7500 yr of mire-pool development and the history of Pinus sylvestris (L.) in Sub-Arctic coastal Norway

In coastal North Norway, mire areas and mire pools frequently exist, but their development and time of origin are poorly known. In order to investigate the development of a coastal mire pool and relate its changes to known climatic changes, a sediment sequence from the mire-pool Lillevardhaugvatnet (c. 0.05 ha large), was ¹⁴C-dated, investigated for loss on ignition and analysed for pollen and botanical macrofossils.The bottom of the sequence dates c. 7500 cal. BP. The site gradually developed from a swamp forest c. 6200 cal. BP via a more open dwarf-shrub phase to a pool c. 5000 cal. BP. The pool grew in depth as the result of continuous peat growth damming the water body. The water level of the pool was probably lowered by erosional drain c. 2700 cal. BP. Redeposited peat in the sequence occurred c. 2100 cal. BP and c. 1100 cal. BP. ¹⁴C-dates and pollen indicate that erosion and redeposition of the peat surrounding the mire pool is a normal process, connected with the expansion of the water body.The combination of macrofossils and pollen accumulation rates (PAR) of P. sylvestris indicates that in small lakes in coastal areas of North Norway, a PAR of 200–400 cm^− 2 yr^− 1 is sufficient for indicating local presence of P. sylvestris. P. sylvestris is represented with abundant macrofossils between 4800 and 2100 cal. BP. It is suggested that a marked P. sylvestris decrease about 2100 cal. BP may be a combined effect of human impact and climatic deterioration. A possible final termination of the P. sylvestris population about 1600 cal. BP may be considered human-made.     

Contribution to the flora history of the genus Polemonium with special reference to North Norway

A key for the identification of pollen of the European species of Polemonium is presented. Fossil pollen records from Norway are surveyed and discussed. The records available show that pollen is derived both from natural stands close to the shoreline, and from plants established as apophytes in grazed meadows. It is suggested that P. caeruleum is a Late Glacial element, which arrived from the south at least, but probably also from the northeast. Pollen of P. boreale -type has a wider distribution in the Late Weichselian, at least in northern Russia. A pollen diagram from Bodø illustrates the fossil record occurrence of Polemonium in a Late Holocene sequence.     

Holocene climate and environmental history of Brurskardstjørni,a lake in the catchment of Øvre Heimdalsvatn,south-central Norway

The Holocene lake history, vegetation history and climate history of Brurskardstjørni, an alpine lake in the Jotunheimen Mountains of south-central Norway, are reconstructed. The reconstructions are based on fossil pollen, plant macrofossils, diatoms, chironomids and sediment characteristics. Subsequent to deglaciation, the lake was formed at about 11,000 cal years BP. A diverse chironomid assemblage quickly colonised the lake, whereas the first diatoms were found about 400 years later. At that time, the lake water was turbid with a high pH. The surrounding soils were immature and unstable and dominated by open pioneer vegetation. Compared to the present, summer temperatures were warmer and there was less winter precipitation. From about 10,000 cal years BP, local organic production increased rapidly and from about 9,500 cal years BP a few macrofossils and a high pollen influx of birch suggest that the tree-line was close to the lake. Pine most likely reached its highest tree-line altitude around 9,000 cal years BP and has receded since that time. From about 5,000 cal years BP, the total amount of trees and shrubs decreased and the landscape became more open, probably due to decreasing temperatures and increasing effective moisture lowering the birch tree-line. Coinciding with a cooling during the last 3,000 years, lake-water pH decreased. There is large incongruence between the Holocene July temperatures inferred from pollen and chironomids. The biological proxies responded to a combined effect of environmental change and biotic interactions. This response is interpreted with reference to taxon–environment relationships in the modern calibration data sets and with reference to the latent structure and ecological demands of the fossil assemblages.     

