Core alignment and composite depth scale of DSDP Site 86-577

Deep Sea Drilling Project Site 577 on Shatsky Rise (North Pacific Ocean) recovered a series of cores at three holes that contain calcareous nannofossil ooze of latest Cretaceous (late Maastrichtian) through early Eocene age. Several important records have been generated using samples from these cores, but the stratigraphy has remained outdated and confusing. Here we revise the stratigraphy at Site 577. This includes refining several age datums, realigning cores in the depth domain, and placing all stratigraphic markers on a current time scale. The work provides a template for appropriately bringing latest Cretaceous and Paleogene data sets at old drill sites into current paleoceanographic literature for this time interval. While the Paleocene Eocene Thermal Maximum (PETM) lies within core gaps at Holes 577* and 577A, the sedimentary record at the site holds other important events and remains crucially relevant to understanding changes in oceanographic conditions from the latest Cretaceous through early Paleogene.

Biosiliceous sedimentation at ODP Site 128-798

Upper Pliocene through Holocene sediments recovered at Site 798 in the Japan Sea (Oki Ridge) exhibit rhythmic variation in weight percent biogenic opal at intervals of ~5 m and periods equivalent to the 41-k.y. obliquity cycle. Variance at 17 and 100 k.y. is observed prior to 1.3 Ma. These cycles are also clearly defined by log data and correspond to clusters of decimeter-scale dark-colored sediment units alternating with clusters of light-colored units. Opal content varies between 3% and 22% between 0 and 1.3 Ma and from 3% to 43% between 1.3 and 2.6 Ma. Long-term opal accumulation rates average 1.8 g/cm**2/k.y. in the late Pliocene/early Pleistocene and decrease by about 60% at ~1.3 Ma. Rough calculations suggest that opal accumulation rates increased and terrigenous flux decreased during the Holocene relative to the last glacial period. Our age control is not yet sufficient to allow a similar analysis of the 41-k.y. cyclicity in opal content throughout the Pleistocene. Stable isotope results from planktonic foraminifers confirm previous suggestions of a strong surface-water freshening event during isotope stage 2; however, this episode appears to be unique during the Pleistocene. Benthic foraminifers are depleted in 18O during parts of glacial stages 2 and 6 relative to adjacent interglacials, suggesting unusual warming and/or freshening of deep waters. Collectively, the stable isotope and %opal data are consistent with continuing isolation of the Japan Sea during the Quaternary with important transitions occurring at 1.3, 0.7 to 1.0, and 0.2 to 0.3 Ma. Complex relationships among the stable isotope results, %opal data, and sediment characteristics such as color and organic and inorganic carbon content preclude development of a simple model to explain cyclical sedimentation. Opal maxima occur within both light and dark intervals and the processes that control surface-water productivity are at times decoupled from the factors that regulate deep-water dysaerobia. We suggest that water column overturn is controlled largely by regional atmospheric circulation that must also have an as yet poorly understood effect on surface-water fertility.

Stable carbon and oxygen isotope compositions of Eocene benthic foraminifera from ODP Site 207-1258

