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BIV C16 Litteraturlista Litteraturlistan gäller ett (1) år efter avslutat kurstillfälle Humaniora och teo log i Centrum fö r teo log i och re l ig ionsvetenskap Litteraturlista för BIV C16 Bibelvetenskap: Nya testamentet på grundspråk – fördjupningskurs, 15 hp, VT 2026 fastställd av studierektor 2025-12-08 Litteratur Ekenberg, Anders (2006). Det förlorade originalet: Kompendium i textkritik (Canva

https://www.ctr.lu.se/media/utbildning/dokument/kurser/BIVC16/20261/BIV_C16_Litteraturlista.pdf - 2026-07-12

På denna sida kan du läsa om friskvårdsförmåner på Lunds universitet. Friskvårdsersättning 2026 Från och med den 1 januari 2026 är beloppet för friskvårdsersättning 3 000 kronor per år. Sista datum för att ansöka om friskvårdsersättning är den 30 november 2026.Även friskvårdsköp som du gjort i november och december 2025 kan ersättas av 2026 års friskvårdsersättning (upp till 3 000 kronor per år).

https://www.medarbetarwebben.lu.se/anstallning/arbetsmiljo-och-halsa/din-halsa/friskvardsersattning-och-friskvardstimme - 2026-07-11

HÖGSKOLEUTBILDNING I KYRKOMUSIK | 120 HP Hållpunkter för din ansökan Ansök till programmet på antagning.seAnsökningsperiod: 1 december 2025 – 15 januari 2026. Styrk din behörighet. Sista kompletteringsdag för att styrka din behörighet är 26 januari 2026. Kallelse till antagningsprov skickas i början av februari till den mejladress du angav vid ansökan. Skicka noter till pianoackompanjatör med vanl

https://www.mhm.lu.se/utbildning/antagning/antagning-musikerutbildningar/antagning-till-kyrkomusikerutbildning/antagning-till-kantorsutbildning - 2026-07-11

Ansökan och antagningNär kommer antagningsbeskedet?Det nationella antagningsbeskedet efter 1:a antagningsomgången blir tillgängligt för alla antagna studenter den 10 juli på Mina sidor på antagning.se. Du måste svara senast den 20 juli, klockan 23.59! Det gör du på Mina sidor på antagning.se. Svarar du inte förlorar du din plats.Nästa antagningsbesked kommer efter 2:a antagningsomgången och finns

https://www.ses.lu.se/fragor-och-svar-om-terminsstarten - 2026-07-11

https://www.mhm.lu.se/sites/mhm.lu.se/files/utbildningsplan_filmmusik_2019_is_3_april_beli_gallande.pdf - 2026-07-12

This study explores the relationship between land-use and floristic diversity between 600 BC and AD 2008 in the uplands of southern Sweden. We use fossil pollen assemblages and the Regional Estimates of Vegetation Abundance from Large Sites (REVEALS) model to quantitatively reconstruct land cover at a regional scale. Floristic richness and evenness are estimated using palynological richness and RE

The study explores divergent representations and cultural identity in a historically contested landscape. The first form of representations includes politically amended place marketing. It is analysed how public discourse on a city’s development and regeneration articulate inscriptions of local authorities to pursue political-economic agendas. The second form of representations is diaspora’s imagi

Efforts to extract a Greenland ice core with a complete record of the Eemian interglacial (130,000 to 115,000 years ago) have until now been unsuccessful. The response of the Greenland ice sheet to the warmer-than-present climate of the Eemian has thus remained unclear. Here we present the new North Greenland Eemian Ice Drilling ('NEEM') ice core and show only a modest ice-sheet response to the st

1. Temperate semi-natural grasslands are characterized by high levels of species diversity and have a high conservation value. Plant species diversity in grazed semi-natural grasslands is known to be influenced by management intensity and habitat connectivity. Both grazing pressure and between-patch connectivity are expected to depend on the movement patterns of livestock in the landscape. 2. The

