A desregulação da homeostase do ferro: base molecular e patologias associadas

A homeostase do ferro requer um rigoroso processo de regulação, uma vez que este é um elemento essencial para alguns dos mecanismos celulares básicos mas, quando se encontra em excesso, origina profundos danos celulares e falha de órgãos. Dado que o organismo humano não possui um mecanismo ativo de excreção de ferro, é essencial que a sua homeostase seja estabelecida através de uma estreita comunicação entre os locais de absorção, utilização e armazenamento. Esta interligação é conseguida, essencialmente, através da ação de uma hormona circulante, a hepcidina. A hepcidina é sintetizada ao nível dos hepatócitos do fígado, sendo a sua expressão aumentada pelos níveis de ferro e inflamação e suprimida pela eritropoiese e hipoxia. A hepcidina regula negativamente a absorção duodenal do ferro proveniente da alimentação, a libertação pelos macrófagos do ferro resultante da fagocitose dos glóbulos vermelhos senescentes, assim como a libertação do ferro armazenado nos hepatócitos. A hemocromatose hereditátria (HH) do tipo 1 é uma doença de transmissão autossómica recessiva associada a mutações no gene HFE (p.Cys282Tyr e p.His63Asp). É a patologia humana mais comum de sobrecarga primária em ferro, apresenta penetrância incompleta, e é um dos distúrbios genéticos mais frequentes em caucasianos de ascendência Norte-Europeia. Na hemocromatose, apesar de haver um excesso de ferro no organismo, este facto não é refletido no nível de expressão da hormona hepcidina (cujos níveis deveriam aumentar). Pelo contrário, o nível de expressão da hepcidina encontra-se diminuído o que perpetua a constante absorção do ferro a nível duodenal. Os sintomas associados à doença iniciam-se geralmente na meia-idade e começam por consistir em sintomas gerais de fadiga e dores articulares. No entanto, a progressiva acumulação do ferro em vários órgãos (tais como fígado, coração e pâncreas) provoca aí graves danos, tais como cirrose, carcinoma hepatocelular, cardiomiopatias e diabetes. Para além da HH do tipo 1, podem ocorrer outros tipos de hemocromatose por mutações noutros genes relacionados com o metabolismo do ferro (tais como TFR2, HJV, HAMP, SLC40A1, etc). Mutações em genes como HAMP e HJV associam-se a hemocromatoses mais graves, de início ainda na juventude (hemocromatose juvenil). A implementação no nosso laboratório da nova metodologia de Next-Generation Sequencing permitiu-nos realizar a pesquisa de variantes simultaneamente em 6 genes relacionados com o metabolismo do ferro, em 88 doentes com fenótipo de hemocromatose hereditária não-clássica. Foram identificadas 54 variantes diferentes sendo algumas delas novas. Estudos in silico e estudos funcionais in vitro (em linhas celulares) permitiram-nos comprovar a patogenicidade de algumas das variantes novas e compreender os mecanismos moleculares subjacentes ao desenvolvimento da sobrecarga em ferro. Pelo contrário, no lado oposto do espetro das patologias relacionadas com o ferro, encontram-se as anemias por falta de ferro (anemias ferropénicas). A Organização Mundial de Saúde define anemia quando os níveis de hemoglobina no sangue são menores do que 12 g/dL na Mulher e 13 g/dL no Homem. A hemoglobina é a proteína existente nos glóbulos vermelhos do sangue, responsável pelo transporte de oxigénio no organismo, e cuja molécula é um tetrâmero formado por 4 cadeias polipeptídicas (as globinas) e 4 grupos heme que contêm 4 átomos de ferro. A falta de ferro impede que se formem as moléculas de hemoglobina a níveis normais em cerca de 20% da população portuguesa e isso é devido a carências alimentares ou a dificuldades na absorção do ferro proveniente da alimentação. Entre os fatores genéticos moduladores desta última situação parecem estar algumas variantes polimórficas no gene TMPRSS6, codificante da proteína Matriptase-2, um dos agentes envolvidos na regulação da expressão da hepcidina. Por outro lado, mutações neste gene dão origem a anemias ferropénicas graves, refratárias ao tratamento oral com ferro (Iron Refractory Iron Deficiency Anaemia - IRIDA). As Hemoglobinopatias são outro tipo de anemia hereditária. Estas não estão relacionadas com o défice de ferro mas sim com defeitos nas cadeias globínicas, constituintes da hemoglobina (α2β2). As hemoglobinopatias que estão relacionadas com um problema quantitativo, ou seja quando há ausência ou diminuição de síntese de uma cadeia globínica, denominam-se talassémias: beta-talassémia, alfa-talassémia, delta-talassémia, etc, consoante o gene afetado. Por outro lado, quando o problema é de carácter qualitativo, ou seja ocorre a síntese de uma cadeia globínica estruturalmente anómala, esta é denominada uma variante de hemoglobina. Enquadra-se neste último grupo a Anemia das Células Falciformes ou Drepanocitose. As hemoglobinopatias são das patologias genéticas mais frequentes no mundo, sendo que nalguns locais são um grave problema de saúde pública. Em Portugal foram realizados estudos epidemiológicos que permitiram determinar a frequência de portadores na população e foi implementado um programa de prevenção.

