hr of continuous exposure to IGF-l and the stimulation was dependent upon IGF-1 concentration approaching maximal stimulation at 50 ng.ml^?1. AIB uptake was inhibited by increasing concentrations of α-(methylamino)isobtyric acid (MeAIB). Approximately 75% of basal (unstimulated) Na⁺-dependent AIB uptake was inhibited by MeAIB. The IGF-1-stimulated increment above basal AIB uptake was completely inhibited by MeAIB. IGF-1 increased the maximum uptake yelocity but not Km. Using equimolar concentrations, stimulation was greater with IGF-1 then with IGF-2. Stimulation by IGF-1, but not insulin, was inhibited by anit-IGF-1 receptor antibody, indicating mediation via the IGF-1 receptor. H7, a nonspecific inhibitor of serine-threonine kinase, inhibited IGF-1-dependent stimulation of AIB uptake. In addition, calphostin C (a specific inhibitor of protein kinase C), but not H89 (a specific inhibitor of protein kinase A), inhibited the IGF-1 action. This study further characterizes regulated amino acid uptake by the human placental trophoblasts and demonstrates that the Na⁺-dependent component of AIB uptake is stimulated by physiologic concentrations of IGF-1. © 1995 Wiley-Liss Inc.     

Phylogenetic relationships among transposon-like elements in human and primate DNA

A THE-1 sequence in intron 7 of the human dystrophin gene has been found to represent a new subfamily of THE-1 elements. The sequence is closely related to the MstII family of repetitive sequences and is more like single-copy sequences found in the galago genome than any other THE-1 sequence previously reported. This new THE-1 sequence has been compared with two other complete THE-1 sequences and three related long-terminal repeat elements that we have previously found in intron 7 of the dystrophin gene, and with members of the same family from elsewhere in the primate genome. Parsimony and deletion analysis show that the cluster of THE-1 sequences in intron 7 of the dystrophin gene has arisen from at least three individual insertion events, rather than from the insertion and duplication of a single progenitor sequence. Correspondence to: G.B. Petersen     

Ligand-Induced Translocation of Epidermal Growth Factor Receptor to the Nucleus of NR6/HER Fibroblasts Is Serum Dependent

Ligand-induced translocation of epidermal growth factor receptors (EGF-R) to the nucleus of NR6/HER fibroblasts has been studied by immunoelectron microscopy. Following treatment of NR6/HER cells with epidermal growth factor (EGF) for 1 h, there was a decrease in EGF-R labeling at the plasma membrane and a corresponding increase in EGF-R in the nucleus. This was preceded by a rapid and sustained increase in nuclear phosphotyrosine content, detectable within 2 min of EGF treatment. EGF-R translocation into the nucleus was completely prevented by 18 h serum starvation prior to treatment with EGF. These results indicate that translocation of EGF-R to the nucleus is a controlled process and they suggest theft EGF-R may directly influence nuclear function.