Different coordination modes of an aryl-substituted hydrotris(pyrazolyl)borate ligand in rhodium and iridium complexes

Complexes Tp^tolRh(C₂H₄)₂ (1a) and Tp^tolRh(CH₂C(Me)C(Me)CH₂) (1b) have been prepared by reaction of KTp^tol with the appropriate [RhCl(olefin)₂]₂ dimer (Tp^tol means hydrotris(3-p-tolylpyrazol-1-yl)borate). The two complexes show a dynamic behaviour that involves exchange between κ² and κ³ coordination modes of the Tp^tol ligand. The iridium analogue, Tp^tolIr(CH₂C(Me)CHCH₂) (2) has also been synthesized, and has been converted into the Ir(III) dinitrogen complex [(κ⁴-N,N’,N’’,C-Tp^tol)Ir(Ph)(N₂) (3) by irradiation with UV light under a dinitrogen atmosphere. Compound 3 constitutes a rare example of Ir(III)-N₂ complex structurally characterized by X-ray crystallography. Its N₂ ligand can be easily substituted by acetonitrile or ethylene upon heating and denticity changes in the Tp^tol ligand, from κ⁴-N,N’,N’’,C (monometallated Tp^tol, from now on represented as Tp^tol′) to κ⁵-N,N′,N″,C,C″ (dimetallated Tp^tol ligand, represented as Tp^tol″) have been observed. When complex 3 is heated in the presence of acetylene, dimerization of the alkyne takes place to yield the enyne complex [(κ⁵-N,N′,N′′,C,C′-Tp^tol)Ir(CH₂CHCCH), 7¸ in which the unsaturated organic moiety is bonded to iridium through the carbon-carbon double bond.     

Heteroleptic κ(N,C)-2-phenylpyridine platinum complexes: The use of bis(pyrazolyl)borates as ancillary ligands

Luminescent platinum(II) bis(pyrazolyl)borate complexes bearing orthometalated phenylpyridines (based on 2-phenylpyridine, 3-hexyloxy-2-phenylpyridine and (4-(pyridine-2-yl)-phenyl)methanol) and bis(pyrazolyl)borate ligands (employed as potassium dihydridobis(pyrazolyl)borate and potassium dihydridobis(3,5-dimethylpyrazolyl)borate) have been synthesized and characterized. By reaction of K₂PtCl₄ with phenylpyridine ligands a precursor has been obtained which was further converted to the corresponding heteroleptic complexes. All platinum(II) bis(pyrazolyl)borate complexes have been investigated by nuclear magnetic resonance, Fourier transform infrared spectroscopy, thermal analysis and UV-Vis absorption spectroscopy. Luminescence as well as lifetime measurements in solution and in the solid state have been performed to establish a qualitative relationship between structure and luminescence properties. The absorption and emission properties of these complexes are governed by the nature of the orthometalating ligand with emission maxima ranging from 488 to 551 nm. Emission spectra at room temperature show well-resolved vibronic fine structures and a strong spin-orbit coupling. For the compounds under investigation the mixing of the excited states leads to apparent lifetimes in the microsecond regime (5.7-8.6 μs), rendering these materials phosphorescent.     

The site of regulation of light capture in Symbiodinium: Does the peridinin–chlorophyll a–protein detach to regulate light capture?

Dinoflagellates from the genus Symbiodinium form symbiotic associations with cnidarians including corals and anemones. The photosynthetic apparatuses of these dinoflagellates possess a unique photosynthetic antenna system incorporating the peridinin–chlorophyll a–protein (PCP). It has been proposed that the appearance of a PCP-specific 77 K fluorescence emission band around 672–675 nm indicates that high light treatment results in PCP dissociation from intrinsic membrane antenna complexes, blocking excitation transfer to the intrinsic membrane-bound antenna complexes, chlorophyll a–chlorophyll c₂–peridinin–protein-complex (acpPC) and associated photosystems (Reynolds et al., 2008 Proc Natl Acad Sci USA 105:13674–13678).We have tested this model using time-resolved fluorescence decay kinetics in conjunction with global fitting to compare the time-evolution of the PCP spectral bands before and after high light exposure. Our results show that no long-lived PCP fluorescence emission components appear either before or after high light treatment, indicating that the efficiency of excitation transfer from PCP to membrane antenna systems remains efficient and rapid even after exposure to high light. The apparent increased relative emission at around 675 nm was, instead, caused by strong preferential exciton quenching of the membrane antenna complexes associated with acpPC and reaction centers. This strong non-photochemical quenching (NPQ) is consistent with the activation of xanthophyll-associated quenching mechanisms and the generally-observed avoidance in nature of long-lived photoexcited states that can lead to oxidative damage. The acpPC component appears to be the most strongly quenched under high light exposure suggesting that it houses the photoprotective exciton quencher.     