Looks Like FH But it’s not FH: Extended Lipid Profile of Paediatric Clinical FH Patients Reveals a Different Lipid Profile in FH Negative Patients

Aim: Familial Hypercholesterolemia (FH) is a common autosomal dominant disorder, caused by mutations in genes involved in cholesterol’s clearance (LDLR, APOB, PCSK 9). Clinical diagnosis is usually based on high total cholesterol or LDL-C levels and family history of premature coronary heart disease. Using an extended lipid profile of paediatric dyslipidemic patients, we aim to identify biomarkers for a better diagnosis of FH in clinical settings.

Using percentiles to diagnose familial hypercholesterolemia in Portugal

Aims: Familial hypercholesterolemia (FH) is a genetic disorder of lipid metabolism, clinically characterised by high levels of low-density lipoprotein cholesterol (LDL-C) that leads to cholesterol accumulation in tendons and arteries, premature atherosclerosis and increased risk of premature coronary heart disease. In 1999, the Portuguese FH Study was established at the National Institute of Health to identify the genetic cause of hypercholesterolemia in individuals with a clinical diagnosis of FH and to perform an epidemiologic study to determine the prevalence and distribution of FH in Portugal. In the last 16 years, a genetic defect was identified in 749 patients, representing 3. 7 % of the cases estimated to exist in Portugal. Index patients were included in this study using the Simon Broome (SB) criteria. However, there are different FH clinical criteria to diagnose index cases. Since there are no clinical criteria to identify relatives with FH, the aim of this work was to investigate if a diagnostic tool based on population specific 95 th percentile improves the clinical identification of Portuguese FH patients comparing with SB criteria.

Hemorheological alterations in sickle cell anemia and their clinical consequences: the role of genetic modulators

Sickle cell anemia (SCA) is an autosomal recessive chronic hemolytic anemia, caused by homozygosity for the HBB:c.20A>T mutation. The disease presents with high clinical heterogeneity, stroke being the most devastating manifestation. This study aimed to identify genetic modulators of severe hemolysis and stroke risk in children with SCA, as well as understand their consequences at the hemorheological level. Sixty-six children with SCA were categorised according to their degree of cerebral vasculopathy (Stroke/Risk/Control). Relevant data were collected from patients’ medical records. Several polymorphic regions in genes related to vascular cell adhesion and tonus were characterized by molecular methodologies. Data analyses were performed using R software. Several in silico tools (e.g. TFBind, MatInspector) were applied to investigate the main variant consequences. Some genetic variants in vascular adhesion molecule-1 gene promoter and endothelial nitric oxide synthase gene were associated with higher levels of hemolysis and stroke events. They modify important transcription factor binding sites or disturb the corresponding protein structure/function. Our findings emphasize the relevance of the genetic variants in modulating the degree of hemolysis and development of cerebral vasculopathy due to their effect on gene expression, modification of protein biological activities related with erythrocyte/endothelial interactions and consequent hemorheological abnormalities in SCA.

