Fragm. lat. III 15 - Liber Sextus Decretalium, cum apparatu (VI° 1.6.10 - 14)

Trägerband: Ms. Barth. 10; Vorbesitzer: Johannes Pincerna de Erbach; Bartholomaeusstift Frankfurt am Main

(Table 1) Organic carbon contents and vitrinite reflection in sediments from DSDP Holes 63-467, 63-471, and 64-481A

A number of C25 and C30 highly branched isoprenoid (HBI) sulphur compounds (E.G., thiolanes, 1-oxo-thiolanes, thiophenes, and benzo[b]thiophenes) with 2,6,10,14-tetramethyl-7-(3-methylpentyl)pentadecane and 2,6,10,14,18-pentamethyl-7-(3-methylpentyl)nonadecane carbon skeletons were identified in sediments, ranging from Holocene to Upper Cretaceous. These identifications are based on mass spectral characterisation, desulphurisation, and, in some cases, by comparison of mass spectral and relative retention time data with those of authentic standards. The presence of unsaturated C25 and C30 HBI thiolanes in a Recent sediment from the Black Sea (age 3-6 ka) strongly supports their formation during early diagenesis. The co-occurrence of HBI polyenes (C25 and C30) and unsaturated HBI thiolanes (C25 and C30) possessing two double bonds less than the corresponding HBI polyenes, in this Recent sediment, testifies to the formation of unsaturated HBI thiolanes by a reaction of inorganic sulphur species with double bonds of the HBI polyenes. Furthermore, a diagenetic scheme for HBI sulphur compounds is proposed based on the identification of HBI sulphur compounds in sediment samples with different maturity levels.

Experimental assessment of the effects of sublethal salinities on growth performance and stress in cultured tra catfish (Pangasianodon hypophthalmus)

The effects of a range of different sublethal salinities were assessed on physiological processes and growth performance in the freshwater ‘tra’ catfish (Pangasianodon hypophthalmus) juveniles over an 8-week experiment. Fish were distributed randomly among 6 salinity treatments [2, 6, 10, 14 and 18 g/L of salinity and a control (0 g/L)] with a subsequent 13-day period of acclimation. Low salinity conditions from 2 to 10 g/L provided optimal conditions with high survival and good growth performance, while 0 g/L and salinities[14 g/L gave poorer survival rates (p\0.05). Salinity levels from freshwater to 10 g/L did not have any negative effects on fish weight gain, daily weight gain, or specific growth rate. Food conversion ratio, however, was lowest in the control treatment (p\0.05) and highest at the maximum salinities tested (18 g/L treatment). Cortisol levels were elevated in the 14 and 18 g/L treatments after 6 h and reached a peak after 24-h exposure, and this also led to increases in plasma glucose concentration. After 14 days, surviving fish in all treatments appeared to have acclimated to their respective conditions with cortisol levels remaining under 5 ng/ mL with glucose concentrations stable. Tra catfish do not appear to be efficient osmoregulators when salinity levels exceed 10 g/L, and at raised salinity levels, growth performance is compromised. In general, results of this study confirm that providing culture environments in the Mekong River Basin do not exceed 10 g/L salinity and that cultured tra catfish can continue to perform well.