Measurements of Last Interglacial stable water isotopes in ice cores show that central Greenland delta O-18 increased by at least 3 parts per thousand compared to present day. Attempting to quantify the Greenland interglacial temperature change from these ice core measurements rests on our ability to interpret the stable water isotope content of Greenland snow. Current orbitally driven interglacia

Irreversible shifts of large-scale components of the Earth system (so-called ‘tipping elements’) on policy-relevant timescales are a major source of uncertainty for projecting the impacts of future climate change. The high latitudes are particularly vulnerable to positive feedbacks that amplify change through atmosphere-ocean-ice interactions. Unfortunately, the short instrumental record does not

Odeum Mål och strategier 2013 - 2015 Bakgrund 2007 ircättades Odeum vid Lunds universitets och de forsta foreskrifterna for verksamheten fastställdes. 2008 antogs etc sryrdokument frr Odeum rörande mål och strategier for verksamheten 2008 - 2011. 2012'ån&ades Odeums föres}rifter i viss utsträckning till att vara mer anpassade till hur verksamheten utvecklats. I dessa nya foreskrifter beskrivs Odeu

https://www.odeum.lu.se/sites/odeum.lu.se/files/odeum_-_mal_och_strategier_2013-2016.pdf - 2026-07-12

Postal address Pufendorf Insititute, Lund University, Box 117, 221 20 Lund Visiting address Biskopsgatan 3, Lund Website www.pi.lu.se 1 Lund, 1 oktober 2016 Pufendorfinstitutet Inbjudan att inkomma med förslag till "teman" vid Pufendorfinstitutet 2017 Pufendorfinstitutet inbjuder nu till att ansöka om ”tema” med start hösten 2017. Institutets ambition är att, under förutsättning att medel för verk

https://www.pi.lu.se/sites/pi.lu.se/files/utlysning_teman_2017-18_sve.pdf - 2026-07-12

The agriculture sector can contribute to climate change mitigation by reducing its own greenhouse gas (GHG) emissions, sequestering carbon in vegetation and soils, and providing biomass to substitute for fossil fuels and other GHG-intensive products. The sector also needs to address water, soil, and biodiversity impacts caused by historic and current practices. Emerging EU policies create incentiv

Modes of climate variability affect global and regional climates on different spatio-temporal scales, and they have important impacts on human activities and ecosystems. As these modes are a useful tool for simplifying the understanding of the climate system, it is crucial that we gain improved knowledge of their long-term past evolution and interactions over time to contextualise their present an

Nitrogen dioxide (NO2) is an important air pollutant with both environmental and epidemiological effects. The main aim of this study is to analyze spatial patterns and temporal trends in tropospheric NO2 concentrations globally using data from the satellite-based Ozone Monitoring Instrument (OMI). Additional aims are to compare the satellite data with ground-based observations, and to find the tim

Human activities have a huge impact on the carbon cycle by modifying the landscape. Vegetation cover changes attributed to forest clearance and the expansion of agricultural land increases soil erosion, organic matter and other nutrient delivery from terrestrial to aquatic ecosystems. Long-term records of environmental variation at centennial to millennial time scales are essential for the assessm

The global climate transition from the Lateglacial to the Early Holocene is dominated by a rapid warming trend driven by an increase in orbital summer insolation over high northern latitudes and related feedbacks. The warming trend was interrupted by several abrupt shifts between colder (stadial) and warmer (interstadial) climate states following instabilities of the Atlantic Meridional Overturnin

Long-term changes in terrestrial organic matter input into lakes responding to land use changes.

Meteoric beryllium-10 (10Be) is commonly used as a proxy of landscape dynamics (erosion and sedimentation rates) and soil development. Soil represents the first-stage reservoir of meteoric 10Be, and variability in the concentration of the isotope in soils may be affected by soil properties and atmospheric deposition. Although many investigations have targeted this issue, there are still problems i