'Hyperthermals' are intervals of rapid, pronounced global warming known from six episodes within the Palaeocene and Eocene epochs (~65-34 million years (Myr) ago) (Zachos et al., 2005, doi:10.1126/science.1109004; 2008, doi:10.1038/nature06588; Roehl et al., 2007, doi:10.1029/2007GC001784; Thomas et al., 2000; Cramer et al., 2003, doi:10.1029/2003PA000909; Lourens et al., 2005, doi:10.1038/nature03814; Petrizzo, 2005, doi:10.2973/odp.proc.sr.198.102.2005; Sexton et al., 2006, doi:10.1029/2005PA001253; Westerhold et al., 2007, doi:10.1029/2006PA001322; Edgar et al., 2007, doi:10.1038/nature06053; Nicolo et al., 2007, doi:10.1130/G23648A.1; Quillévéré et al., 2008, doi:10.1016/j.epsl.2007.10.040; Stap et al., 2010, doi:10.1130/G30777.1). The most extreme hyperthermal was the 170 thousand year (kyr) interval (Roehl et al., 2007) of 5-7 °C global warming (Zachos et al., 2008) during the Palaeocene-Eocene Thermal Maximum (PETM, 56 Myr ago). The PETM is widely attributed to massive release of greenhouse gases from buried sedimentary carbon reservoirs (Zachos et al., 2005; 2008; Lourenbs et al., 2005; Nicolo et al., 2007; Dickens et al., 1995, doi:10.1029/95PA02087; Dickens, 2000; 2003, doi:10.1016/S0012-821X(03)00325-X; Panchuk et al., 2008, doi:10.1130/G24474A.1) and other, comparatively modest, hyperthermals have also been linked to the release of sedimentary carbon (Zachos et al., 2008, Lourens et al., 2005; Nicolo et al., 2007; Dickens, 2003; Panchuk et al., 2003). Here we show, using new 2.4-Myr-long Eocene deep ocean records, that the comparatively modest hyperthermals are much more numerous than previously documented, paced by the eccentricity of Earth's orbit and have shorter durations (~40 kyr) and more rapid recovery phases than the PETM. These findings point to the operation of fundamentally different forcing and feedback mechanisms than for the PETM, involving redistribution of carbon among Earth's readily exchangeable surface reservoirs rather than carbon exhumation from, and subsequent burial back into, the sedimentary reservoir. Specifically, we interpret our records to indicate repeated, large-scale releases of dissolved organic carbon (at least 1,600 gigatonnes) from the ocean by ventilation (strengthened oxidation) of the ocean interior. The rapid recovery of the carbon cycle following each Eocene hyperthermal strongly suggests that carbon was resequestered by the ocean, rather than the much slower process of silicate rock weathering proposed for the PETM (Zachos et al., 2005; 2003). Our findings suggest that these pronounced climate warming events were driven not by repeated releases of carbon from buried sedimentary sources (Zachos et al., 2008, Lourens et al., 2005; Nicolo et al., 2007; Dickens, 2003; Panchuk et al., 2003) but, rather, by patterns of surficial carbon redistribution familiar from younger intervals of Earth history.

Results of the sensitivity experiments LOVECLIM as NetCDF files

Several abrupt climatic events during the present interglacial have been associated with catastrophic freshwater forcing, such as the events at 9.2and 8.2 ka BP (Alley et al., 1997; Barber et al., 1999; Marshall et al. 2007; Fleitmann et al. 2008). Proxy evidence suggests that similar events may have occurred during the last interglacial (e.g., Beets & Beets 2003; Beets et al., 2006), suggesting that freshwater-induced perturbations are an important mechanism for abrupt climate change in interglacial climates. In addition solar variability (Neff et al., 2001; Wang et al., 2005) and explosive volcanic eruptions (Crowley, 2000; Shindell et al., 2003; Jansen et al., 2007) can trigger centennial-scale climate events during interglacials and may thus have been responsible for a part of interglacial climate variability. We investigate the sensitivity of the present and last interglacial climates to realistic perturbations resulting from freshwater, solar or volcanic forcings. We will compare the differences between the two interglacial periods, between different climate models and evaluate the resulting using proxy archives.

