Espressione di geni correlati allo stress ossidativo nell'ascidia coloniale Botryllus schlosseri esposta a diverse condizioni ambientali nella Laguna di Venezia

I pattern di espressione genica permettono di valutare se gli organismi siano soggetti a stress ambientali, spesso associati a stress ossidativo e produzione di specie reattive dell’ossigeno, che possono essere analizzate per studiare gli effetti sub-letali indotti dall’ambiente negli organismi. Scopo di questa ricerca è stato valutare la possibilità di utilizzo dell’ascidia coloniale B. schlosseri come biomarker in ambiente lagunare. Le colonie, esposte a diverse condizioni ambientali nella Laguna di Venezia, sono state confrontate con esemplari allevati in condizioni di controllo. La ricerca si è concentrata in 2 siti con diverso grado di idrodinamicità e impatto antropico. Mentre nel sito 1, più vicino alla bocca di porto, si è rilevata la presenza di Tunicati, il sito 2 ne è privo. Il sito 2 ha registrato valori di pH e temperatura più alti. Inoltre, nel sito 2 è stata rilevata una mortalità maggiore delle colonie e alterazioni della morfologia nelle colonie sopravvissute. Ciò suggerisce che il sito 2 presenti condizioni avverse per B. schlosseri. Sui campioni di B. schlosseri sono state eseguite PCR semiquantitative per analizzare l’espressione di un gruppo di geni coinvolto nella risposta allo stress ossidativo: la glutammato cistein ligasi la glutatione sintetasi, 2 isoforme di glutatione perossidasi e la superossido dismutasi (SOD). Tutti i geni presentano livelli di trascrizione doppi nelle colonie del sito 1 rispetto al controllo. Viceversa, il sito 2 mostra livelli di espressione di poco superiori al controllo. Analisi spettrofotometriche evidenziano che le attività enzimatiche di SOD e catalasi sono più alte nel sito 2 rispetto al sito 1. Si può pertanto ipotizzare che le colonie esposte al sito 2 siano soggette a un maggiore stress. B. schlosseri appare dunque un buon indicatore dello stato ecologico dell’ambiente lagunare, entro parametri di pH e temperatura in cui abitualmente vive.

温度影响轮虫卵割速度卵割规律和星状体移动速度之研究

<正> 一.绪言从初期胚胎发育过程和发生生理的研究,知道卵的性质有全能与限能的不同。全能卵(regulative egg)的初期发育,在某一固定的温度下,卵的每次分割是按冪次式(exponential type)而进行,每完成一有丝分裂周期(mitotic cycle)所需的时间都相同。这种情形,早经 Gray,Balinsky,和 Syngajemskaja 等,备就 Echinus miliaris,Ascidia(Ciona intestinalis)和 Campanularie,等动物卵的观察,先

Benthos fauna in the North Sea from 2 surveys in 1986 and 1987

During two surveys in the North Sea, in summer 1986 and in winter 1987, larger epibenthos was collected with a 2 m beam trawl. The distributions of the species were checked for average linkage by means of the JACCARD-index cluster analysis. In summer two main clusters can be recognized. These are situated to the north and to the south of the Dogger Bank. In winter two main clusters may be recognized as well, but these clusters divide the North Sea into a western and an eastern part. We conclude, that these differences of epibenthos characteristics are correlated with seasonal changes in water body distributions.

Ascidiofauna in the Southern Ocean

Three Spanish Antarctic research cruises (Ant-8611, Bentart-94 and Bentart-95) were carried out in the South Shetland Archipelago (Antarctic Peninsula) and Scotia Arc (South Orkney, South Sandwich and South Georgia archipelagos) on the continental shelf and upper slope (10-600 m depth). They have contributed to our knowledge about ascidian distribution and the zoogeographical relationships with the neighbouring areas and the other Subantarctic islands. The distribution of ascidian species suggests that the Scotia Arc is divided into two sectors, the South Orkney Archipelago, related to the Antarctic Province, and the South Georgia Archipelago (probably including the South Sandwich Archipelago), which is intermediate between the Antarctic Province and the Magellan region.

Response of nannoplankton to major changes in sea-surface temperature at the South Chatham Rise, southeastern New Zealand

A high-resolution history of paleoceanographic changes in the subpolar waters of the southern margin of the Subtropical Convergence Zone during the last 130 kyr, is present in foraminiferal assemblages of DSDP Site 594. The foraminifera indicate that sea-surface temperatures during the Last Interglacial Climax were warmer than today, and that between substage 5d through to the end of isotope stage 2, temperatures were mostly cooler than Holocene temperatures. The paleotemperatures suggest that (1) the Subtropical Convergence was located over the site during substage 5e, later moving further north, then moving southwards to near the site during the Holocene, and (2) the Polar Front was positioned over the Site during glacial stages 6, 4, 2 and possibly parts of stage 3. Several major events are indicated by the nannofloral assemblages during these large changes in sea-surface temperature and associated reorganization of ocean circulation. First, the time-progressive trends between E. huxleyi and medium to large Gephyrocupsa are unique to this site, with E. huxleyi dominating over medium Gephyrocupsa during stages 5c-a, middle part of stage 4 and after the middle point of stage 3. This unusual trend may (at least partly) be caused by the shift of the Polar Front across the site. Second, upwelling flora (E. huxleyi and small placoliths) increase in abundance during stages 1, 3 and 5, suggesting that upwelling or disturbance of water stratification took place during the interglacials. Thirdly, there are no significant differences between the distribution patterns of the various morphotypes of medium to large Gephyrocupsu, and the combined value of all medium Gephyrocupsu increases in abundance during glacials (stages 2 and 4 and the end of stage 6), similar to the abundance trends in benthic foraminifera. Finally, subordinate nannofossil taxa also show distinctive climatic trends during the last glacial cycle: (1) Syrucosphaera spp. are present in increased abundance during warmer extremes in climate (substages 5e, 5a, and stage 1); (2) Coccolithus pelagicus and Culcidiscus leptoporus dominate the subordinate nannofossil taxa, and their relative proportions seem to provide a useful paleoceanographic index, with C. pelagicus dominating when the Polar Front Zone is over the site (stages 6, 4 and 2), whilst C. leptoporus is relatively more abundant when the STC is positioned over the site (stages 1 and 5e). Increased abundance of C. pelagicus also can indicate intensified coastal upwelling.