Plasticité du cortex visuel: «homéodynamie» des connexions neuronales et modèle d’effets d’antidépresseurs

Les informations sensorielles sont traitées dans le cortex par des réseaux de neurones co-activés qui forment des assemblées neuronales fonctionnelles. Le traitement visuel dans le cortex est régit par différents aspects des caractéristiques neuronales tels que l’aspect anatomique, électrophysiologique et moléculaire. Au sein du cortex visuel primaire, les neurones sont sélectifs à divers attributs des stimuli tels que l’orientation, la direction, le mouvement et la fréquence spatiale. Chacun de ces attributs conduit à une activité de décharge maximale pour une population neuronale spécifique. Les neurones du cortex visuel ont cependant la capacité de changer leur sélectivité en réponse à une exposition prolongée d’un stimulus approprié appelée apprentissage visuel ou adaptation visuelle à un stimulus non préférentiel. De ce fait, l’objectif principal de cette thèse est d’investiguer les mécanismes neuronaux qui régissent le traitement visuel durant une plasticité induite par adaptation chez des animaux adultes. Ces mécanismes sont traités sous différents aspects : la connectivité neuronale, la sélectivité neuronale, les propriétés électrophysiologiques des neurones et les effets des drogues (sérotonine et fluoxétine). Le modèle testé se base sur les colonnes d’orientation du cortex visuel primaire. La présente thèse est subdivisée en quatre principaux chapitres. Le premier chapitre (A) traite de la réorganisation du cortex visuel primaire suite à une plasticité induite par adaptation visuelle. Le second chapitre (B) examine la connectivité neuronale fonctionnelle en se basant sur des corrélations croisées entre paires neuronales ainsi que sur des corrélations d’activités de populations neuronales. Le troisième chapitre (C) met en liaison les aspects cités précédemment (les effets de l’adaptation visuelle et la connectivité fonctionnelle) aux propriétés électrophysiologiques des neurones (deux classes de neurones sont traitées : les neurones à décharge régulière et les neurones à décharge rapide ou burst). Enfin, le dernier chapitre (D) a pour objectif l’étude de l’effet du couplage de l’adaptation visuelle à l’administration de certaines drogues, notamment la sérotonine et la fluoxétine (inhibiteur sélectif de recapture de la sérotonine). Méthodes En utilisant des enregistrements extracellulaires d’activités neuronales dans le cortex visuel primaire (V1) combinés à un processus d’imagerie cérébrale optique intrinsèque, nous enregistrons l’activité de décharge de populations neuronales et nous examinons l’activité de neurones individuels extraite des signaux multi-unitaires. L’analyse de l’activité cérébrale se base sur différents algorithmes : la distinction des propriétés électrophysiologiques des neurones se fait par calcul de l’intervalle de temps entre la vallée et le pic maximal du potentiel d’action (largeur du potentiel d’action), la sélectivité des neurones est basée sur leur taux de décharge à différents stimuli, et la connectivité fonctionnelle utilise des calculs de corrélations croisées. L’utilisation des drogues se fait par administration locale sur la surface du cortex (après une craniotomie et une durotomie). Résultats et conclusions Dans le premier chapitre, nous démontrons la capacité des neurones à modifier leur sélectivité après une période d’adaptation visuelle à un stimulus particulier, ces changements aboutissent à une réorganisation des cartes corticales suivant un patron spécifique. Nous attribuons ce résultat à la flexibilité de groupes fonctionnels de neurones qui étaient longtemps considérés comme des unités anatomiques rigides. En effet, nous observons une restructuration extensive des domaines d’orientation dans le but de remodeler les colonnes d’orientation où chaque stimulus est représenté de façon égale. Ceci est d’autant plus confirmé dans le second chapitre où dans ce cas, les cartes de connectivité fonctionnelle sont investiguées. En accord avec les résultats énumérés précédemment, les cartes de connectivité montrent également une restructuration massive mais de façon intéressante, les neurones utilisent une stratégie de sommation afin de stabiliser leurs poids de connectivité totaux. Ces dynamiques de connectivité sont examinées dans le troisième chapitre en relation avec les propriétés électrophysiologiques des neurones. En effet, deux modes de décharge neuronale permettent la distinction entre deux classes neuronales. Leurs dynamiques de corrélations distinctes suggèrent que ces deux classes jouent des rôles clés différents dans l’encodage et l’intégration des stimuli visuels au sein d’une population neuronale. Enfin, dans le dernier chapitre, l’adaptation visuelle est combinée avec l’administration de certaines substances, notamment la sérotonine (neurotransmetteur) et la fluoxétine (inhibiteur sélectif de recapture de la sérotonine). Ces deux substances produisent un effet similaire en facilitant l’acquisition des stimuli imposés par adaptation. Lorsqu’un stimulus non optimal est présenté en présence de l’une des deux substances, nous observons une augmentation du taux de décharge des neurones en présentant ce stimulus. Nous présentons un modèle neuronal basé sur cette recherche afin d’expliquer les fluctuations du taux de décharge neuronale en présence ou en absence des drogues. Cette thèse présente de nouvelles perspectives quant à la compréhension de l’adaptation des neurones du cortex visuel primaire adulte dans le but de changer leur sélectivité dans un environnement d’apprentissage. Nous montrons qu’il y a un parfait équilibre entre leurs habiletés plastiques et leur dynamique d’homéostasie.