Efficacia della formazione alla salute e sicurezza sul lavoro: fattori di successo e criticità

Background: sulla base delle evidenze emerse dalle rassegne sistematiche in materia (Johnstone, 1994; Cohen et al.,1998; Robson et al., 2012; Burke et al., 2006; Ricci et al., 2015) si è ipotizzato che la formazione alla salute e sicurezza sul lavoro sia maggiormente efficace quando non è presentata come obbligatoria e venga articolata su più livelli di apprendimento, attraverso metodologie adeguate per ogni livello, con docenti che abbiano caratteristiche corrispondenti allo specifico obiettivo di apprendimento e la cui durata sia parametrata all’obiettivo stesso. Obiettivo di questa ricerca è valutare se esista e quanto sia intensa la relazione causale tra la formazione alla sicurezza sul lavoro e i suoi effetti sul miglioramento delle conoscenze, degli atteggiamenti, dei comportamenti, degli esiti per la salute, del clima di sicurezza aziendale, del controllo comportamentale percepito dai lavoratori, delle condizioni operative e procedure interne, oltre l’eventuale effetto di moderazione determinato da caratteristiche socio-demografiche dei partecipanti e dal gradimento della formazione. Metodo: la variabile indipendente è costituita dell’intervento formativo erogato, articolato in tre condizioni: formazione obbligatoria, formazione non obbligatoria, gruppo di controllo: sono stati posti a confronto due interventi di pari durata (16 settimane, per 10h complessive), realizzati con identiche modalità (step1 audio-visivo; step2 affiancamento su lavoro da parte del preposto; step3 discussione di auto-casi), ma differenziati rispetto all’essere presentati uno come formazione obbligatoria, l’altro come non obbligatoria. I due gruppi sono anche stati confrontati con un gruppo di controllo per il quale la formazione è prevista successivamente. I partecipanti sono stati assegnati in modo casuale al gruppo con obbligo formativo, senza obbligo formativo, di controllo. Sono stati presi come indicatori (variabili dipendenti) per valutare l’effetto della formazione: I livello – conoscenze: riconoscimento o produzione di un maggior numero di risposte corrette. II livello – atteggiamenti e credenze: maggiore propensione a mettere in atto comportamenti auto ed etero protettivi. III livello – comportamenti: comportamenti osservati più adeguati per la tutela della salute propria e altrui. IV livello – salute: maggior grado di benessere bio-psico-sociale auto-riferito. Le misure di esito consistono nella variazione tra la rilevazione iniziale e ogni rilevazione successiva, sulla base delle diverse misure registrate per ognuno dei quattro livelli dell’intervento formativo. Lo stesso confronto del tempo è stato realizzato per le misure del clima di sicurezza aziendale, del controllo comportamentale percepito dai lavoratori, delle condizioni operative e procedure interne, oltre l’eventuale effetto di moderazione determinato da caratteristiche socio-demografiche dei partecipanti e dal gradimento della formazione, quest’ultimo misurato solo immediatamente al termine dell’intervento. Risultati: le condizioni di intervento non differiscono in termini di efficacia, la formazione determina infatti gli stessi risultati per i partecipanti del gruppo obbligo formativo e di quello non obbligo, con una significativa differenza post-intervento rispetto al gruppo di controllo. La formazione ha un effetto forte nel miglioramento delle conoscenze che solo parzialmente decade nel tempo, ma comunque mantenendo un livello maggiore rispetto ai valori iniziali. In relazione al miglioramento di atteggiamenti e comportamenti sicuri nel lavoro al Videoterminale, l’effetto della formazione è modesto: per gli atteggiamenti si registra solo un miglioramento verso l’applicazione delle procedure come utili realmente e non come mero adempimento, ma tale effetto decade entro quattro mesi riportando i partecipanti su valori iniziali; i comportamenti invece migliorano nel tempo, ma con deboli differenze tra partecipanti alla formazione e gruppo di controllo, tuttavia tale miglioramento non decade in seguito. Non si registrano invece effetti della formazione nella direzione attesa in termini di esiti per la salute, per il miglioramento del clima di sicurezza e come maggior controllo comportamentale percepito, non risultano nemmeno dati evidenti di moderazione degli effetti dovuti a caratteristiche socio-demografiche dei partecipanti. Inoltre emerge che il gradimento per la formazione è correlato con migliori atteggiamenti (strumento audio-visivo), il miglioramento del clima di sicurezza e un maggior controllo comportamentale percepito (studio di auto-casi), ovvero gli step che hanno visto l’intervento di formatori qualificati. Infine, la formazione ha determinato migliori condizioni operative e l’adeguamento delle procedure interne. Conclusioni: la presente ricerca ci consente di affermare che la formazione erogata è stata efficace, oltre che molto gradita dai partecipanti, in particolare quando il formatore è qualificato per questa attività (step1 e 3). L’apprendimento prodotto è tanto più stabile nel tempo quanto più i contenuti sono in stretta relazione con l’esperienza lavorativa quotidiana dei partecipanti, mentre negli altri casi il decremento degli effetti è alquanto rapido, di conseguenza ribadiamo la necessità di erogare la formazione con continuità nel tempo. E’ risultato comunque modesto l’effetto della formazione per migliorare gli atteggiamenti e i comportamenti nel lavoro al VDT, ma, al di là di alcuni limiti metodologici, sono obiettivi ambiziosi che richiedono più tempo di quanto abbiamo potuto disporre in questa occasione e il cui conseguimento risente molto delle prassi reali adottate nel contesto lavorativo dopo il termine della formazione. Le evidenze finora prodotte non hanno poi chiarito in modo definitivo se attraverso la formazione si possano determinare effetti significativi nel miglioramento di esiti per la salute, anche eventualmente attraverso interventi di supporto individuale. Inoltre l’assenza di differenze significative negli effetti tra i partecipanti assegnati alla condizione di obbligo e quelli di non obbligo, eccezion fatta in direzione opposta alle attese per la misura del danno da lavoro, suggeriscono che nell’erogare la formazione, occorre sottolineare in misura molto rilevante l’importanza dell’intervento che viene realizzato, anche qualora esistesse una prescrizione normativa cogente. Infine, la ricerca ci ha fornito anche indicazioni metodologiche e misure valide che invitano ad estendere questa formazione, e la sua valutazione di efficacia, a diversi comparti economici e svariate mansioni. Nel fare questo è possibile fare riferimento, e testare nuovamente, un modello che indica la corretta percezione del rischio (conoscenza) come fattore necessario, ma non sufficiente per ottenere, con la mediazione di atteggiamenti favorevoli allo specifico comportamento, azioni sicure, attraverso le quali si rinforza l’atteggiamento e migliorano le conoscenze. La formazione, per raggiungere i propri obiettivi, deve tuttavia agire anche sui meccanismi di conformismo sociale favorevoli alla safety, questi originano da conoscenze e azioni sicure e reciprocamente le rinforzano.

