scholarly journals Significance of the Himaraya-Tibet Massif for the Global Changes. Climatic Changes Recorded in the Deep Sea Sediments(ODP site 974B) of the Mediterranean Sea During the Last 4.5Ma.

1997 ◽  
Vol 106 (2) ◽  
pp. 218-225
Author(s):  
Kazuyoshi YAMADA ◽  
Hitoshi FUKUSAWA
2010 ◽  
Vol 72 (2) ◽  
pp. 208-218 ◽  
Author(s):  
Cinzia Corinaldesi ◽  
Antonio Dell'Anno ◽  
Mirko Magagnini ◽  
Roberto Danovaro

1996 ◽  
Vol 12 (4) ◽  
pp. 247-251
Author(s):  
R. Delfanti ◽  
C. Papucci ◽  
C. Testa ◽  
D. Desideri ◽  
M. A. Meli ◽  
...  

2019 ◽  
Vol 9 (1) ◽  
Author(s):  
Nives Ogrinc ◽  
Holger Hintelmann ◽  
Jože Kotnik ◽  
Milena Horvat ◽  
Nicola Pirrone

Ocean Science ◽  
2013 ◽  
Vol 9 (2) ◽  
pp. 301-324 ◽  
Author(s):  
K. Schroeder ◽  
C. Millot ◽  
L. Bengara ◽  
S. Ben Ismail ◽  
M. Bensi ◽  
...  

Abstract. The long-term monitoring of basic hydrological parameters (temperature and salinity), collected as time series with adequate temporal resolution (i.e. with a sampling interval allowing the resolution of all important timescales) in key places of the Mediterranean Sea (straits and channels, zones of dense water formation, deep parts of the basins), constitute a priority in the context of global changes. This led CIESM (The Mediterranean Science Commission) to support, since 2002, the HYDROCHANGES programme (http//www.ciesm.org/marine/programs/hydrochanges.htm), a network of autonomous conductivity, temperature, and depth (CTD) sensors, deployed on mainly short and easily manageable subsurface moorings, within the core of a certain water mass. The HYDROCHANGES strategy is twofold and develops on different scales. To get information about long-term changes of hydrological characteristics, long time series are needed. But before these series are long enough they allow the detection of links between them at shorter timescales that may provide extremely valuable information about the functioning of the Mediterranean Sea. The aim of this paper is to present the history of the programme and the current set-up of the network (monitored sites, involved groups) as well as to provide for the first time an overview of all the time series collected under the HYDROCHANGES umbrella, discussing the results obtained thanks to the programme.


2018 ◽  
Vol 168 ◽  
pp. 57-64 ◽  
Author(s):  
Giulio Barone ◽  
Eugenio Rastelli ◽  
Cinzia Corinaldesi ◽  
Michael Tangherlini ◽  
Roberto Danovaro ◽  
...  

2003 ◽  
Vol 37 ◽  
pp. 93-108 ◽  
Author(s):  
Milena Horvat ◽  
Jože Kotnik ◽  
Martina Logar ◽  
Vesna Fajon ◽  
Tomislav Zvonarić ◽  
...  

ZooKeys ◽  
2018 ◽  
Vol 771 ◽  
pp. 15-40 ◽  
Author(s):  
Hiroshi Yamasaki ◽  
Katarzyna Grzelak ◽  
Martin V. Sørensen ◽  
Birger Neuhaus ◽  
Kai Horst George

Kinorhynchs rarely show a wide distribution pattern, due to their putatively low dispersal capabilities and/or limited sampling efforts. In this study, a new kinorhynch species is described,Echinoderespterussp. n., which shows a geographically and bathymetrically wide distribution, occurring on the Karasik Seamount and off the Svalbard Islands (Arctic Ocean), on the Sedlo Seamount (northeast Atlantic Ocean), and on the deep-sea floor off Crete and on the Anaximenes Seamount (Mediterranean Sea), at a depth range of 675–4,403 m. The new species is characterized by a combination of middorsal acicular spines on segments 4–8, laterodorsal tubes on segment 10, lateroventral tubes on segment 5, lateroventral acicular spines on segments 6–9, tufts of long hairs rising from slits in a laterodorsal position on segment 9, truncated tergal extensions on segment 11, and the absence of any type-2 gland cell outlet. The specimens belonging to the populations from the Arctic Ocean, the Sedlo Seamount, and the Mediterranean Sea show morphological variation in the thickness and length of the spines as well as in the presence/absence of ventromedial sensory spots on segment 7. The different populations are regarded as belonging to a single species because of their overlapping variable characters.


2006 ◽  
Vol 53 (12) ◽  
pp. 1895-1906 ◽  
Author(s):  
Guiomar Rotllant ◽  
Esteban Abad ◽  
Francisco Sardà ◽  
Manuela Ábalos ◽  
Joan B. Company ◽  
...  

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