Hiatal surfaces from the Miocene Globigerina Limestone Formation of Malta: Biostratigraphy, sedimentology, trace fossils and early diagenesis

The Miocene Globigerina Limestone of the Maltese islands contains widespread omission surfaces with very different characteristics and origins.The terminal Lower Globigerina Limestone hardground (TLGLHg) formed during a period of falling sea level. Coccolith assemblages suggest shallowness. Sedimentary structures and trace fossil assemblages, indicate increasing frequency of storm events and erosional episodes, towards the surface. Calcite cementation which took place around Thalassinoides burrows and formed irregular nodules was followed by dissolution of aragonite. It is suggested that lithification was linked to microbial reactions involving organic matter.In contrast two later surfaces, the terminal Middle Globigerina Limestone omissionground (TMGLOg), which marks the Lower to Middle Miocene boundary, and the Fomm-ir-Rih local hardground (FiRLHg) both contain early diagenetic dolomite. Lithification took place in two phases. The dolomite is interpreted to have formed beneath the sea floor; it was subsequently exhumed and partially corroded as the precipitation of calcitic and phosphatic cements took place around burrows open to the circulation of sea water.     

Les sépultures italiennes du Paléolithique supérieur. Reconstitutions du régime alimentaire

The identification of dietary habits is increasingly seen as a fundamental aspect for studying the ancient human populations. Accordingly, several projects aiming to identify Paleolithic individuals’ dietary patterns were developed to analyze the organic component of bone tissue and identify isotopic markers to reconstruct the food typology. Bone fragments from six individuals were selected for carbon and nitrogen stable isotopes analysis. The interpretation of human isotopic data was framed through a dataset of twenty-one Italian Paleolithic individuals. The isotopic data generated for the Paleolithic individuals agree with the information already provided by the archaeological record concerning the Italian hunter and gatherer communities. Their subsistence economy was essentially grounded upon the exploitation of high protein foods, either from terrestrial fauna resources or inland lacustrine or riverine species.     

Trophic structure of macro- and meso-invertebrates in Japanese coniferous forest: Carbon and nitrogen stable isotopes analyses

Few studies have been published on the feeding ecology of Japanese soil fauna based on stable isotope analysis. Therefore, the present work aims to use this technique for studying the trophic structure of Japanese soil fauna at two coniferous forests. Significant differences were observed between investigated sites (Arahama and Gamo) in genus richness and abundance, while for Shannon diversity indexes the difference was non-significant. The isotopic signatures (δ¹³C and δ¹⁵N) of the invertebrates collected at Arahama ranged from 0.3 to 6.3‰ for δ¹⁵N and from −27.3 to −23.3‰ for δ¹³C. At Gamo, invertebrates δ¹³C values ranged from −26.1 to −23.5‰ and δ¹⁵N values ranged from 1.6 to 6.8‰. At both sites, invertebrates formed two distinct groups on the basis of combined C and N stable isotope ratios. The locations of these groups related to δ¹³C values. The less enriched group (δ¹³C < −25‰) and the more enriched one (δ¹³C > −25‰). The range of δ¹⁵N for the present animals exceeded two trophic levels. While, the gradual ¹⁵N enrichment within the invertebrates species may indicate the dominance of omnivory in soil food webs. The differences between sites in δ¹⁵N confirm the importance of studying the trophic structure of soil fauna locally.     

Molluscs,isotopes and ecological fractionation: Examples from the upper Palaeogene of the Hampshire Basin

Carbon and oxygen isotopic analyses from upper Palaeogene molluscs collected in the Hampshire Basin (S. England) show that, in addition to long‐term trends in the data caused by climatic change, there is variation within samples collected from any one horizon. This variation is not attributable to diagenesis or other “noise”;. Linear trends in data from the meso‐ and oligohaline organisms are salinity‐dependent, as is a differentiation into clusters of the marine and brackish water animals. Within the marine organisms there is further distinction between taxa, controlled by micro‐environment. This is quite distinct from disequilibrium precipitation, as shell growth occurs in equilibrium with local isotopic ratios, though this may not necessarily be the same as contemporary mean ocean values. This “ecological fractionation”; can seriously affect the isotopic signal from a suite of fossils. Its existence should therefore be borne in mind when interpreting any biogenic isotope data from diverse taxa, localities, or micro‐habitats.     