Profiling in sport using momentum and perturbations

Examining a team’s performance from a physical point of view their momentum might indicate unexpected turning points in defeat or success. Physicists describe this value as to require some effort to be started, but also that it is relatively easy to keep it going once a sufficient level is reached (Reed and Hughes, 2006). Unlike football, rugby, handball and many more sports, a regular volleyball match is not limited by time but by points that need to be gathered. Every minute more than one point is won by either one team or the other. That means a series of successive points enlarges the gap between the teams making it more and more difficult to catch up with the leading one. This concept of gathering momentum, or the reverse in a performance, can give the coaches, athletes and sports scientists further insights into winning and losing performances. Momentum investigations also contain dependencies between performances or questions if future performances are reliant upon past streaks. Squash and volleyball share the characteristic of being played up to a certain amount of points. Squash was examined according to the momentum of players by Hughes et al. (2006). The initial aim was to expand normative profiles of elite squash players using momentum graphs of winners and errors to explore ‘turning points’ in a performance. Dynamic systems theory has enabled the definition of perturbations in sports exhibiting rhythms (Hughes et al., 2000; McGarry et al., 2002; Murray et al., 2008), and how players and teams cause these disruptions of rhythm can inform on the way they play, these techniques also contribute to profiling methods. Together with the analysis of one’s own performance it is essential to have an understanding of your oppositions’ tactical strengths and weaknesses. By modelling the oppositions’ performance it is possible to predict certain outcomes and patterns, and therefore intervene or change tactics before the critical incident occurs. The modelling of competitive sport is an informative analytic technique as it directs the attention of the modeller to the critical aspects of data that delineate successful performance (McGarry & Franks, 1996). Using tactical performance profiles to pull out and visualise these critical aspects of performance, players can build justified and sophisticated tactical plans. The area is discussed and reviewed, critically appraising the research completed in this element of Performance Analysis.