La communication hors du commun : aporétique de la communauté inachevée

En prenant pour appui initial le caractère équivoque de la communication, cette dissertation interroge les manières par lesquelles la vie en commun prend aussi effet comme œuvre de mort. S’inspirant du renouvellement de la recherche sur le thème de la communauté, l’interrogation se déploie en trois mouvements principaux. Chacun de ces mouvements ouvre et négocie trois grandes impasses : épistémologique, politique et éthique. La recherche propose de s’y frayer un chemin en s’appuyant principalement sur les travaux de Jean-Luc Nancy, Giorgio Agamben et Roberto Esposito. Le premier mouvement ouvre au voilement de l’idée de communication. L’idée de communication est voilée par une idéologie qui hérite elle-même d’une certaine conception humaniste de la communauté. Un examen de l’essai de Pic de la Mirandole Sur la dignité de l’homme permet d’exposer les valeurs associées à cette tradition qui recouvrent le caractère ambivalent de la communication. Ce premier mouvement mène au seuil de la situation politique contemporaine, marquée notamment par la nécessité de penser « notre » condition après la crise des valeurs humanistes. Le deuxième mouvement s’applique à l’examen de trois événements politiques contemporains. Chacun donne à comprendre comment s’exprime le péril associé à ce voilement : la fusillade au Collège Dawson de Montréal en 2006, un incident impliquant l’usage de gaz lacrymogènes lors de manifestations menées en 2013 à la Place Taksim à Istanbul, en Turquie, et une analyse de la crise de la dette publique grecque. L’aporie qui articule communication et incommunicabilité y est examinée à partir des thèmes de l’incommensurabilité des modes de vie en commun, de la biopolitique et du fascisme. Le fait que le péril qui menace de « nous » partager soit encore, malgré tout, ce que « nous » avons en partage invite à avancer là où aucune voie ne semble s’ouvrir. Le troisième mouvement présente les manières par lesquelles l’aporie de la communication peut être saisie en montrant qu’il est possible de penser par delà l’opposition de la communication et de la non-communication. Ce problème est abordé à l’horizon de la tradition philosophique concernant la question de l’être. Le saisissement du commun comme d’un propre — l’appropriation de l’inappropriable — ouvre à une conception de la communication « hors du commun ». Ces trois mouvements ne portent pas jusqu’à une conclusion. Ils ouvrent plutôt sur une autre conception de la communication. Celle-ci expose la possibilité sans cesse reconduite de l’événement fragile et intime dont « nous » sommes le nom.