Forest response to climate changes in Atlantic Equatorial Africa during the last 4000 years BP and inheritance on the modern landscapes

This review paper synthesizes the recent published palaeoecological results obtained in Atlantic Equatorial Africa (ECOFIT program) on the history of forest ecosystems and inferred climate changes during the past 4000 years. Evidence are mainly provided by pollen analysis carried out at nine sites from Congo, Cameroon and Ghana, locally supported by macroflora remains, phytoliths, diatoms, δ¹³C and mineralogical data. At all the sites, except Lake Bosumtwi (Ghana), following a large expansion of rain and mesophilous forests until 3000 years BP , a major change is registered, affecting floristic composition, structure and geographical distribution. According to the hydrological sensitivity of the different sites, local openings of the forests with development of heliophilous formations and/or isolated enclosed savannas are observed at the most humid sites; complete disappearance of forested formations at the driest. The agreement between pollen records, hydrological and hydrobiological data definitely demonstrates that an arid event has been the primary driving factor of this change and is responsable for the main features of the modern landscapes in Atlantic Equatorial Africa. Moreover, the most recent palaeoecological data obtained in Congo (Lake Sinnda), indicate that this Late Holocene increasing aridity was of longer duration, from 4000 to 1300 years BP , and more progressive than previously inferred. A new expansion of forests is locally detected c. 900–600 BP despite increased human impact.     

Osmunda regalis in the early Holocene of Western Norway

A fossil sporangium and spores of Osmunda regalis were found in sediments bio-stratigraphically dated to about 9500 years old on the island of Utsira, SW Norway. The ages of the Utsira remains and finds of spores from Jæren indicate that Osmunda immigrated into Norway, perhaps from Britain, during the first 1000 years of the Holocene. The ages of its recorded arrival at other sites show that Osmunda spread rapidly within the limits of its present distribution in Norway by about 8300 BP.     

Sensitivity of IgG-ELISA for Detecting Airborne Pollen Antigens of Betulaceae

Pollen sculpture elements of four Rhododendron species from 49 populations were studied using scanning electron microscopy. The sculpture in the polar areas of the studied taxa pollen differed in type, shape, size, and distribution of individual elements. There were five sculpture types identified. The pollen of Rhododendron ledebourii from various populations in Altai revealed sculpture elements characteristic of R. dauricum, R. mucronulatum, and R. sichotense, questioning the taxonomic position of the former species. Analysis of the geographical distribution of sculpture types clarified species boundaries and zones of sympatric distribution. The northern boundary of R. mucronulatum was expanded and new populations of R. sichotense were revealed. In the sympatric zones of R. mucronulatum and R. sichotense, there were intermediate populations showing pollen sculptures typical of R. dauricum, R. mucronulatum, and R. sichotense. The sculpture diversity observed in the pollen of R. dauricum, together with its presence in sympatric zones, suggests that it is probably a hybrid of R. sichotense and R. mucronulatum or a subspecies of R. sichotense.     

Massive settlements of the Pacific oyster, <Emphasis Type="Italic">Crassostrea gigas</Emphasis>, in Scandinavia

The Pacific oyster (Crassostrea gigas) is an important aquaculture species world-wide. Due to its wide environmental tolerance and high growth rate, it has also become a successful invader in many areas, leading to major ecosystem changes. Low water temperatures were previously believed to restrict the establishment of Pacific oysters in Scandinavia. However, recent surveys reveal that the Pacific oyster is now established in many areas in Scandinavia. We present data on the current distribution, abundance and age-structure in Denmark, Sweden and Norway. The biomass of oysters in the Danish Wadden Sea increased from 1,056 to 6,264 tonnes between 2005 and 2007. Massive settlements were observed along the Swedish west coast in 2007, with densities >400 oysters per m⁻². In Norway, populations are established on the southern coast, and specimens have been found as far north as 60°N. The potential impacts and probable causes of this recent large-scale establishment are discussed.     