缺磷胁迫导致高等植物叶片中磷脂酰甘油（PG）含量降低的机理研究

磷脂酰甘油（PG）是植物类囊体膜中唯一的磷脂，在它的sn-2位上总是连着一个棕榈酸（16：0）或反式十六碳烯酸（16：1 trans）。由于PG的分子结构独特，对它的功能已有了很多研究，目前认为PG在维持类囊体膜的结构与功能方面具有非常重要的作用。缺磷胁迫下，蓝藻、衣藻及拟南芥、大麦等物种中均检测到了PG含量的下降。对这一现象的常见解释是缺磷导致了PG生物合成受阻，从而引起了其含量的降低。但迄今为止尚没有试验证据支持。本研究比较了缺磷对不同叶龄的小麦与烟草叶片中PG含量与PG水解酶的活性的影响，同时对缺磷叶片酶粗提液水解外源PG后的主要产物、几种磷脂酶抑制剂对上述酶反应的影响等进行了研究，以阐明缺磷条件下叶片中PG含量下降的主要原 因。 缺磷小麦第一叶完全展开时，PG含量与PG水解酶活性均与对照相似;而第三叶完全展开时，尽管缺磷第三叶中PG水解酶活性也与对照相似，但其PG含量低于对照。这一结果表明，在小麦叶片完全展开之前，缺磷条件未影响叶片中的PG水解酶活性，第三叶中较低的PG含量应由PG的生物合成受阻引起。并且，由于缺磷植株第一叶完全展开时PG含量未受影响而第三叶中却表现出了轻微降低，可以推测叶片萌发越晚，PG生物合成受到的抑制就会越严重。 为了研究叶片衰老过程中PG含量下降的原因，我们比较了6，10，14与18日龄时缺磷与对照小麦植株第一叶中PG的相对含量与PG水解酶活性。研究发现：6日龄时，刚刚完全展开的缺磷和对照小麦第一叶中无论是PG含量还是PG水解酶活性都较为相似;而随着叶片的逐渐衰老，缺磷植株第一叶中PG含量大幅度下降，同时伴随着PG水解酶活性的急剧上升。18日龄时，缺磷小麦第一叶中的PG含量较对照降低了69.1%，其PG水解酶活性也远高于对照，37ºC下温育30min后，缺磷叶片的酶粗提液使外源PG含量降低了74.16%，而对照中只降低了13.7%。上述结果表明，缺磷条件下，小麦叶片中PG含量降低的程度与PG水解酶活性的强弱密切相关，PG水解加剧是导致老叶中PG含量降低的一个重要原因。 磷脂酶是水解磷脂的主要酶类。目前在植物体中发现的磷脂酶种类主要有磷脂酶D（PLD）、磷脂酶C（PLC）与磷脂酶A（PLA）。通过薄层层析（TLC），我们发现缺磷小麦叶片的酶粗提液水解外源PG后的主要产物是磷脂酸（PA）、二脂酰甘油（DAG）与游离脂肪酸（FFA）。将n-丁醇加入到缺磷小麦叶片的体外酶反应体系中后，观察到PA、DAG与FFA的生成量均表现出一定程度的降低。由于n-丁醇是PA经PLD途径生成的抑制剂，因此，上述结果表明PLD参与了缺磷条件下小麦叶片中PG的水解。硫酸新霉素是PLC的非特异性抑制剂，低浓度的硫酸新霉素（100μM 和 200μM ）加入到缺磷小麦叶片的体外酶反应体系后，三种产物的生成受到了严重抑制，表明PLC也与缺磷叶片中PG的降解密切相关。 为了进一步分析缺磷导致PG含量降低的原因，我们以烟草为试验材料，检测了缺磷胁迫对烟草嫩叶和老叶中的PG含量、PG水解酶活性、与PG降解相关的酶的种类及PLC、PLDα、PLDβ与PAT-1基因在mRNA上表达水平的的影响。结果表明，缺磷烟草叶片中PG含量的降低由PG生物合成受阻与PG降解加剧共同导致，PLC和PLD活性与烟草叶片中PG的降解有关。缺磷植株老叶中PG水解酶活性及PLC、PLDα、PLDβ基因在mRNA水平上的表达量均高于对照，表明在磷胁迫条件下，老叶中PG水解酶活性可能受到转录水平上的调节， PLC、PLDα、PLDβ转录活性的增强导致了PLC、PLD活性加强，从而引起PG降解的加剧，最终导致了PG含量的降低。与PLC、PLDα和PLDβ不同，缺磷胁迫对patatin蛋白（表现PLA2活性）的编码基因PAT-1在转录水平上的表达无影响，TLC分析PG的水解产物也未检测到溶血磷脂酰甘油（LPG）的生成。由此可见，PLA活性可能与缺磷条件下PG的降解无关。