Molecular mechanism of 2-APB-induced Ca influx in external acidification in PC12

2-Aminoethoxydiphenyl borate (2-APB) is used as a pharmacological tool because it antagonizes inositol 1,4,5-trisphosphate receptors and store-operated Ca²⁺ (SOC) channels, and activates some TRP channels. Recently, we reported that 2-APB enhanced the increase in cytotoxic [Ca²⁺]_i, resulting in cell death under external acidic conditions in rat pheochromocytoma cell line PC12. However, the molecular mechanism and functional role of the 2-APB-induced Ca²⁺ influx in PC12 have not been clarified. In this study, to identify the possible target for the action of 2-APB we examined the pharmacological and molecular properties of [Ca²⁺]_i and secretory responses to 2-APB under extracellular low pH conditions. 2-APB dose-dependently induced a [Ca²⁺]_i increase and dopamine release, which were greatly enhanced by the external acidification (pH 6.5). [Ca²⁺]_i and secretory responses to 2-APB at pH 6.5 were inhibited by the removal of extracellular Ca²⁺ and SOC channel blockers such as SK&F96365, La³⁺ and Gd³⁺. PC12 expressed all SOC channel molecules, Orai 1, Orai 2 and Orai 3. When we used an siRNA system, downregulation of Orai 3, but not Orai 1 and Orai 2, attenuated both [Ca²⁺]_i and secretory responses to 2-APB. These results suggest that 2-APB evokes external acid-dependent increases of [Ca²⁺]_i and dopamine release in PC12 through the activation of Orai 3. The present results indicate that 2-APB may be a useful pharmacological tool for Orai channel-related signaling.     

The role of TRPM2 in pancreatic β-cells and the development of diabetes

TRPM2 is a Ca²⁺-permeable non-selective cation channel that can be activated by adenosine dinucleotides, hydrogen peroxide, or intracellular Ca²⁺. The protein is expressed in a wide variety of cells, including neurons in the brain, immune cells, endocrine cells, and endothelial cells. This channel is also well expressed in β-cells in the pancreas. Insulin secretion from pancreatic β-cells is the primary mechanism by which the concentration of blood glucose is reduced. Thus, impairment of insulin secretion leads to hyperglycemia and eventually causes diabetes. Glucose is the principal stimulator of insulin secretion. The primary pathway involved in glucose-stimulated insulin secretion is the ATP-sensitive K⁺ (K_ATP) channel to voltage-gated Ca²⁺ channel (VGCC)-mediated pathway. Increases in the intracellular Ca²⁺ concentration are necessary for insulin secretion, but VGCC is not sufficient to explain [Ca²⁺]_i increases in pancreatic β-cells and the resultant secretion of insulin. In this review, we focus on TRPM2 as a candidate for a [Ca²⁺]_i modulator in pancreatic β-cells and its involvement in insulin secretion and development of diabetes. Although further analyses are needed to clarify the mechanism underlying TRPM2-mediated insulin secretion, TRPM2 could be a key player in the regulation of insulin secretion and could represent a new target for diabetes therapy.     

Lipid and DNA Evidence of Dominance of Planktonic Archaea Preserved in Sediments of the South China Sea: Insight for Application of the TEX86 Proxy in an Unstable Marine Sediment Environment

The marine planktonic archaea are dominated by Thaumarchaeotal Marine Group I, which is characterized by the lipid biomarker thaumarchaeol. The marine benthic archaea are characterized by greater diversity of currently unknown species whose lipid biomarker signatures are uncertain. In this study, a sediment core from the northwestern part of the South China Sea (SCS) (water depth 1474 m) was analyzed using molecular DNA and lipid biomarker approaches. While 16S rRNA gene analysis showed changing archaeal community structures with sediment depth, this change had little impact on the fossil record of archaeal lipids that are characteristic of the planktonic community. As a result, the fossil archaeal lipids recorded paleo sea surface temperature of the SCS since the last glacial maxima by the TEX₈₆ proxy, which agreed generally with the winter temperature recorded by planktonic foraminiferas collected from the same area of the SCS that hosted mass-transported deposits. This suggests that this deep water deposit may have partially preserved paleoclimate record reflecting seasonal temperature variation in a near shore setting, which is in contrast to annual sea surface temperature or sub sea surface temperature variation recorded by TEX₈₆ in the open ocean.     

