A comprehensive anatomical characterization and radiographic study of stage III testicular cancer in a 31-year-old male patient

The purpose of this investigation was to characterize an unusual case of stage III testicular germ cell tumor (TGCT) in a 31-year-old male with metastases to nodes, bone, viscera and brain, and to understand all possible routes of metastatic disease. Testicular cancer (TC) has an increasing incidence worldwide, and its etiology, risk factors and pathogenesis are not completely understood. Medical records were reviewed, and the cadaveric specimen evaluated by physical examination and gross dissection. Paraffin embedded tissue sections of the primary tumor were stained with Hematoxylin and Eosin (H&E) for histological study. To examine metastatic spread, pre- and post-mortem digital radiologic image acquisition was done using x-ray films, and high- resolution CT Scans and MRI Scans. Image analysis, multi-planar reformatting, and three- dimensional (3-D) reconstruction were done on radiographic series. Dissection showed masses bilaterally from the apex through the lung base; masses on the internal thoracic wall, and hepatomegaly and splenomegaly with multiple tumor masses. Testicular parenchyma was composed of primitive germ cells that formed glomeruloid or embryonal-like structures, as well as areas with a micro-cystic histologic pattern and areas of fibrous dysplasia. Medical imaging 3- D video radiographic dissection was notable for a 38.45 mm diameter, mid-brain tumor; extreme hepatomegaly with numerous tumors, lung tumors, a large penetrating tumor of the left ilium, and multiple tumors throughout both lungs and the thoracolumbar spine (T5-S1). This study provides insight into the histology and metastatic spread of TGCT that is essential for clinicians to understand in the evaluation and treatment of TC patients

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Implications for food safety of the uptake by tomato of 25 trace-elements from a phosphogypsum amended soil from SW Spain.

Phosphogypsum (PG) has been usually applied as Ca-amendment to reclaim sodic soils such as those in the marshland area of Lebrija (SW Spain). This work aimed at the effects of PG amendments on the uptake of trace-elements by tomato and its implications for food safety. A completely randomized experiment was performed using a representative soil from Lebrija in a greenhouse involving six replicates and four PG treatments equivalent to 0, 20, 60, and 200 Mg ha(-1). Soil-to-plant transfer factors (TFs) were determined for Be, B, Al, Ti, V, Cr, Mn, Fe, Co, Ni, Cu, Zn, As, Se, Sr, Mo, Ag, Cd, Sb, Cs, Ba, Tl, Pb, Th and U. The highest TF in shoots was observed for Cd (4.0; 1.5 in fruits), its concentration being increased with increasing PG doses due to its content in this metal (2.1 mg Cd kg(-1)PG). Phosphogypsum applying decreased the concentrations of Mn, Co and Cu in shoots; and of B, Cu, Sb, Cs, Ba, Tl and Th in fruits, however enhanced the accumulation of Se in fruits. Although Cd concentrations in tomato were below the maximum allowed levels in control pots (0 Mg PG ha(-1)), PG amendments above 60 Mg ha(-1) exceeded such limits.

Reversed flow of Atlantic deep water during the Last Glacial Maximum.

The meridional overturning circulation (MOC) of the Atlantic Ocean is considered to be one of the most important components of the climate system. This is because its warm surface currents, such as the Gulf Stream, redistribute huge amounts of energy from tropical to high latitudes and influence regional weather and climate patterns, whereas its lower limb ventilates the deep ocean and affects the storage of carbon in the abyss, away from the atmosphere. Despite its significance for future climate, the operation of the MOC under contrasting climates of the past remains controversial. Nutrient-based proxies and recent model simulations indicate that during the Last Glacial Maximum the convective activity in the North Atlantic Ocean was much weaker than at present. In contrast, rate-sensitive radiogenic (231)Pa/(230)Th isotope ratios from the North Atlantic have been interpreted to indicate only minor changes in MOC strength. Here we show that the basin-scale abyssal circulation of the Atlantic Ocean was probably reversed during the Last Glacial Maximum and was dominated by northward water flow from the Southern Ocean. These conclusions are based on new high-resolution data from the South Atlantic Ocean that establish the basin-scale north to south gradient in (231)Pa/(230)Th, and thus the direction of the deep ocean circulation. Our findings are consistent with nutrient-based proxies and argue that further analysis of (231)Pa/(230)Th outside the North Atlantic basin will enhance our understanding of past ocean circulation, provided that spatial gradients are carefully considered. This broader perspective suggests that the modern pattern of the Atlantic MOC-with a prominent southerly flow of deep waters originating in the North Atlantic-arose only during the Holocene epoch.