Pinus pollen season trend in South Spain

In Andalusia (southern Spain), Pinus species are found in mountainous areas and nature reserves, though some species are also grown as ornamentals in cities. Annual airborne pollen trends are regarded as an indicator of variations in climate prompted by overall climate change. Airborne pollen concentration also provides a useful tool for analyzing alterations in the distribution of vegetation in response to environmental factors and to changes in land use. The present study analyzed the Pinus pollen season over 22 years (1993–2014) in 4 Andalusian cities (Córdoba, Granada, Jaén, and Málaga), and examined correlations between airborne pollen concentrations and meteorological parameters (temperature and rainfall). Pinus pollen season lasted from March to June, starting first in Málaga and later in eastern Andalusia. Differences between the pollen curves for each city were attributable to differing proportions of pine species in each province. Temperatures during the months prior to flowering tended to fall, prompting delayed onset of the pollen season in most cities. No significant results were observed for rainfall patterns in most cities. Total pollen concentrations increased at most sites, suggesting that the recorded decline in pine-nut output was not influenced by flowering rates, but to the impact of a local pest.     

The role of the expansion of native-invasive plant species in coastal dunes: The case of Retama monosperma in SW Spain

Invasion by allochthonous plant species are identified, at present, among the main conservation hazards to coastal dunes. Nevertheless, the role of the expansion, with invasive character, of native species in these ecosystems has received little attention in ecological studies. In recent decades, Retama monosperma, a late colonizing legume shrub found in coastal sandy areas, endemic to the SW of the Iberian Peninsula and NW Morocco, has displayed invasive behavior in coastal dunes in different parts of the world, including its natural area of distribution. Its rapid expansion and increase in coverage has significantly contributed to the dune stabilization process, sometimes involving notable changes in the environment, plant community and shaping local distribution of some associated fauna, thus modifying the functioning of the whole ecosystem. In this review we examine the role of the expansion of R. monosperma in SW Spain coastal dunes, causes and implications, in the context of the ecological theory of invasions, and comparing it with other case studies.     

Climatic and human effects on the post-glacial dynamics of <Emphasis Type="Italic">Fagus</Emphasis> <Emphasis Type="Italic">sylvatica</Emphasis> L. in NW Iberia

Our aim is to determine the population dynamics of Fagus sylvatica L. during the last 4,000 cal. BP in NW Iberia and the causes of its spatial and temporal patterns, previous palaeoecological studies having shown that between the Upper Pleistocene and the recent Holocene Fagus survived in this region. A number of pollen sites have allowed a reconstruction of the regional dynamics of Fagus from the Last Glaciation to the present. Specifically, two high-resolution pollen sequences located in both extremes of the Cantabrian region were analysed to discuss the beech forest dynamics during the last four millennia. Beech pollen percentages increased progressively to dominant species levels in eastern Cantabria, but only brief, minor increases are recorded in the west, where they never exceeded 2%. The expansion in the east shows three well-defined stages: an initial increase that lasted up to about 2,500 cal. BP, coinciding with a general increase in total tree pollen throughout the Cantabrian Mountains; a stage lasting between 2,500 and 1,500 cal. BP, in which Fagus pollen levels fluctuated while total tree pollen percentages began to decline and Ericaceae to increase; and a final further increase peaking around 1,250 cal. BP. The first stage (ca. 4,000–2,500 cal. BP) probably formed part of the final ascent of the tree line at the end of the mid-Holocene as the consequence of climatic improvement. Its maintenance during the second stage, while other tree species began to recede under unstable environmental conditions, is attributable to displacement of other genera such as Corylus and Quercus. Its final peak may have been facilitated by human disturbance of woodland, Fagus being a competitive species readily able to take advantage of such disturbances. That no such process occurred in the western Cantabrian area may be due to both the direct biological influence of harsher climatic conditions, and the lack of interest by human populations in settling highlands, which is attributable both to this climatic factor and to the fact that, compared with the east, this area has a greater extent of lowland and wide flat valleys where settlements were concentrated.     