(Table 1) Elements at DSDP Section 93-605-66-1

The oldest sediments cored at Site 605 are upper Maestrichtian argillaceous limestone (Hole 605, Subunit VB). The terrigeneous silt content of the uppermost Maestrichtian is quite low, averaging about 3%, whereas the carbonate content is high, usually greater than 60%; the silt contains only traces of glauconite (Site 605 chapter, this volume). Within Subunit VB a K/T boundary was defined by planktonic foraminifers. It was expected to be spread over an extended vertical interval because of the continental margin depositional setting. Examination by the shipboard party showed that the K/T boundary occurs in Section 605-66-1, between 70 and 75 cm. At the contact, the foraminiferal Globigerina pseudobulloides Zone (PIc) and the Coccolith Cruciplacolithus primus Subzone (CPla) overlie, respectively, the Abathomphalus mayaroensis and Nephrolithus frequens zones (Site 605). However, the thin K/T boundary clay, which is always present in complete sections, was not found, indicating either that the K/T boundary clay was not present or, more likely, that it was washed away during the coring operation.

Expression of biomineralization-related ion transport genes in Emiliania huxleyi

Biomineralization in the marine phytoplankton Emiliania huxleyi is a stringently controlled intracellular process. The molecular basis of coccolith production is still relatively unknown although its importance in global biogeochemical cycles and varying sensitivity to increased pCO2 levels has been well documented. This study looks into the role of several candidate Ca2+, H+ and inorganic carbon transport genes in E. huxleyi, using quantitative reverse transcriptase PCR. Differential gene expression analysis was investigated in two isogenic pairs of calcifying and non-calcifying strains of E. huxleyi and cultures grown at various Ca2+ concentrations to alter calcite production. We show that calcification correlated to the consistent upregulation of a putative HCO3- transporter belonging to the solute carrier 4 (SLC4) family, a Ca2+/H+ exchanger belonging to the CAX family of exchangers and a vacuolar H+-ATPase. We also show that the coccolith-associated protein, GPA is downregulated in calcifying cells. The data provide strong evidence that these genes play key roles in E. huxleyi biomineralization. Based on the gene expression data and the current literature a working model for biomineralization-related ion transport in coccolithophores is presented.

Rock magnetic records and geochemical methods of sediment cores off NW Africa

Two gravity cores retrieved off NW Africa at the border of arid and subtropical environments (GeoB 13602-1 and GeoB 13601-4) were analyzed to extract records of Late Quaternary climate change and sediment export. We apply End Member (EM) unmixing to 350 acquisition curves of isothermal remanent magnetization (IRM). Our approach enables to discriminate rock magnetic signatures of aeolian and fluvial material, to determine biomineralization and reductive diagenesis. Based on the occurrence of pedogenically formed magnetic minerals in the fluvial and aeolian EMs, we can infer that goethite formed in favor to hematite in more humid climate zones. The diagenetic EM dominates in the lower parts of the cores and within a thin near-surface layer probably representing the modern Fe**2+/Fe**3+ redox boundary. Up to 60% of the IRM signal is allocated to a biogenic EM underlining the importance of bacterial magnetite even in siliciclastic sediments. Magnetosomes are found well preserved over most of the record, indicating suboxic conditions. Temporal variations of the aeolian and fluvial EMs appear to faithfully reproduce and support trends of dry and humid conditions on the continent. The proportion of aeolian to fluvial material was dramatically higher during Heinrich Stadials, especially during Heinrich Stadial 1. Dust export from the Arabian-Asian corridor appears to vary contemporaneous to increased dust fluxes on the continental margin of NW Africa emphasizing that melt-water discharge in the North Atlantic had an enormous impact on atmospheric dynamics.