辽宁北票喇嘛洞遗址出土人骨稳定同位素分析

喇嘛洞遗址是我国北方地区一处以三燕文化墓葬为主的大型墓地,对其出土人骨进行C和N稳定同位素分析,可望了解先民的食谱,揭示其生活方式进而探索鲜卑与汉的相互联系。该遗址20个墓葬出土人骨的C、N含量以及C/N摩尔比反映了样品均保存较好,可用作食谱分析。人骨中骨胶原δ13C和δ15N分析显示,先民主要以C4类食物为食,且基本为素食,这当与发达的糜子和粟米农业密切相关,表明喇嘛洞遗址鲜卑生活方式已受到汉文化的强烈影响,由游猎为生转变为农业生产为主。对不同性别的先民食谱差异性进行t检验,发现男女食谱上不存在显著差异。样品BLM63和BLM99的δ15N值相对较高,揭示了其食物结构中含有一定量的肉类。     

Fine-fraction carbonate stable isotopes as indicators of seasonal shallow mixed-layer paleohydrography

We have measured stable isotopic compositions of Miocene pelagic fine-fraction (<63 μm) carbonates from oligotrophic deep-sea sites in the Pacific and Atlantic oceans and compared them with those of coexisting foraminifers to test their utility as near sea-surface indicators. Fine-fraction carbonates (primarily polyspecific nannofossils) and surface-dwelling planktic foraminiferal (Globigerinoides) stable isotopes both have been considered to reflect surface-water hydrographic conditions. However, our results indicate that fine-fraction stable isotopes are offset from and do not correlate well with those of Globigerinoides. In contrast, stable isotopic records of the deep-dwelling planktic foraminifer Globoquadrina are in good correspondence with the fine-fraction records in terms of long-term (ca. >1 m.y.) trends and temporal variability. On the basis of a time-series hydrography and flux study site in the oligotrophic subtropical North Atlantic, we interpret the isotopic discrepancies between fine-fraction and Globigerinoides as resulting primarily from season of calcification, as well as possible vital effects. We suggest that fine-fraction stable isotope values from oligotrophic waters reflect late winter–early spring relatively cool, nutrient-rich shallow mixed-layer conditions during the time of deep mixing (i.e., spring bloom), whereas Globigerinoides stable isotope values record conditions that prevailed in the stratified surface waters in the warmer late spring–fall. This implies that paired analyses of fine-fraction and surface-dwelling planktic foraminiferal δ¹⁸O could be applied to reconstruct paleoseasonality of the open oceans. However, because the fine-fraction δ¹³C values are not representative of the annual mean surface-water δ¹³C, we recommend use of near surface-dwelling planktic foraminiferal δ¹³C as a proxy for δ¹³C of stratified surface waters that are more or less in equilibrium with the atmosphere with respect to pCO₂.     

Variability of stable isotope signatures (δC and δN) in two spider crab populations (Maja brachydactyla) in Western Europe

The ontogenic variations of nitrogen and carbon stable isotopic signatures (δ¹⁵N and δ¹³C) were investigated in two spider crab (Maja brachydactyla) populations inhabiting in different biotopes of Western Europe. The Iroise Sea population is localized in Western Brittany and characterized by a seasonal migration occurring on a large bathymetric and habitat gradient while the Seine Bay population, in the Eastern English Channel, remains in a more homogeneous environment during its migration. In the Iroise Sea population, δ¹³C values increased significantly both with body size and age, revealing a shift towards “benthic-component” prey with spider crab growth. On the contrary, neither body size nor ageing gave rise to a significant trophic level change (derived from the δ¹⁵N). In this M. brachydactyla population, the seasonal migrations from coastal waters in summer to offshore habitats in winter involved significant but slight differences in both δ¹³C and δ¹⁵N. In the Seine Bay population, low variations for both carbon and nitrogen were recorded related to either sex or size or seasonal migration. Thus, the δ¹³C and δ¹⁵N variability in the spider crab depends on the availability and diversity of prey in its different living habitats, as well as on the morphological aptitudes of individuals to feed on prey (individual's size).     