Introduction: International conference on forest ecosystems: Ecology,conservation and sustainable management

Abstract

A pollen diagram from a small lake, Kutulahdenlampi, in northern Finland is interpreted in terms of the development of forest vegetation during the Holocene. The abundance of each of the forest taxa is considered independently by means of pollen accumulation rates (PARs), using as the reference material, long term average pollen deposition values monitored by a network of pollen traps. Particular attention is paid to the arrival of spruce and to the species in the original forests that this newcomer replaces. A model of pollen dispersal and deposition developed by Sugita is used to estimate the area around the lake that the pollen assemblage is most clearly reflecting. This relevant source area of pollen (RSAP), for the present day situations is c. 1,500 m. Pollen loadings calculated for a simulated landscape that mimics (i) that of the present day and (ii) for the situation at 8,000 BP (as deduced from the PARs) are compared with the pollen assemblages from the diagram at those points in time, and are seen to be compatible. The advantages of combining PAR and modelling to look at the spatial scale of vegetation reconstructions are discussed.     

Local adaptation at the range peripheries of Sitka spruce

High‐dispersal rates in heterogeneous environments and historical rapid range expansion can hamper local adaptation; however, we often see clinal variation in high‐dispersal tree species. To understand the mechanisms of the species’ distribution, we investigated local adaptation and adaptive plasticity in a range‐wide context in Sitka spruce, a wind‐pollinated tree species that has recently expanded its range after glaciations. Phenotypic traits were observed using growth chamber experiments that mimicked temperature and photoperiodic regimes from the limits of the species realized niche. Bud phenology exhibited parallel reaction norms among populations; however, putatively adaptive plasticity and strong divergent selection were seen in bud burst and bud set timing respectively. Natural selection appears to have favoured genotypes that maximize growth rate during available frost‐free periods in each environment. We conclude that Sitka spruce has developed local adaptation and adaptive plasticity throughout its range in response to current climatic conditions despite generally high pollen flow and recent range expansion.     

Holocene Palynological Records in Lake Selincuo,Northern Xizang

Selincuo (31°34′–31°57′N, 88°31′–89°21′E)is one of the great lakes in northern Xizang surrounded by alpine grassland, composed mainly of Stipa purpurea, S, subssessifolia var. bassipulomosa. A 3.08 m long core has been taken from a water depth of 27 m, 3 km to the north from the lake. Palynological records of the core combined with surface sample results have revealed from the regional as well as local vegetational and environmental history since the last 12 000 a BP, a very low pollen concentration (19–209 grains/g), mainly of airborne pollen, which indicated a treeless alpine sparse vegetation. A great vegetation change took place at Ca. 9 600 a BP when alpine sparse vegetation was replaced by alpine grassland lasting until Ca. 6 000 a BP. Quite a number of tree pollen grains found in this time interval might be explained as a result of expansion of forests somewhere around the Xizang Plateau. These changes must have caused by climatic warming during the Early Holocene. During the last 6 000 years the vegetation had remained as the alpine grassland, although probably more luxurouste than before, but their was an obvious increase of arboreal pollen, such as the increase of Abies during Ca. 6 000–4 000 a BP, Picea 4 000–2 200 a BP, Pinus 2 200–1 000 a BP which indicated continuous expansion of forests growing around the plateaus. During the last 1 000 years both the concentration and proportion of the arboreal pollen decreased and those of Cypraceae pollen increased sharply. This might mean a reduction of the forests around the plateau and an expansion of swamps around the lake.     

The Fagus sylvatica forests in the Larvik region, south-eastern Norway: their origin and history

The origin and developmental history of Fagus sylvatica forests in south-eastern Norway have been studied through pollen analysis and AMS radiocarbon-dating of peat from two small forest hollows. In this area F. sylvatica appears to have a long history, from the first occurrence of F. sylvatica pollen at ca. 9100 cal. b.p. to its local expansion ca. 1300–1200 cal. b.p. At this time a shift from a diverse landscape mosaic with many plant taxa present, including broad-leaved trees, to a less diverse landscape mosaic with Picea abies and F. sylvatica trees is interpreted from the pollen data. The long history of F. sylvatica suggests that the existing forests are not recent plantations, but implies that these forests are native. The presence of pollen indicative of anthropogenic activity combined with charcoal before the expansion of F. sylvatica, as well as comparison with data from nearby sites, suggest that the forest development was likely to be a result of human activity and climatic changes, particularly changes in moisture conditions.     