Pollen record and age determiation of sediments from the Labaz Lake area

Pollen records from perennially frozen sequences provide vegetation and climate reconstruction for the last 48,000 14C years in the central part of Taymyr Peninsula. Open larch forest with Alnus fruticosa and Betula nana grew during the Kargin (Middle Weichselian) Interstade, ca. 48,000-25,000 14C yr B.P. The climate was generally warmer and wetter than today. Open steppe-like communities with Artemisia, Poaceae, Asteraceae, and herb tundralike communities with dwarf Betula and Salix dominated during the Sartan (Late Weichselian) Stade, ca. 24,000-10,300 14C yr B.P. The statistical information method used for climate reconstruction shows that the coldest climate was ca. 20,000-17,000 14C yr B.P. A warming (Allerød Interstade?) with mean July temperature ca. 1.5°C warmer than today occurred ca. 12,000 14C yr B.P. The following cooling with temperatures about 3°-4°C cooler than present and precipitation about 100 mm lower corresponds well with the Younger Dryas Stade. Tundra-steppe vegetation changed to Betula nana-Alnus fruticosa shrub tundra ca. 10,000 14C yr B.P. Larch appeared in the area ca. 9400 14C yr B.P. and disappeared after 2900 14C yr B.P. Cooling events ca. 10,500, 9600, and 8200 14C yr B.P. characterized the first half of the Holocene. A significant warming occurred ca. 8500 14C yr B.P., but the Holocene temperature maximum was at about 6000-4500 14C yr B.P. The vegetation cover approximated modern conditions ca. 2800 14C yr B.P. Late Holocene warming events occurred at ca. 3500, 2000, and 1000 14C yr B.P. A cooling (Little Ice Age?) took place between 500 and 200 14C yr ago.

The late Pliocene pollen record of ODP Site 108-658 off Cape Blanc, Atlantic Ocean

A 200 m long marine pollen record from ODP Site 658 (21°N, 19°W) reveals cyclic fluctuations in vegetation and continental climate in northwestern Africa from 3.7 to 1.7 Ma. These cycles parallel oxygen isotope stages. Prior to 3.5 Ma, the distribution of tropical forests and mangrove swamps reached Cape Blanc, 5°N of the present distribution. Between 3.5 and 2.6 Ma, forests occurred at this latitude during irregular intervals and nearly disappeared afterwards. Likewise, a Saharan paleoriver flowed continuously until isotope Stage 134 (3.35 Ma). When river discharge ceased, wind transport of pollen grains prevailed over fluvial transport. Pollen indicators of trade winds gradually increased between 3.3 and 2.5 Ma. A strong aridification of the climate of northwestern Africa occurred during isotope Stage 130 (3.26 Ma). Afterwards, humid conditions reestablised followed by another aridification around 2.7 Ma. Repetitive latitudinal shifts of vegetation zones ranging from wooded savanna to desert flora dominated for the first time between between 2.6 and 2.4 Ma as a response to the glacial stages 104, 100 and 98. Although climatic conditions, recorded in the Pliocene, were not as dry as those of the middle and Late Pleistocene, latitudinal vegetation shifts near the end of the Pliocene resembled those of the interglacial-glacial cycles of the Brunhes chron.

Pollen content and radiocarbon ages of profile Delorett, Austria

A pollen profile from the highest known peatbog in the Alps is presented. The peatbog started to grow about 8000 years ago and over the last 5000 years. The influence of man on the vegetation is documented. Before the beginning of the bronze age pasturing started.

Results of a sediment profile and water analyses from Lake Hancza in northeastern Poland

We investigated the sedimentary record of Lake Hancza (northeastern Poland) using a multi-proxy approach, focusing on early to mid-Holocene climatic and environmental changes. AMS 14C dating of terrestrial macrofossils and sedimentation rate estimates from occasional varve thickness measurements were used to establish a chronology. The onset of the Holocene at c. 11600 cal. a BP is marked by the decline of Lateglacial shrub vegetation and a shift from clastic-detrital deposition to an autochthonous sedimentation dominated by biochemical calcite precipitation. Between 10000 and 9000 cal. a BP, a further environmental and climatic improvement is indicated by the spread of deciduous forests, an increase in lake organic matter and a 1.7% rise in the oxygen isotope ratios of both endogenic calcite and ostracod valves. Rising d18O values were probably caused by a combination of hydrological and climatic factors. The persistence of relatively cold and dry climate conditions in northeastern Poland during the first one and a half millennia of the Holocene could be related to a regional eastern European atmospheric circulation pattern. Prevailing anticyclonic circulation linked to a high-pressure cell above the retreating Scandinavian Ice Sheet might have blocked the influence of warm and moist Westerlies and attenuated the early Holocene climatic amelioration in the Lake Hancza region until the final decay of the ice sheet.