Thermal and mechanical shocks affecting the first flush of production of Lentinula edodes on Eucalyptus saligna logs

O objetivo deste trabalho foi avaliar o efeito do choque térmico e mecânico na produtividade de Lentinula edodes em 140 toras de Eucalyptus saligna, completamente colonizadas pelo fungo, em diferentes tempos de imersão em água e no primeiro fluxo de produção. As toras foram imersas em água resfriada (16ºC) ou à temperatura ambiente (22ºC); os períodos de imersão corresponderam a 6, 10, 14, 18, 22, 26 e 38 horas; o choque mecânico foi acompanhado por três quedas consecutivas da tora, em posição vertical, no chão. A temperatura da água e o tempo de imersão afetaram a produção de L. edodes, resultando em aumentos significativos (2 a 4 vezes) nos tratamentos em que as toras foram submetidas à água resfriada e nos tempos de imersão mais curtos (6 e 10 horas). O choque mecânico não resultou em aumento na produção de basidiomas.

A comparison between multi-proxy and historical data of drift-ice conditions on the East Greenland shelf

The reduction in sea ice along the SE Greenland coast during the last century has severely impacted ice-rafting to this area. In order to reconstruct ice-rafting and oceanographic conditions in the area of Denmark Strait during the last ~150 years, we conducted a multiproxy study on three short (20 cm) sediment cores from outer Kangerdlugssuaq Trough (~300 m water depth). The proxy-based data obtained have been compared with historical and instrumental data to gain a better understanding of the ice sheet-ocean interactions in the area. A robust chronology has been developed based on 210Pb and 137Cs measurements on core PO175GKC#9 (~66.2°N, 32°W) and expanded to the two adjacent cores based on correlations between calcite weight percent records. Our proxy records include sea-ice and phytoplankton biomarkers, and a variety of mineralogical determinations based on the <2 mm sediment fraction, including identification with quantitative x-ray diffraction, ice-rafted debris counts on the 63-150 µm sand fraction, and source identifications based on the composition of Fe oxides in the 45-250 µm fraction. A multivariate statistical analysis indicated significant correlations between our proxy records and historical data, especially with the mean annual temperature data from Stykkishólmur (Iceland) and the storis index (historical observations of sea-ice export via the East Greenland Current). In particular, the biological proxies (calcite weight percent, IP25, and total organic carbon %) showed significant linkage with the storis index. Our records show two distinct intervals in the recent history of the SE Greenland coast. The first of these (ad 1850-1910) shows predominantly perennial sea-ice conditions in the area, while the second (ad 1910-1990) shows more seasonally open water conditions.

High-resolution IP25 of three sediment cores in the western North Pacific and Bering Sea

Due to its strong influence on heat and moisture exchange between the ocean and the atmosphere, sea ice is an essential component of the global climate system. In the context of its alarming decrease in terms of concentration, thickness and duration, understanding the processes controlling sea-ice variability and reconstructing paleo-sea-ice extent in polar regions have become of great interest for the scientific community. In this study, for the first time, IP25, a recently developed biomarker sea-ice proxy, was used for a high-resolution reconstruction of the sea-ice extent and its variability in the western North Pacific and western Bering Sea during the past 18,000 years. To identify mechanisms controlling the sea-ice variability, IP25 data were associated with published sea-surface temperature as well as diatom and biogenic opal data. The results indicate that a seasonal sea-ice cover existed during cold periods (Heinrich Stadial 1 and Younger Dryas), whereas during warmer intervals (Bølling-Allerød and Holocene) reduced sea ice or ice-free conditions prevailed in the study area. The variability in sea-ice extent seems to be linked to climate anomalies and sea-level changes controlling the oceanographic circulation between the subarctic Pacific and the Bering Sea, especially the Alaskan Stream injection though the Aleutian passes.