Recovery process of genetic diversity through seed and pollen immigration at the northernmost leading-edge population of Fagus crenata

The range expansion of a plant species begins with colonization of ecological empty patches from posterior source populations. This process involves stochastic loss of genetic diversity. However, the founder population could restore genetic diversity by gene flow from posterior populations via seeds and pollen and its recovery affects evolutionary potential for species expansion. To clarify the recovery process of genetic diversity during species range expansion, gene flow via seeds and pollen was investigated at the expansion front of Fagus crenata. Based on eight nuclear microsatellite genotypes of a total of 150 individuals and 225 seeds at the northernmost leading-edge population, genetic diversity, fine-scale spatial genetic structure (FSGS), and genetic differentiation from other five northern populations were investigated. Moreover, both seed and pollen immigration and their effects on genetic diversity at different successional stages were analyzed. The leading-edge population showed lower genetic diversity and substantial genetic differentiation, reflecting its strong genetic drift. Non-significant FSGS and a negative inbreeding coefficient for mature trees may indicate that the earliest generation consisted of founders from foreign seed sources. The significant proportion of seed and pollen immigration increased the number of different alleles for later successional stages. The effective number of pollen parents from foreign sources (20.8) was markedly higher than that from the local source (2.1). These results indicated that pollen immigration incorporated new and rare alleles and increased the genetic diversity of the population. However, the proportion of foreign gene flow decreased during succession, probably due to the increased reproductive success of local individuals as they reached maturity and grew in size.     

Spatial variation in local pollen flow and mating success in a Picea abies clone archive and their implications for a novel ��breeding without breeding�� strategy

Currently, Norway spruce (Picea abies) breeding in Sweden is based on crosses between the best clones followed by clonal testing of the progenies to select for the long-term breeding population. An alternative breeding strategy called “Breeding without Breeding” (BwB) is proposed, which, in principle, relies on the DNA marker-based pedigree reconstruction from wind-pollinated progenies instead of controlled crosses. To test whether the pedigree structure could be established from progenies of clonal trials, we investigated the spatial pattern of local pollen flow and paternity assignment in a clone archive of Norway spruce. The results showed that 42% of the progeny can be assigned to fathers within 30-m distance with high confidence. Effective pollen dispersal decreased rapidly with distance and followed exponential distribution on local scale. The extent of close-neighbor (within 6 m) mating ranged from 0% to 48% among grafts with an average of 13%. Distance explained 25% deviance in mating success, and other factors such as phenology and spatial configuration of the clones should have contributed the rest. The success of parentage assignment in clone archive opens up the possibility to apply BwB in clonal trials of species that are easy to propagate vegetatively. This procedure could substantially shorten the breeding cycle and still give similar gain per year as the conventional breeding.     

A satellite-based map of onset of birch (<Emphasis Type="Italic">Betula</Emphasis>) flowering in Norway

Birch (Betula pubescens L.) is by far the most common deciduous tree in Norway and birch forests define the forest line both northwards and upwards. Because of its mountainous topography, long fjords, and long length from north to south, Norway is climatically and ecologically very diverse. Therefore, developing pollen forecasts in Norway is a challenging task. In this study we use MODIS-NDVI (normalized difference vegetation index) satellite data with 250 m spatial resolution and 16-days time resolution for the period 2000–2007, and birch pollen counts from ten Burkad traps distributed throughout Norway, to characterize the onset of birch flowering in Norway. Four of the seven trap stations with long-term series show significant values at the 5% level or better between the MODIS-NDVI defined onset and the date when the annual accumulated birch pollen sum reaches 2.5% of the annual total. A map of Norway that shows the eight-year mean (2000–2007) onset of birch flowering was produced. It reveals large differences in the timing of the onset of birch flowering along the north–south and altitude gradients. The map provides useful general information that can be utilized by the Norwegian pollen forecast service. This study shows that remote sensing is a useful tool for not only characterizing the onset of the birch pollen season but also revealing regional differences not easily detected by pollen stations alone.     