Sources and fates of dissolved organic carbon in lakes as determined by whole-lake carbon isotope additions

Four whole-lake inorganic ¹³C addition experiments were conducted in lakes of differing trophic status. Inorganic ¹³C addition enriched algal carbon in ¹³C and changed the C-DOC by +1.5‰ to +9.5‰, depending on the specific lake. This change in C-DOC represented a significant input of algal DOC that was not completely consumed by bacteria. We modeled the dynamics in C-DOC to estimate the fluxes of algal and terrestrial carbon to and from the DOC pool, and determine the composition of the standing stock. Two experiments in lightly stained, oligotrophic lakes indicated that algal production was the source of about 20% of the DOC pool. In the following year, the experiment was repeated in one of these lakes under conditions of nutrient enrichment, and in a third, more humic lake. Algal contributions to the DOC pool were 40% in the nutrient enriched lake and 5% in the more humic lake. Spectroscopic and elemental analyses corroborated the presence of increased algal DOC in the nutrient enriched lake. Natural abundance measurements of the C of DOC in 32 lakes also revealed the dual contributions of both terrestrial and algal carbon to DOC. From these results, we suggest an approach for inferring the contribution of algal and terrestrial DOC using easily measurable parameters.     

宁夏盐池不同坡位旱地紫苜蓿水分来源

紫苜蓿(Medicago sativa)是一种经济和生态价值较高的优良牧草, 但其耗水量大, 在西北半干旱地区仅靠天然降水难以满足紫苜蓿的正常生长发育。宁夏盐池北部地处毛乌素沙地南缘, 地下水埋深较浅, 地下水有可能成为紫苜蓿的潜在水源, 弥补天然降水的不足。本试验在地势平坦的缓坡丘陵梁地和丘间低地, 选择8年生旱地紫苜蓿试验地作为研究对象, 采用稳定同位素技术, 研究了不同海拔的4个坡位(海拔自低到高分别为: 坡1、坡2、坡3和坡4)紫苜蓿的水分来源及其生长生理表现。结果表明: 坡位对0-300 cm土壤剖面含水量有显著影响, 海拔最低的坡1土壤含水量最高。土壤水和植物茎秆水δ ¹⁸O-δD坐标点大部分位于中国西北地区地方大气降水线(LMWL)的右侧, 说明植物利用的水源氢氧同位素组成受到蒸发的影响而发生了富集作用。0-450 cm土壤剖面水δ ¹⁸O值随着海拔高度的增加而增大。同一坡位土壤水δ ¹⁸O值随着土壤深度的增加逐渐下降。深层土壤水δ ¹⁸O值与地下水δ ¹⁸O相近, 说明地下水通过土壤毛细管上升而补充其上层土壤水分。0-40 cm土壤水δ ¹⁸O值随季节波动较大, 270 cm以下土壤水δ ¹⁸O值较为稳定。4、7、8月份坡1紫苜蓿茎秆水δ ¹⁸O值显著低于其他3个坡位(p < 0.001)。在4、6、7三个月, 坡位1紫苜蓿对深层土壤水(270 cm以下)的利用率最高。而在8月份, 坡1、坡3、坡4紫苜蓿主要利用150-270 cm、270-450 cm土层土壤水以及地下水, 坡2对表层(0-20 cm)土壤水利用率最高。坡1紫苜蓿的产量、整株Δ ¹³C值及气孔导度显著高于其他3个坡位。本研究表明: 在平均年降水量只有280 mm的西北半干旱地区种植旱地紫苜蓿要尽量选择地势较低的滩地, 使其能够利用到埋深较浅地下水, 以满足植物生长发育的需要并取得较好的生态和经济效益。     

