Results of n-alkane biomarker analyses and paleoclimate reconstruction

The current study presents quantitative reconstructions of tree cover, annual precipitation and mean July temperature derived from the pollen record from Lake Billyakh (65°17'N, 126°47'E, 340 m above sea level) spanning the last ca. 50 kyr. The reconstruction of tree cover suggests presence of woody plants through the entire analyzed time interval, although trees played only a minor role in the vegetation around Lake Billyakh prior to 14 kyr BP (<5%). This result corroborates low percentages of tree pollen and low scores of the cold deciduous forest biome in the PG1755 record from Lake Billyakh. The reconstructed values of the mean temperature of the warmest month ~8-10 °C do not support larch forest or woodland around Lake Billyakh during the coldest phase of the last glacial between ~32 and ~15 kyr BP. However, modern cases from northern Siberia, ca. 750 km north of Lake Billyakh, demonstrate that individual larch plants can grow within shrub and grass tundra landscape in very low mean July temperatures of about 8 °C. This makes plausible our hypothesis that the western and southern foreland of the Verkhoyansk Mountains could provide enough moist and warm microhabitats and allow individual larch specimens to survive climatic extremes of the last glacial. Reconstructed mean values of precipitation are about 270 mm/yr during the last glacial interval. This value is almost 100 mm higher than modern averages reported for the extreme-continental north-eastern Siberia east of Lake Billyakh, where larch-dominated cold deciduous forest grows at present. This suggests that last glacial environments around Lake Billyakh were never too dry for larch to grow and that the summer warmth was the main factor, which limited tree growth during the last glacial interval. The n-alkane analysis of the Siberian plants presented in this study demonstrates rather complex alkane distribution patterns, which challenge the interpretation of the fossil records. In particular, extremely low n-alkane concentrations in the leaves of local coniferous trees and shrubs suggest that their contribution to the litter and therefore to the fossil lake sediments might be not high enough for tracing the Quaternary history of the needleleaved taxa using the n-alkane biomarker method.

Genes implicados en la respuesta molecular al estrés hídrico en Pinus pinaster Ait

