Ultrastructural studies on Cymbomonas tetramitiformis (Prasinophyceae). I. General structure, scale microstructure, and ontogeny

2003 ◽  
Vol 81 (7) ◽  
pp. 657-671 ◽  
Author(s):  
Øjvind Moestrup ◽  
Isao Inouye ◽  
Terumitsu Hori

The marine prasinophycean flagellate Cymbomonas tetramitiformis has been established in culture from Japan and Australia and is examined in detail by electron microscopy. The results are described as a series of reports, the first of which deals with the general cell structure and the structure and morphogenesis of the organic scales that cover the surface of the cell and the flagella. The cell produces seven types of organic scales, all of which are manufactured in the cisternae of the Golgi apparatus. Two scale types are deposited on the cell body and cover the cell in three close-fitting layers, two types are confined to the flagellar pit region, and three types cover the flagellar surfaces. Cymbomonas is quadriflagellate and closely related to another quadriflagellate, Pyramimonas, in scale structure and scale ontogeny. It differs markedly in cell symmetry, swimming behavior, and in details of the flagellar apparatus. The flagellar end of the cell with the flagellar pit is surrounded by a horseshoe-shaped rim, which is very different from the usually four-lobed anterior end of Pyramimonas. Cymbomonas also shows resemblance in scale structure to members of the order Mamiellales, notably Mamiella, and to the phycoma-producing genera Pterosperma and Halosphaera. The Japanese isolate of Cymbomonas formed cysts for a short period, and the cyst appears to be homologous with the so-called phycoma stage of Pterosperma and Halosphaera. Since two chloroplasts were seen in the cysts, the cysts probably arise as a result of sexual reproduction. Concomitant with the presence of cysts in the culture, tiny uniflagellate cells were also present, and they probably represent gametes. Cymbomonas was described from the Adriatic in 1913 and was not reported again anywhere until 1986 and 1987 when Throndsen refound it in the Gulf of Naples in southern Italy. It has subsequently been found in large parts of the world and is now readily recognized by its characteristic scales and mode of swimming. It is often common but does not appear to form blooms.Key words: Prasinophyceae, marine nanoplankton, ultrastructure, Cymbomonas.

2021 ◽  
Author(s):  
Laurie Charrieau ◽  
Katsunori Kimoto ◽  
Delphine Dissard ◽  
Beatrice Below ◽  
Kazuhiko Fujita ◽  
...  

<p>Ocean acidification is a consequence of current anthropogenic climate changes. The concomitant decrease in pH and carbonate ion concentration in sea water may have severe impacts on calcifying organisms. Coral reefs are among the first ecosystems recognized vulnerable to ocean acidification. Within coral reefs, large benthic foraminifera (LBF) are major calcium carbonate producers.</p><p>The aim of this study was to evaluate the effects of varying pH on survival and calcification of the symbiont-bearing LBF species <em>Peneroplis</em> spp. We performed culture experiments to study their resistance to ocean acidification conditions, as well as their resilience once placed back under open ocean pH (7.9).</p><p>After three days, small signs of test decalcification were observed on specimens kept at pH 7.4, and severe test decalcification was observed on specimens kept at pH 6.9, with the inner organic lining clearly appearing. After 32 days under pH 7.4, similar strongly decalcified specimens were observed. All the specimens were alive at the end of the experiment. This result demonstrates the resistance of <em>Peneroplis </em>spp. to an acidified pH, at least on a short period of time.</p><p>After being partially decalcified, some of the living specimens were placed back at pH 7.9. After one month, the majority of the specimens showed recalcification features, mostly by addition of new chambers. The trace elements concentrations of the newly formed chambers were analysed by LA-ICPMS. Interestingly, more chambers were added when food was given, which highlights the crucial role of energy source in the recalcification process. Moreover, the newly formed chambers were most of the time abnormal, and the general structure of the tests was altered, with potential impacts on reproduction and in situ survival. In conclusion, if symbiont-bearing LBF show some resistance and resilience to lowered pH conditions, they will remain strongly affected by ocean acidification.</p>