The Case Law of the ECJ concerning the Free Provision of Services : 2000 - 2005. Research Papers in Law, 2/2006

Introduction. The present overview covers the period starting from 2000 until the end of 2005.1 This is the follow-up to our overview covering the 1995-1999 period.2 The first striking feature of the present contribution is that it has to deal with almost 3,5 times as many cases as the previous one. Hence, the ECJ has gone from deciding 40 cases in the five year period between 1995- 1999 to deciding over 140 cases based on Art 49 between 2000-2005. This confirms, beyond any doubt, the tendency already observed in our previous overview, that a “third generation” case law on services is being developed at a very rapid pace by the ECJ. This third generation case law is based on the idea that Article 49 EC is not limited to striking down discriminatory measures but extends to the elimination of all hindrances to the free provision of services. This idea was first expressed in the Tourist Guide cases, the Greek and Dutch TV cases and most importantly in the Säger case.3 It has been confirmed ever since. As was to be expected, this broad brush approach of the Court’s has led to an ever-increasing amount of litigation reaching Luxemburg. It is clear that, if indicators were used to weight the importance of the Court’s case law during the relevant period, services would score much higher than goods, both from a quantitative and from a qualitative perspective.4 Hence, contrary to the previous overview, this one cannot deal in detail with any of the judgments delivered during the reference period. The aim of the present contribution is restricted to presenting the basic trends of the Court’s case law in the field of services Therefore, the analysis follows a fundamentally horizontal approach, fleetingly considering the facts of individual cases, with a view to identifying the conceptual premises of the Court’s approach to the free movement of services. Nonetheless, the substantial solutions adopted by the Court in some key topics, such as concession contracts, healthcare services, posted workers and gambling, are also presented as case studies. In this regard, the analysis is organized in four sections. First we explore the (ever expanding) scope of the freedom to provide services (Section 2), then we go on to identify the nature of the violations and of justifications thereto (Section 3), before carrying out some case studies to concretely illustrate the above (Section 4). Then, for the sake of completeness, we try to deduce the general principles running through the totality of the relevant case law (Section 5). Inevitably, some concluding remarks follow (Section 6).5

Pollen abundances, and temperature and precipitation reconstruction for the Eocene to Oligocene transition in northern high latitudes