La presente tesis doctoral se centra en el estudio de la respuesta molecular de las coníferas mediterráneas al estrés hídrico. Para ello se ha escogido como especie modelo Pinus pinaster Ait., la conífera más abundante en España, y que habita un amplio rango de situaciones ecológicas, especialmente en lo relativo a la disponibilidad de agua. En primer lugar, se ha aplicado un estrés hídrico controlado en cultivo hidropónico y se ha generando una genoteca sustractiva con objeto de identificar los genes inducidos por el estrés, analizando su expresión en raíces, tallos y acículas. A continuación, se ha analizado, la expresión de los genes anteriormente obtenidos así como de otros seleccionados de las bases de datos disponibles, durante una sequía prolongada en tierra, similar a las que las plantas deben afrontar en la naturaleza. Se ha utilizado en este caso, además de P. pinaster, P. pinea, otra conífera mediterránea adaptada a las sequías recurrentes. Este trabajo ha permitido identificar genes candidato expresionales, presumiblemente comunes en la respuesta molecular de las coníferas al déficit hídrico. Se han detectado diferencias notables en la expresión de determinados genes, que podrían ser los responsables de las diferencias exhibidas por ambas especies en el comportamiento frente a la sequía. Entre los genes identificados como inducidos por el estrés hídrico se encuentran varios miembros de la familia de las deshidrinas. Trabajos previos han utilizado deshidrinas como genes candidato; no obstante, la falta de especificidad de ciertos fragmentos y marcadores utilizados, debido a la complejidad estructural de esta familia, resta fiabilidad a algunos de los resultados publicados. Por este motivo, se ha estudiado en detalle esta familia en P. pinaster, se han identificado y caracterizado 8 miembros y se ha analizado su patrón de expresión frente a sequía. Este estudio ha permitido describir por primera vez unos segmentos conservados en la secuencia de aminoácidos de las deshidrinas de pináceas, cuya presencia y número de repeticiones parece estar relacionado con su especificidad. Por último, se han escogido tres genes implicados en distintas fases de la respuesta al estrés hídrico para su análisis exhaustivo: una deshidrina, una nodulina y un factor de transcripción tipo AP2. Se ha caracterizado su estructura exón/intrón y secuenciado su región promotora. Además, se han obtenido líneas transformadas que sobreexpresan estos genes tanto de forma heteróloga, en la especie modelo Arabidopsis thaliana, como en el propio P. pinaster. Este material facilitará la realización de futuros estudios sobre la función y el mecanismo de actuación de estos genes en la respuesta al estrés hídrico. ABSTRACT This thesis focuses in the study of the molecular response to water stress in Mediterranean conifers. For this purpose, P. pinaster was selected as model species. It’s the most abundant conifer in Spain, living in a wide range of ecological conditions, especially regarding water availability. First, we have applied a controlled polyethylene glycol-induced water stress in hydroponic culture and obtained a suppression subtractive hybridization (SSH) library, with the aim of identifying genes induced by water stress, analysing their expression in roots, stems and needles. We have then analysed the expression patterns of the identified genes, together with other genes selected from public databases. This study was conducted throughout a prolonged drought stress in soil, similar to the ones plants have to face in nature. In this case not only P. pinaster was analysed but also P. pinea, another Mediterranean conifer well adapted to recurrent droughts. This work has enabled us to identify of reliable candidate genes, presumably shared with other conifers in the response to water stress. We observed remarkable differences in the expression of some genes, which could be involved in the differential behaviour that these species show in the water stress response. Within the genes induced by water stress, several members of the dehydrin gene family were identified. Due to the structural complexity of the family, certain ambiguities and inconsistencies have been detected in previous works that have used dehydrins as candidate genes. For this reason, we have analysed thoroughly this gene family in P. pinaster, and have identified and characterized eight different members, whose expression patterns during drought have also been assessed. This study has allowed us to identify for the first time novel conserved segments in the amino acids sequences of Pinaceae. The presence and number of repetitions of these segments could be associated with the functional specificity of these proteins. Finally, three genes involved in different steps of the water stress response were selected for an exhaustive analysis: a dehydrin, a nodulin and an AP2 transcription factor. For all of them, the exon/intron structure was established and their promoter region was sequenced. Also, transformed lines were obtained both in Arabidopsis thaliana and in P. pinaster for the constitutive overexpression of these genes. This material will facilitate the development of further studies to investigate the function of these genes during the water stress response

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, DNA and Vegetation records from surface sediments of lacustrine lakes along a forest tundra - tundra transect at the Taymyr peninsula, northern Siberia

Reliable information of past vegetation changes are important to project future changes, especially for areas undergoing rapid transitioning such as the boreal treeline. The application of detailed sedDNA records has the potential to enhance our understanding of vegetation changes gained mainly from pollen studies of lake sediments. This study investigates sedDNA and pollen records from 31 lakes along a gradient of increasing larch forest cover in northern Siberia (Taymyr Peninsula) and compares them with vegetation field surveys within the lake's catchment. With respect to vegetation richness, sedDNA recorded 114 taxa, about half of them to species level, while pollen analyses identified 43 pollen taxa. Both approaches exceed the 31 taxa revealed by vegetation field surveys of 400 m**2 plots. From north to south, Larix percentages increase, as is consistently recorded by all three methods. Furthermore, tundra sites are separated from forested sites in the plots of the principal component analyses. Comparison of ordination results by Procrustes and Protest analyses yields a significant fit among all compared pairs of records. Despite the overall comparability of sedDNA and pollen analyses certain idiosyncrasies in the compositional signal are observed, such as high percentages of Alnus and Betula in all pollen spectra and high percentages of Salix in all sedDNA spectra. In conclusion, our results from the treeline show that sedDNA analyses perform better than pollen in recording site-specific richness (i.e. presence/absence of certain vegetation taxa in the direct vicinity of the lake) and perform as good as pollen in tracing regional vegetation composition.