1983 ◽  
Vol 73 (1) ◽  
pp. 187-200
Author(s):  
Edoardo Del Pezzo ◽  
Giovanni Iannaccone ◽  
Marcello Martini ◽  
Roberto Scarpa

abstract The seismic activity associated with the catastrophic southern Italy earthquake was monitored by 11 seismic stations operating before this event, within an epicentral distance of 200 km, and by 32 additional short-period seismometers installed soon after the main shock. The hypocenter of this event was located at 40°46′N and 15°18′E, at 16 km depth. The fault-plane solution reveals normal faulting, with tensile axis dipping 18° and oriented orthogonal to the axis of the Apennines chain. This mechanism is in good agreement with the stress pattern inferred from some previous earthquakes and the local seismotectonics. The hypocenter locations of more than 600 aftershocks, with local magnitudes greater than 2.4, show a pronounced alignment extending for about 70 km, oriented north 120° and scattered laterally less than 15 km. These events are mostly concentrated between 8 and 16 km depth. A cluster of aftershocks occurred close to the hypocenter of the main shock covering a region elongated 25 km which corresponds also to the highly damaged area. No significant spreading of the aftershock area with time is observed, but one of the events with higher magnitude (ML = 4.8, 14 February 1981) is displaced 20 km NW from the tip of the aftershock region. The time evolution of the number of aftershocks fits well Omori's hyperbolic law with a decay coeffcient of 1.07 ± 0.06. The possibility of a future delayed multiple sequence of large events, as already observed in the past along the central and southern Apennines, is discussed. In particular, a relatively high seismic potential seems to exist along the northern boundary of the 1980 rupture segment.


2005 ◽  
Vol 343 (1-3) ◽  
pp. 83-95 ◽  
Author(s):  
Barbara Naso ◽  
Daniele Perrone ◽  
Maria Carmela Ferrante ◽  
Marcella Bilancione ◽  
Antonia Lucisano

2018 ◽  
Vol 6 (4) ◽  
pp. 365-380 ◽  
Author(s):  
Luca Appolloni ◽  
Roberto Sandulli ◽  
Carlo Nike Bianchi ◽  
Giovanni Fulvio Russo

1991 ◽  
Vol 136 (1) ◽  
pp. 127-141 ◽  
Author(s):  
Edoardo Del Pezzo ◽  
Marcello Martini ◽  
Giuliano Milana

2016 ◽  
Vol 16 (12) ◽  
pp. 2485-2500 ◽  
Author(s):  
Carmela Vennari ◽  
Mario Parise ◽  
Nicoletta Santangelo ◽  
Antonio Santo

Abstract. This study presents an historical database of flash flood events in the Campania region of southern Italy. The study focuses on small catchments characterized by intermittent flow, generally occurring during and after heavy rainstorms, which can be hydrologically defined as small Mediterranean catchments. As the outlet zones of these catchments (consisting mainly of alluvial fans or fan deltas) are highly urbanized in Campania, the population living in the delivery areas is exposed to high risk. Detailed scrutiny and critical analysis of the existing literature, and of the data inventory available, allowed us to build a robust database consisting of about 500 events from 1540 to 2015, which is continuously updated. Since this study is the first step of a longer project to perform a hazard analysis, information about time and site of occurrence is known for all events. As for the hazard analysis envisaged, collecting information about past events could provide information on future events, in terms of damage and also spatial and temporal occurrence. After introducing the issue of flash floods in Italy we then describe the geological and geomorphological settings of the study area. The database is then presented, illustrating the methodology used in collecting information and its general structure. The collected data are then discussed and the statistical data analysis presented.


2006 ◽  
Vol 111 (B10) ◽  
Author(s):  
Luca D'Auria ◽  
Enrica Marotta ◽  
Marcello Martini ◽  
Patrizia Ricciolino

2020 ◽  
Author(s):  
Stefano Carlino ◽  
Vincenzo Convertito ◽  
Anna Tramelli ◽  
Vincenzo De Novellis ◽  
Nicola Alessandro Pino

<p>We report here a first comparative analysis between recent and historical earthquakes, occurred in the island of Ischia (Southern Italy), which produced heavy damages and thousands of fatalities. The island of Ischia is located in the Gulf of Naples, and represents a peculiar case of resurgent caldera in which volcano-tectonic earthquakes, with low magnitude, have generated large damages and catastrophic effects, as is the case for the 4 March 1881 (I<sub>max</sub>8-9 MCS) and the 28 July 1883 (I<sub>max</sub>10-11 MCS) events. Both the earthquakes struck the northern area of the island, similarly to the recent 21 August 2017 earthquake. The results allowed us to assess the location, as well as the possible dimension and the related maximum magnitude of the seismogenic structure, located in the northern sector of the island, and responsible of damaging earthquakes. Our results also provide an additional framework to interpret mechanisms leading to earthquakes associated with dynamics of calderas.</p><p> </p>


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