extracted with EDTA) to total primary production (TPP) were rneasured using "C-tracer to estirnate the ratio for each fraction of organic carbon photosynthetically produced by microphytobenthos and phytoplankton. TEOC for rn.icrophytobenthos ranged frorn 4 2 to 73% of TPP and was rnade up mostly of 14C-Colloidal-OC The TEOC/TPP for phytoplankton ranged frorn 1.5 to 220,). The ratio of I4C-EPS to I4C-CoUoidal-OC for rnicrophytobenthos was 41 to 53%, and for phytoplankton was 4.4 to 24%. Algal species in the transitional phase were used for experiments because microphytobenthos Nitzschia hybridaeformis most abundantly produced TEOC and EPS in the transitional phase during growth in experirnents studying the effect of the growth phase. By using EDTA for the extraction of extraceUular organic matter, it beComes clear that excretion of colloidal organic matter by rnicrophytobenthos has always been underestimated. These results suggest that the large arnount of TEOC containing EPS produced by microphytobenthos plays a more mportant role than secretion of phytoplankton as a source of organic carbon for heterotrophic organisms in the intertidal-flat ecosystem.

No abstract

Whole Fusobacterium species, but not F. nucleatum, are common in UC patients and have a role in persistence of colonic inflammation in UC. However, Fusobacterium infection is associated with rather mild clinical phenotypes of UC.

Background. Gastric cancer is discovered even after successful eradication of H. pylori. We investigated clinic pathological features of early gastric cancers after H. pylori eradication. Methods. 51 early gastric cancers (EGCs) from 44 patients diagnosed after successful H. pylori eradication were included as eradication group. The clinic-pathological features were compared with that of 131 EGCs from 120 patients who did not have a history of H. pylori eradication (control group). Results. Compared with control group, clinic-pathological features of eradication group were characterized as depressed (p < 0.0001), reddish (p = 0.0001), and smaller (p = 0.0095) lesions, which was also confirmed in the comparison of six metachronous lesions diagnosed after initial ESD and subsequent successful H. pylori eradication. Prevalence of both SM2 (submucosal invasion greater than 500 μm) and unexpected SM2 cases tended to be higher in eradication group (p = 0.077, 0.0867, resp.). Prevalence of inconclusive diagnosis of gastric cancer during pretreatment biopsy was also higher in the same group (26.0% versus 1.6%, p < 0.0001). Conclusions. Informative clinic pathological features of EGC after H. pylori eradication are depressed, reddish appearances, which should be treated as a caution because histological diagnosis of cancerous tissue is sometimes difficult by endoscopic biopsy.

On 11 March 2011, a massive tsunami generated by a mega‐earthquake with a moment magnitude of 9.0 hit a wide area of Pacific coast of northeast Japan. We observed and analyzed the effects of the earthquake and tsunami event on populations of the abalone Haliotis discus hannai and sea urchin Strongylocentrotus nudus at Tomarihama in Miyagi, where we have carried out regular surveys since January 2008. Before the event, algal forests dominated by the brown macroalga Eisenia bicyclis had developed in the survey area shallower than 5 m in depth, where adult abalone >50 mm in shell length (SL) inhabited. Juvenile abalone <20 mm SL and juvenile and adult urchins inhabited the deeper area dominated by crustose coralline algae (CCA). After the event, although no apparent decrease was observed in the brown macroalgal population, the mean density of adult abalone >50 mm SL, mainly inhabiting the algal forests, was reduced by more than half. The impact of the tsunami was more profound in the CCA area than in the macroalgal forest. Juvenile abalone and urchins largely decreased to 14 and 5% of the densities just before the event, respectively. The distribution pattern of juvenile abalone and urchins could be a cause of the marked decrease, because most of these animals inhabited the CCA area where the disturbance by the massive water movement was not reduced by the effects of the macroalgal forest.