Characterization of the NOP -1 opsin photoreceptor in the filamentous fungus Neurospora crassa

Light absorption is an important process for energy production and sensory perception in many organisms. In the filamentous fungus, Neurospora crassa, blue-light is an important regulator of both asexual and sexual development, but the identity of the blue-light receptor is unknown. The work presented in this dissertation initiated the characterization of the putative N. crassa opsin photoreceptor, NOP-1. Opsins were thought to exist only in the archaea and mammals until the discovery of nop-1. All opsins have the same conserved structure of seven transmembrane helical domains with a lysine residue in the seventh helix specific for forming a Schiff-base linkage with retinal. The predicted NOP-1 protein sequence is equally similar to archaeal rhodopsins and a newly identified fungal opsin-related protein group (ORPs). ORPs maintain the seven transmembrane helical structure of opsins, but lack the conserved lysine residue for binding retinal. An ORP gene, orp-1 was identified in N. crassa and this work includes the cloning and sequence analysis of this gene. Characterization of NOP-1 function in N. crassa development began with the construction of a Δnop-1 deletion mutant. Extensive phenotypic analysis of Δnop-1 mutants revealed only subtle defects during development primarily under environmental conditions that induce a stress response. NOP-1 was overexpressed in the heterologous system Pichia pastoris, and it was demonstrated that NOP-1 protein bound all-trans retinal to form a green-light absorbing pigment (λmax = 534 nm) with a photochemical reaction cycle similar to archaeal sensory rhodopsins. nop-1 gene expression was monitored during N. crassa development. nop-1 transcript is highly expressed during asexual sporulation (conidiation) and transcript levels are abundant in the later stages of conidial development. nop-1 expression is not regulated by blue-light or elevated temperatures. Potential functions for NOP-1 were discovered through the transcriptional analysis of conidiation-associated genes in Δnop-1 mutants. NOP-1 exhibits antagonistic transcriptional regulation of conidiation-associated genes late in conidial development, by enhancing the carotenogenic gene, al-2 and repressing the conidiation-specific genes, con-10 and con-13. ^

Evaluation of long chain 1,14-alkyl diols in marine sediments as indicators for upwelling and temperature

Long chain alkyl diols form a group of lipids occurring widely in marine environments. Recent studies have suggested several palaeoclimatological applications for proxies based on their distributions, but also revealed uncertainties about their applicability. Here we evaluate the use of long chain 1,14-alkyl diol indices for reconstruction of temperature and upwelling conditions by comparing index values, obtained from a comprehensive set of marine surface sediments, with environmental factors like sea surface temperature (SST), salinity and nutrient concentrations. Previous cultivation efforts indicated a strong effect of temperature on the degree of saturation and the chain length distribution of long chain 1,14-alkyl diols in Proboscia spp., quantified in the diol saturation index (DSI) and diol chain length index (DCI), respectively. However, values of these indices in surface sediments show no relationship with annual mean SST of the overlying water. It remains unknown what determines the DSI, although our data suggests that it may be affected by diagenesis, while the relationship between temperature and DCI may be different for different Proboscia species. In addition, contributions of algae other than Proboscia diatoms may affect both indices, although our data provide no direct evidence for additional long chain 1,14-alkyl diol sources. Two other indices using the abundance of 1,14-diols vs. 1,13-diols and C30 1,15-diols have previously been applied as indicators for upwelling intensity at different locations. The geographical distribution of their values supports the use of 1,14 diols vs. 1,13 diols [C28 + C30 1,14-diols]/[(C28 + C30 1,13-diols) + (C28 + C30 1,14-diols)] as a general indicator for high nutrient or upwelling conditions.