A profound global climate shift took place at the Eocene-Oligocene transition (~33.5 million years ago) when Cretaceous/early Palaeogene greenhouse conditions gave way to icehouse conditions (Zachos et al., 2001, doi:10.1126/science.1059412; Coxall et al., 2005, doi:10.1038/nature03135; Lear et al., 2008, doi:10.1130/G24584A.1). During this interval, changes in the Earth's orbit and a long-term drop in atmospheric carbon dioxide concentrations (Pagani et al., 2005, doi:10.1126/science.1110063; Pearson and Palmer, 2000, doi:10.1038/35021000; DeConto and Pollard, 2003, doi:10.1038/nature01290) resulted in both the growth of Antarctic ice sheets to approximately their modern size (Coxall et al., 2005, doi:10.1038/nature03135; Lear et al., 2008, doi:10.1130/G24584A.1) and the appearance of Northern Hemisphere glacial ice (Eldrett et al., 2007, doi:10.1038/nature05591; Moran et al., 2006, doi:10.1038/nature04800). However, palaeoclimatic studies of this interval are contradictory: although some analyses indicate no major climatic changes (Kohn et al., 2004, doi:10.1130/G20442.1; Grimes et al., 2005, doi:10.1130/G21019.1), others imply cooler temperatures (Zanazzi et al., 2007, doi:10.1038/nature05551), increased seasonality (Ivany et al., 2000, doi:10.1038/35038044; Terry, 2001, doi:10.1016/S0031-0182(00)00248-0) and/or aridity (Ivany et al., 2000, doi:10.1038/35038044; Terry, 2001, doi:10.1016/S0031-0182(00)00248-0; Sheldon et al., 2002, doi:10.1086/342865; Dupont-Nivet et al., 2007, doi:10.1038/nature05516). Climatic conditions in high northern latitudes over this interval are particularly poorly known. Here we present northern high-latitude terrestrial climate estimates for the Eocene to Oligocene interval, based on bioclimatic analysis of terrestrially derived spore and pollen assemblages preserved in marine sediments from the Norwegian-Greenland Sea. Our data indicate a cooling of ~5 °C in cold-month (winter) mean temperatures to 0-2 °C, and a concomitant increased seasonality before the Oi-1 glaciation event. These data indicate that a cooling component is indeed incorporated in the d18O isotope shift across the Eocene-Oligocene transition. However, the relatively warm summer temperatures at that time mean that continental ice on East Greenland was probably restricted to alpine outlet glaciers.

Late Pliocene variations of the Mediterranean outflow

Late Pliocene changes in the advection of Mediterranean Outflow Water (MOW) derivates were reconstructed at northeast Atlantic DSDP/ODP sites 548 and 982 and compared to records of WMDW at West Mediterranean Site 978. Neodymium isotope (epsilon-Nd) values more positive than ~10.5/~ 11 reflect diluted MOW derivates that spread almost continuously into the northeast Atlantic from 3.7 to 2.55 Ma, reaching Rockall Plateau Site 982 from 3.63 to 2.75 Ma. From 3.4 to 3.3 Ma average MOW temperature and salinity increased by 2°-4 °C and ~1 psu both at proximal Site 548 and distal Site 982. The rise implies a rise in flow strength, coeval with a long-term rise in both west Mediterranean Sea surface salinity by almost 2 psu and average bottom water salinity (BWS) by ~1 psu, despite inherent uncertainties in BWS estimates. The changes were linked with major Mediterranean aridification and a drop in African monsoon humidity. In contrast to model expectations, the rise in MOW salt discharge after 3.4 Ma did not translate into improved ventilation of North Atlantic Deep Water, since it possibly was too small to significantly influence Atlantic Meridional Overturning Circulation. Right after ~2.95 Ma, with the onset of major Northern Hemisphere Glaciation, long-term average bottom water temperature (BWT) and BWS at Site 548 dropped abruptly by ~5 °C and ~1-2 psu, in contrast to more distal Site 982, where BWT and BWS continued to oscillate at estimates of ~2 °C and 1.5-2.5 psu higher than today until ~2.6 Ma. We relate the small-scale changes both to a reduced MOW flow and to enhanced dilution by warm waters of a strengthened North Atlantic Current temporarily replacing MOW derivates at Rockall Plateau.