Paleotemperatures of La Malinche: a palynological hypothesis

Paleotemperatures of the last 10,000 years at 3,100 m elevation on La Malinche volcano (Mexico) were reconstructed by treating pollen analytic data by Ohngemach and Straka with numerical techniques. Pollen data from 104 modern and 97 fossil samples were analyzed in order to: (1) calibrate transfer functions linking modern pollen data to climate and vegetation data from available maps (and cross-validate the predictive model of temperature on modern data sets), and (2) reconstruct paleotemperature for the last 10,000 years from fossil pollen data. A paleotemperature curve was obtained, that ranges between 7°C in the glacial period and 12.5°C at 8,000 years BP. It matches glacial stratigraphy. Temperature is described as follows: Section S1 (from the deposit's bottom to 8,500 years BP) from 7 to 8°C. S2 from 9.0 to 11°C. S3 (around 8,000 years BP) 11.5–12.5°C. S4 from 12 to 9°C. S5 (2,700 years BP) has poor pollen concentration and estimates are unreliable. S6 from 9 to 5.5°C. S7 (around 1,550 years BP) from 6.5 to 7.5°C; S8 (ending 1.000 years BP), from 7.5 to 9.5°C and includes anthropogenic influences. S6 is given a new interpretation: open vegetation with low local pollen production and greater influence of long distance components.     

Pollen morphology and its systematic and ecological significance in Rheum (Polygonaceae) from China

Pollen morphology of 40 species of Rheum , belonging to eight sections, was investigated under LM and SEM. Four new exine patterns were found in the species: a) microechinate-foveolate, b) rugulate, c) verrucate-perforate, and d) verrucate-rugulate ornamentation. In addition, two patterns, the Rheum-type pollens with microechinate-perforate and fine-reticulate, as previously described, were also confirmed in the present study. Based on above study the evolution trends of pollen morphology in the taxa involved were discussed phylogenetically as below. As microechinate-perforate exine pattern existed commonly, the pattern is, therefore, regarded as the most primitive among all the six types. The fine-reticulate type was thought as a derivative type, deriving from the basic microechinate-foveolate-perforate pattern, and followed by the rugulate and verrucate-perforate ornamentation. The verrucate-rugulate ornamentation should be the most advanced. More than one pollen type often exist in most of the sections in Rheum. The pollen morphology of Rheum was strongly correlated with its geographical and ecological distribution. Three medicinally important species R. officinale, R. palmatum and R. tanguticum can be palynologically distinguished by their ornamentations.     

History of Late Holocene vegetation at Quintana Roo,Caribbean coast of Mexico

A pollen record of a Late Holocene sediment core from the Mexican Caribbean coast (Quintana Roo) shows the development and changes of a mangrove system. Humid conditions seem to have persisted for the period approximately 2500–1500 ¹⁴C yr BP (pollen zone I), and mangrove Rhizophora mangle dominated with a good representation of elements from the nearby semi-evergreen tropical forest. During the period approximately 1500–1200 ¹⁴C yr BP (pollen zone II) the mangrove Conocarpus erecta dominated. R. mangle almost disappeared and other taxa appeared, suggesting drier climatic conditions and generally more open vegetation. This dry period coincided with the period of the Maya cultural decline. The following period (pollen zone III, approximately 1200–1000 ¹⁴C yr BP) was characterized by the recovery of R. mangle, indicating more humid conditions than in the preceding pollen zone. Pollen zone IV (approximately 1000 ¹⁴C yr BP till present) suggests a drier period reoccuring with C. erecta; this marks the transition to present day conditions.