Pollen record and age determinations of a profile at Cape Mamontov Klyk, Siberia

Non-glaciated Arctic lowlands in north-east Siberia were subjected to extensive landscape and environmental changes during the Late Quaternary. Coastal cliffs along the Arctic shelf seas expose terrestrial archives containing numerous palaeoenvironmental indicators (e.g., pollen, plant macro-fossils and mammal fossils) preserved in the permafrost. The presented sedimentological (grain size, magnetic susceptibility and biogeochemical parameters), cryolithological, geochronological (radiocarbon, accelerator mass spectrometry and infrared-stimulated luminescence), heavy mineral and palaeoecological records from Cape Mamontov Klyk record the environmental dynamics of an Arctic shelf lowland east of the Taymyr Peninsula, and thus, near the eastern edge of the Eurasian ice sheet, over the last 60 Ky. This region is also considered to be the westernmost part of Beringia, the non-glaciated landmass that lay between the Eurasian and the Laurentian ice caps during the Late Pleistocene. Several units and subunits of sand deposits, peat-sand alternations, ice-rich palaeocryosol sequences (Ice Complex) and peaty fillings of thermokarst depressions and valleys were presented. The recorded proxy data sets reflect cold stadial climate conditions between 60 and 50 Kya, moderate inderstadial conditions between 50 and 25 Kya and cold stadial conditions from 25 to 15 Kya. The Late Pleistocene to Holocene transition, including the Allerød warm period, the early to middle Holocene thermal optimum and the late Holocene cooling, are also recorded. Three phases of landscape dynamic (fluvial/alluvial, irregular slope run-off and thermokarst) were presented in a schematic model, and were subsequently correlated with the supraregional environmental history between the Early Weichselian and the Holocene.

Pollen profile from Schonen, Sweden

Two new Standard pollen diagrams from the raised bog Ageröds mosse in central Scania are presented and discussed. They have been made giving extensive consideration to the NAP and spores also. The new diagrams comprise in the main only the Post-glacial and can easily be compared with the earlier published Standard diagram from the bog (T. NILSSON 1935). The development of the Post-glacial Vegetation in the surroundings is also discussed and compared with the conditions in the southernmost part of the province (Bjärsjöholmssjön, T. Nilsson 1961). One of the new diagrams has been prepared in connection with the study of a core brought up by means of a special borer in order to bring about C14 datings. The core was almost ömlong and had a diameter of 6 cm. It was divided into pieces of 2-6 cm, which were preserved. After the preparation of the pollen diagram, suitable samples were selected for C14 dating. In all 33 samples, comprising the whole Post-glacial inclusive of the youngest part of the Late-glacial, were C14-dated. With the aid of the C14 dates the growth conditions of the bog are discussed. After very slow Sedimentation of predominantly minerogenous deposits in the last part of the Late-glacial, and still slow Sedimentation of gyttjas in the oldest part of the Post-glacial, the rate of growth (primarily of the gyttja) distinctly increased in the first part of the Late Boreal. A temporary retardation of the growth of the sphagnum peat at the end of the Sub-boreal is probably entirely local. The average rate of growth of the really highly humified parts of the old sphagnum peat amounts to 42 mm per Century, that of the slightly humified young sphagnum peat 81 mm per Century or somewhat more. Based on the C14-determinations, the pollen zone boundaries have been given the following approximate dates: boundary Late-glacial/Post-glacial (DR/PB) 8300 B.C., boundary Pre-boreal/Boreal (PB/BO) 7900 B.C., boundary Early Boreal/Late Boreal (BO 1/2) 6800 B.C., boundary Boreal/Atlantic (BO/AT) 6200 B.C., boundary Early Atlantic/Late Atlantic (AT 1/2) 4600 B.C. (?), boundary Atlantic/Sub-boreal (AT/SB) 3300 B.C., boundary Early Sub-boreal/Late Sub-boreal (SB 1/2) 1700-1800 B.C., boundary Sub-boreal/Sub-atlantic (SB/ SA) 300 B.C., boundary Early Sub-atlantic/Late Sub-atlantic (SA 1/2) 650 A.D.