Radiocarbon dating and alkenone-based proxies of sediment core GeoB7702-3

In this study we utilize two organic geochemical proxies, the Uk'37 index and TEX86, to examine past sea surface temperatures (SST) from a site located near the Nile River Delta in the eastern Mediterranean (EM) Sea. The Uk'37 and TEX86 records generally are in agreement and indicate SST ranges of 14°C-26°C and 14°C-28°C, respectively, during the last 27 cal ka. During the Holocene, TEX86-based SST estimates are usually higher than Uk'37-based SST estimates, which is likely due to seasonal differences between the timing of the haptophyte and crenarchaeota blooms in the EM and is related to the onset of the modern flow regime of the Nile River. Both records show that SST varied on centennial to millennial timescales in response to global climate events, i.e., cooling during the Last Glacial Maximum (LGM), Heinrich event 1 (H1), and the Younger Dryas (YD) and warming during the Bølling-Allerød and in the early Holocene during deposition of sapropel S1. The H1 cooling was particularly severe and is marked by a drop in SST of ~4.5°C in comparison to pre-H1 SST, with temperatures >1°C cooler than during the LGM. In contrast to high-latitude and western Mediterranean records, which indicate both an abrupt onset and termination of the YD event, the transition from the YD to the Holocene was much more gradual in the EM.

Investigations on two sediment cores from the Arctic Ocean

During the "RV Polarstem"-Expedition ARK VIII/2 sediment samples were obtained at the continental slope of NW-Spitsbergen. Detailed sedimentological and geochemical analysis were carried out at two undisturbed box cores (PS2122-1GKG, PS2123-2GKG) as well as two gravity cores (PS2122-1SL, PS2123-2SL). The following parameters were deterrnined: Organic carbon, nitrogen and carbonate contents, hydrogen index, stable isotopes, ice rafted debris, grain-size distribution and biogenic opal. The main objective of this study was the reconstruction of paleoenvironmental changes off the northwest coast of Spitsbergen during the last glacial/interglacial-cycle, i.e., during the last about 128.000 years. The results of the investigations can be summarized as follows: - During isotope stage 1 (Holocene) and 5.5 (Eemian Interglacial), light stable isotopes (d180: 3.4-2 %o; d13C: 0.26-0.5 %o), increased bioturbation, high content of planktonic foraminifera and biogenic opal and low quantity of ice-rafted material, indicate seasonally ice-free conditions along the northwest coast due to the intfluence of the Westspitsbergen Current. - Additionally, the sediment characteristics of the middle of isotope stage 2 (Last Glacial Maximum) and at the end of stage 3 confirms an inflow of warmer Atlantic water. The highest production of planktonic and benthic foraminifera (N. pachyderma sin., Cassidulina teretis) (CaC03: 10 %) may reflect the expansion of the 'Whalers Bay'-Polynya as a result of the influence of the Westspitsbergen Current. Presumably, occasionally open-ice conditions provide sufficient precipitation to buildup the Svalbard/Barents Ice Sheet. - The time intervals for the glacier advances on Svalbard given by Mangerud et al. (1992), can be correlated with increased accumulation of ice-rafted material in the sediments at the northwest coast of Spitsbergen. Especially during isotope stage 4 and at the beginning of the Last Glacial Maximum (isotope stage 2), a drastically increased supply of coarse terrigenous material occurs. The high accumulation rate (0.18-0.21 g/cm**2/ka) of terrigenous organic carbon is indicated by high C/N ratios (until 16) and low hydrogen index (50 mg HC/gC). In constrast to deep sea sediments in the Fram-Strait (Hebbeln 1992), the glacier advance between 118.000 and 108.000 years B.P. ist documented in the continental slope sediments. - At the end of the Weichselian ice age, the deglaciation at the northwest coast starts with a typical melt-water signal in the stables isotope record (d18O: 3.5 %o; d13C: -0.16 %o) and high contents of gravel (6-13 %). The signal can be assigned to an event at the westcoast of Spitsbergen (core NP90-39), dated to 14.500 years B.P. (Andersen et al. 1993).

Institutional resistances before school mediation. An inquiry in the conflict settings

This paper deals with the conceptions of the different school actors about the meaning and the implications of mediation in their schools, drawing on data from a qualitative approach carried out as part of a wider project to map mediation perspectives and practices in Catalonia. The authors analyze the scope of the situations regarded as suitable or unsuitable for the introduction of restorative practices, as well as the resistance to change in the practice of conflict resolutions and in the democratization of school culture.