Isotopic ecology and dietary profiles of Liberian chimpanzees

An extensive suite of isotopic data (δ¹³C, δ¹⁵N, and δ¹⁸O) from enamel apatite and bone collagen of adult male and female wild chimpanzees establishes baseline values for Pan troglodytes verus in a primary rainforest setting. The Ganta chimpanzee sample derives from a restricted region in northern Liberia. Diet is examined using stable light isotopes at three life stages—infant, young juvenile, and adult—and developmental differences are investigated within and between individual males and females. The isotopic data are very homogeneous with few exceptions. Juvenile females show consistent enrichment in ¹³C relative to infants, while juvenile males do not. These data suggest that age at weaning may be more variable for male offspring who survive to adulthood than for female offspring. Alternatively, or additionally, the weaning diet of males and females may differ, with greater consumption of technologically extracted insects and/or nuts by young females. Metabolic differences, including growth and hormone-mediated responses, may also contribute to the observed variation.The Ganta chimpanzee data offer an independent and objective line of evidence to primatologists interested in the dietary strategies of the great apes and to paleoanthropologists seeking comparative models for reconstructing early hominin subsistence patterns. Despite the high diversity of dietary items consumed by chimpanzees, isotopic signatures of chimpanzees from a primary rainforest setting exhibit narrow ranges of variation similar to chimpanzees in more open habitats.     

秦岭南麓3种典型植物水分利用来源及水文生态位特征

水分是限制植物生长的关键因子,植物的水分利用来源反映了植被对环境变化响应的生态水文过程,成为植被建设重要关注点之一,然而当前关于秦岭地区典型植物的水分利用模式尚不明晰。以秦岭主要造林树种锐齿栎(Quercus aliena var. acutiserrata)、麻栎(Quercus acutissima Carr.)和马尾松(Pinus massoniana Lamb)为对象,通过测定降雨、土壤水和植物木质部水中δ²H和δ¹⁸O的同位素,借助MixSIAR模型定量分析植物的水分利用特征,并应用Levins指数和相似性比例指数(PS指数)计算水分生态位宽度和重叠度。结果表明:不同树种在同时期的水分来源不同,同一树种在降雨前后水分来源也有别。降雨前锐齿栎主要利用20-40 cm土壤水(42.9%),雨后则逐步转移到浅层0-20 cm土层(56.3%-58.2%);麻栎雨前主要利用深层40-60 cm土壤水(45.3%),雨后逐渐转移为浅层,且随着降雨量的增加,浅层水源利用比例增大(40%增加到58.7%)。马尾松在降雨前和小雨事件后的水分利用来源变化不明显,而发生大雨(259 mm)之后,对浅层0-20 cm的水分利用由38%增加到91.1%。锐齿栎-麻栎林的PS指数为77.3%,二者间水分竞争较弱,而锐齿栎-马尾松林、麻栎-马尾松林之间存在明显的水分竞争关系(PS指数在80%以上)。结论:锐齿栎-麻栎混交林是比较适宜的搭配树种,二者对同一土层水分竞争相对较弱。而麻栎和马尾松在降雨前后的水分利用策略相似,表现出明显的水分竞争关系。因此,在未来植被建设中,建议选择合理的树种配置,以实现森林的可持续管理。     

Influence of sunflecks on the δ 13 C of Adenocaulon bicolor plants occurring in contrasting forest understory microsites

Summary Xylem-tapping mistletoe species growing on Mimosaccae, non-Mimosaceae and hosts performing Crassulacean acid metabolism (CAM) were studied along an aridity gradient in the Namib desert. °¹³C-values of mistletoes became more negative with decreasing nitrogen (N)-concentration in their leaves, while the host plants showed no such relationship. This might suggest that mistletoes regulate their water use efficiency according to the nitrogen supply from the host. However, further inspection of the data indicates that the relations of ¹³C-values with leaf nitrogen in mistletoes may result from carbon input from the host. This is especially true for mistletoes growing on CAM plants which exhibit a very high ¹³C-value, but show no evidence of CAM. It is calculated that about 60% of the carbon in mistletoes growing on C3 and on CAM hosts originated from the host. The hypothesis of Marshall and Ehleringer (1990) that xylem tapping mistletoes are also carbon parasites could explain the change in ¹³C-values with N-supply and the difference in ¹³C-values between mistletoes growing on C3 and CAM hosts.This paper is prepared in memory of J. Visser, who joined the collection and identification of species in 1987, but died in 1990