Southern California's megaflood event of ca. 1605 AD linked to large-scale atmospheric forcing

A distinct, 1- to 2-cm-thick flood deposit found in Santa Barbara Basin with a varve-date of 1605 AD ± 5 years testifies to an intensity of precipitation that remains unmatched for later periods when historical or instrumental records can be compared against the varve record. The 1605 AD ± 5 event correlates well with Enzel's (1992) finding of a Silver Lake playa perennial lake at the terminus of the Mojave River (carbon-14-dated 1560 AD ± 90 years), in relative proximity to the rainfall catchment area draining into Santa Barbara Basin. According to Enzel, such a persistent flooding of the Silver Lake playa occurred only once during the last 3,500 years and required a sequence of floods, each comparable in magnitude to the largest floods in the modern record. To gain confidence in dating of the 1605 AD ± 5 event, we compare Southern California's sedimentary evidence against historical reports and multi-proxy time-series that indicate unusual climatic events or are sensitive to changes in large-scale atmospheric circulation patterns. The emerging pattern supports previous suggestions that the first decade of the 17th century was marked by a rapid cooling of the Northern Hemisphere, with some indications for global coverage. A burst of volcanism and the occurrence of El Nino seem to have contributed to the severity of the events. The synopsis of the 1605 AD ± 5 years flood deposit in Santa Barbara Basin, the substantial freshwater body at Silver Lake playa, and much additional paleoclimatic, global evidence testifies for an equatorward shift of global wind patterns as the world experienced an interval of rapid, intense, and widespread cooling.

真菌诱导子对青蒿发根生长和青蒿素生物合成的影响及开花与青蒿素生物合成的相关性研究

本论文主要包括以下两部分内容： 一、真菌诱导子对青蒿发根生长和青蒿素生物合成的影响 用3种真菌诱导子[大丽花轮枝孢（Verticillium dahliae Kleb.）、葡枝根霉(Rhizopus stolonifer (Ehrenb. ex Fr.) Vuill)和束状刺盘孢(Colleto trichumdematium (Pers.) Grove)]分别处理青蒿(Ar temisia annuaL．)的发根，这3种真菌诱导子均能促进发根中青蒿素的合成，其中以大丽花轮枝孢的诱导效果最好;对细胞生长均没有明显影响。经大丽花轮枝孢处理的发根中青蒿素含量达1. 12 mg/gDW，比对照(0. 77 mg/g DW)提高45%。诱导子的作用效果与诱导子浓度、诱导子作用时间及发根的生长状态有关。对大丽花轮枝孢来说，诱导子作用的最适浓度为每毫升培养基含糖0.4 mg;发根在指数生长末期对诱导作用最敏感：在加入诱导子4d后收获发根，发根中的青蒿素含量最高。 二、早花基因FPF1、co对青蒿开花时间的影响及开花与青蒿素生物合成的相关性 1．将来源于拟南芥的早花基因Flowering Promoting Factorl (FPFl)插入到植物表达载体pBI121中，构建CaMV 35S启动子控制下含FPFl基因的植物表达载体pBI121FPF/，用含有pBI121FPF/质粒的根癌农杆菌(Agrobacterium tumefaciens)LBA4404感染青蒿(Artemisia annua L.)叶片并诱导丛生芽，经卡那霉素筛选，获得转基因抗性植株。PCR、 PCR-Southem blot及Southern blot检测表明，外源基因FPFI已整合到青蒿基因组中：RT-PCR及RT-PCR Southern blot分析表明，外源基因在转录水平上已有表达。在短日照条件下，FPF1转基因植株的开花时间较对照提前20天左右，但提早开花的转基因植株与未开花的对照其青蒿素含量无明显差异，即提早开花并不能使开花植株的青蒿素含量有所提高，开花与青蒿素合成之间可能没有直接的关系。 2．将拟南芥的早花基因CONSTANS (CO)置于CaMV 35S启动子之下，通过根癌农杆菌(Agrobacterium tumefaciens)LBA4404介导转入青蒿(Artemisia annuaL．)，使之在青蒿中表达，并得到了抗性植株。PCR、PCR-Southem blot及Southemblot检测表明，外源基因co已整合到青蒿基因组中;RT-PCR及RT-PCR Southemblot分析表明，外源基因在转录水平上已有表达。在短日照条件下，co转基因植株的开花时间较对照提前2周左右，但提早开花的转基因植株的青蒿素含量与未丌花的对照无明显差异，即植株开花前青蒿素含量的提高并不是由于开花本身引起的，再次证明，开花与青蒿素合成之间可能没有直接的关系。

Biology and feeding behavior of Orbinia johnsoni

Orbinia johnsoni were studied from a small sandy beach near Mussel Pt., Pacific Grove, California, where they are most abundant at low tide levels in fine sand. They were found to have a mean length of 190 mm. The orbiniids were found with their guts the fullest during incoming to high tides. It is plausible that this is when they are feeding. It takes about 3 to 3.5 hours for food to travel through the length fo the gut. The orbiniids eat 93 percent sand and seven percent organic detritus. Special note should be taken that some food selectivity appears to be involved and that high percentages of organic matter in the feces are found in worms collected during low, outgoing tides. Evidence suggests that the worms are bottom feeders, not coming to the surface to feed.