The cationic composition and pH in the moulting fluid of Porcellio scaber (Crustacea, Isopoda) during calcium carbonate deposit formation and resorption

Before moulting, terrestrial isopods resorb calcium carbonate (CaCO₃) from the posterior cuticle and store it in sternal deposits. These consist mainly of amorphous calcium carbonate (ACC) spherules that develop within the ecdysial space between the anterior sternal epithelium and the old cuticle. Ions that occur in the moulting fluid, including those required for mineral deposition, are transported from the hemolymph into the ecdysial space by the anterior sternal epithelial cells. The cationic composition of the moulting fluid probably affects mineral deposition and may provide information on the ion-transport activity of the sternal epithelial cells. This study presents the concentrations of inorganic cations within the moulting fluid of the anterior sternites during the late premoult and intramoult stages. The most abundant cation is Na⁺ followed by Mg²⁺, Ca²⁺ and K⁺. The concentrations of these ions do not change significantly between the stages whereas the mean pH changed from 8.2 to 6.9 units between mineral deposition in late premoult, and resorption in intramoult, respectively. Measurements of the transepithelial potential show that there is little driving force for passive movements of calcium across the anterior sternal epithelium. The results suggest a possible role of magnesium ions in ACC formation, and a contribution of pH changes to CaCO₃ precipitation and dissolution.     

Paleoceanographic shifts and global events recorded in late Pliocene shallow marine deposits (2.80–2.55 Ma) of the Sea of Japan

Fossil ostracod assemblages from the upper Pliocene Kuwae Formation of the Kurokawa area, Niigata Prefecture, central Japan were investigated to discern the high resolution paleoceanographic changes in the Sea of Japan during the transitional interval from a warm to a cold climate in the period from 2.80 to 2.55 Ma, dated previously from diatom and nannofossil datum horizons and magnetostratigraphy. The studied ostracod assemblages did not contain Tsushima Warm Core Current taxa known in the modern Sea of Japan, and most of them are cryophilic and circumpolar. The combinations of recognized fossil ostracod assemblages differ from the modern ones of the region, suggesting that the shallow water area was probably colder than that of today. The Kuwae Formation was deposited during several bathymetric fluctuations between upper bathyal and lower sublittoral zone. A large-scale shift from upper bathyal to lower sublittoral condition, which dominated the depositional setting, occurred at 2.70 Ma in the Tainai area, and occurred rapidly during 40,000 years (2.70–2.66 Ma). This shallowing mirrored the shifts induced by global cooling recorded in various evidence such as oxygen isotope data from deep-sea core. Detailed paleodepth fluctuations show four shallowing events that occurred in this area between 2.80 and 2.55 Ma. The third and fourth shallowings at 2.70 and 2.60 Ma were both responses to global climatic cooling corresponding to the oxygen isotope stages G6 and/or G4, and to stage 104, respectively; deduced from the contemporary abundance of cold water species in the study section, observations of shallowing events in the northwestern Pacific Ocean, and the IRD event recorded in high latitude seas.     

Incorporating Restoration in Sustainable Forestry Management: Using Pine-Bark Mulch to Improve Native Species Establishment on Tephra Deposits

Native plant establishment is limited by harsh environmental conditions in areas affected by tephra deposition following volcanic eruptions. Late‐successional species might be lacking even decades after the disturbance. We assessed the effectiveness of pine‐bark mulch, a by‐product of sustainable timber production in the study area, in promoting the establishment and survival of a late‐successional species (Pinus pseudostrobus) and a nitrogen‐fixing legume (Lupinus elegans). We established a factorial experiment in areas covered with tephra during the eruption of the Paricutín volcano in the state of Michoacán, Mexico. After 1 year, P. pseudostrobus survival was significantly higher (p < 0.001) in plots with pine‐bark mulching (46.5%) than in plots without mulching (21.8%). After 2 years, surviving pines with mulching were significantly taller (p= 0.03) than pines without mulching (45.3 ± 3.8 cm and 31.2 ± 3.7 cm, respectively). Lupinus elegans plants survived longer when grown in plots with pine‐bark mulching than without mulching. Mulching reduced tephra temperatures during the dry season (when temperatures can reach up to 58°C 4 cm below the surface of bare tephra). Lupinus elegans plants were affected by herbivory by small rodents, run‐off, and frost at the end of the growing season. Our results suggest that mulching can ameliorate harsh environmental conditions on sites covered with tephra while incorporating a by‐product of sustainable forestry into restoration practice.     

Unique occurrence of pectin-like fibrillar cell wall deposits in xylem fibres of poplar

Using light and electron microscopic techniques, we studied the unique occurrence of fibrillar cell wall deposits in mature xylem fibres from poplar. These cell wall deposits lined the lumen-facing side of the wall, mainly in fibres next to vessel elements. Different lines of evidence point to the pectin-like nature of these fibrillar cell wall deposits. First, specific staining by Alcian Blue 8GX, a dye with high affinity for pectic substances. Second, the strongly reduced staining of the cell wall deposits in microscopic sections treated with pectolytic enzyme. Third, concomitant staining of pits, which are known to consist mainly of pectic substances. Given the pectin-like nature of the fibrillar cell wall deposits as well as their preferred occurrence in fibres neighbouring water-conducting vessel elements, a function for the fibrillar cell wall deposits in lateral water diffusion and stem water storage is hypothesised. The hypothesis is supported by the increased abundance of these cell wall deposits in wood tissue of a drought-sensitive poplar species.