A modern pollen record from the central Gulf of California

As one facet of an effort to tie the pollen record of central Gulf of California deep cores to modern analogs, pollen was analyzed in the uppermost 150-200 years of varved core 7807-1410 taken nearby. Sampling at 2- to 8-year resolution yielded a noncomplacent record, suggesting pollen in these sediments may be a potential high resolution proxy record of short-term climatic events. The pollen spectrum as a whole matches that of upper-most DSDP Site 480 (means of all samples). Lack of a ratio or influx shift following damming of local rivers and a surplus of low-spine Compositae pollen relative to mainland sites support Baumgartner's theory that terrigenous influx to the site is largely aeolian and also suggest that a significant fraction of the pollen influx may come from Baja California.

Introduction

In 1984, a workshop was held on "climatic variability of the eastern North Pacific and western North America." From it has emerged an annual series of workshops held each spring at the Asilomar Conference Center, Monterey Peninsula, California. These annual gatherings have come to be called PACLIM (Pacific Climate) Workshops, reflecting broad interests in the climatologies associated with the Pacific Ocean. Participants in the six workshops that have convened since 1984 have included atmospheric scientists, hydrologists, geologists, glaciologists, oceanographers, limnologists, and both marine and terrestrial biologists.

Introduction

The 1992 PACLIM meeting featured the Long-Term Ecological Research (LTER) program, sponsored by the National Science Foundation. Ranging from hot to cold and wet to dry climatic regimes, these 18 sites are attempting to understand the web of relationships in different locations as communities evolve over time scales of years to decades to centuries. During this time they are subject to external forcings, including those that vary smoothly and somewhat predictably, like the seasons, upon which are superimposed random "shocks" of various magnitudes.

Spawning behavior and larval development in Mopalia lignosa and Mopalia muscosa (Mollusca: Polyplacophora) in central California

Spawning behavior and external features of the larval development were studied in the chitons Mopalia muscosa and M. lignosa during the months of April-June, 1974, at Pacific Grove, California. ... The sequence of events in the development of the two species in the same, though some differences in timing exist.

Atmospheric carbon dioxide and the climatic record

This paper is an attempt to provide a summary review of conclusions from previous studies on this subject. They have been organized under the following subject headings: Conceptualization of the greenhouse effect; The climatic effect of doubled carbon dioxide; Interpretation of the climatic record; Diagnosis of apparent and possible model deficiencies; The paleoclimatic record.

The annual course of precipitation over much of the United States: observed versus GCM simulation

General Circulation Models (GCMs) may be useful in estimating the ecological impacts of global climatic change. We analyzed seasonal weather patterns over the conterminous United States and determined that regional patterns of rainfall seasonality appear to control the distributions of the Nation's major biomes. These regional patterns were compared to the output from three GCMs for validation. The models appear to simulate the appropriate seasonal climates in the northern tier of states. However, the spatial extent of these regions is distorted. None of the models accurately portrayed rainfall seasonalities in the southern tier of states, where biomes are primarily influenced by the Bermuda High.

A statistical model of climates in the southwestern United States

EXTRACT (SEE PDF FOR FULL ABSTRACT): We describe an empirical-statistical model of climates of the southwestern United States. Boundary conditions include sea surface temperatures, atmospheric transmissivity, and topography. Independent variables are derived from the boundary conditions along 1000-km paths of atmospheric circulation. ... Predictor equations are derived over a larger region than the application area to allow for the increased range of paleoclimate. This larger region is delimited by the autocorrelation properties of climatic data.

Climate signals in the lower stratosphere and upper troposphere

Empirical orthogonal function (EOF) analysis and regression analysis are used to investigate zonally averaged seasonal temperature anomaly patterns and trends in the lower stratosphere and upper troposphere. The first four EOFs explain 64 percent of the temperature variance and can be related, respectively, to the solar flux (SF) and El Niño/Southern Oscillation (ENSO), to the quasi-biennial oscillation (QBO), to atmospheric carbon dioxide (CO2) and turbidity (TB), and to ENSO. The signal of the fourth EOF is modulated in January to March by the solar flux, with the sense of the modulation determined by the phase of the quasi-biennial oscillation.

1988 summer drought over the Great Plains: some causes and predictions

EXTRACT (SEE PDF FOR FULL ABSTRACT): The 1988 summer drought over much of the United States is described in terms of hemispheric mid-tropospheric flow patterns, temperature and precipitation anomalies, and sea surface temperature patterns. This drought was similar to earlier Great Plains droughts, although spatially more extensive than most. Three attempts to predict this drought from antecedent spring were moderately successful, though no one anticipated its severity and extent. ... A modified barotropic model iterating from a mean summer estimate of seasonal forcing from the May mid-tropospheric height pattern was reasonably successful in forecasting the drought. Sea surface temperature indications show that cold water (La Niña) along the equator subsequent to the 1987 El Niño, while contributory, cannot be considered a principal cause of the drought, since earlier cold water episodes did not produce drought, and other drought episodes occurred in the absence of cold equatorial waters.

Current water supply conditions in California

This paper contains a brief report on the status of the California water supply situation on March 1, 1989, including a review of the antecedent conditions of the past two dry water years.

Uncovering North American temperature and precipitation patterns associated with the Southern Oscillation

The extreme phases of the Southern Oscillation (SO) have been linked to fairly persistent classes of circulation anomalies over the North Pacific and parts of North America. It has been more difficult to uncover correspondingly consistent patterns of surface temperature and precipitation over much of the continent. The few regions that appear to have consistent SO-related patterns of temperature and precipitation anomalies are identified and discussed. Also discussed are regions that appear to have strong SO-related surface anomalies whose sign varies from episode to episode.