Proteolysis: anytime, any place, anywhere?

Proteolysis via the ubiquitin-proteasome system (UPS) is a rapid and effective method of degrading a specific protein at a specific time, and in many cases a protein is degraded only in response to a particular cellular signal or event. However, an added dimension to the control of protein degradation is possible because the ubiquitin system can be spatially regulated. Controlling where a protein is degraded can enhance the specificity and timing of proteolysis, generate asymmetry and maintain sub-compartments even in the mitotic cell. Here, we discuss this aspect of the UPS.     

Teleology: yesterday,today, and tomorrow?

Teleological explanations in evolutionary biology, from Cuvier to the present (and into the future), depend on the metaphor of design for heuristic power and predictive fertility.     

Hypocretins: waking, arousal, or action?

The role of hypocretin (orexin) neurotransmission in waking and arousal, though of intense interest, is poorly understood. In this issue of Neuron, demonstrate that, in general, hypocretin neurons are minimally active during both sleep and quiet waking. In contrast, these neurons display robust activity during periods of alert and/or active waking.     

Homo floresiensis: microcephalic, pygmoid, Australopithecus, or Homo?

The remarkable partial adult skeleton (LB1) excavated from Liang Bua cave on the island of Flores, Indonesia, has been attributed to a new species, Homo floresiensis, based upon a unique mosaic of primitive and derived features compared to any other hominin. The announcement precipitated widespread interest, and attention quickly focused on its possible affinities. LB1 is a small-bodied hominin with an endocranial volume of 380-410 cm3, a stature of 1m, and an approximate geological age of 18,000 years. The describers [Brown, P., Sutikna, T., Morwood, M.J., Soejono, R.P., Jatmiko, Wayhu Saptomo, E., Awe Due, R., 2004. A new small-bodied hominin from the Late Pleistocene of Flores, Indonesia. Nature 431, 1055-1061] originally proposed that H. floresiensis was the end product of a long period of isolation of H. erectus or early Homo on a small island, a process known as insular dwarfism. More recently Morwood, Brown, and colleagues [Morwood, M.J., Brown, P., Jatmiko, Sutikna, T., Wahyu Saptomo, E., Westaway, K.E., Awe Due, R., Roberts, R.G., Maeda, T., Wasisto, S., Djubiantono, T., 2005. Further evidence for small-bodied hominins from the Late Pleistocene of Flores, Indonesia. Nature 437, 1012-1017] reviewed this assessment in light of new material from the site and concluded that H. floresiensis is not likely to be descended from H. erectus, with the genealogy of the species remaining uncertain. Other interpretations, namely that LB1 is a pygmy or afflicted with microcephaly, have also been put forward. We explore the affinities of LB1 using cranial and postcranial metric and non-metric analyses. LB1 is compared to early Homo, two microcephalic humans, a 'pygmoid' excavated from another cave on Flores, H. sapiens (including African pygmies and Andaman Islanders), Australopithecus, and Paranthropus. Based on these comparisons, we conclude that it is unlikely that LB1 is a microcephalic human, and it cannot be attributed to any known species. Its attribution to a new species, Homo floresiensis, is supported.     

Cell death: programmed, apoptosis, necrosis, or other?

There are at least two major types of active or physiological cell death. The most well-known form, apoptosis or Type I, involves early nuclear collapse, condensation of chromatin, generation of nucleosomal ladders, and cell fragmentation with little or no early alteration of lysosomes. It is most commonly seen in cells deriving from highly mitotic lines, and the cells are phagocytosed by neighboring cells or infiltrating macrophages. In metamorphosing or secretory cells, and under conditions where the majority of cells die, the bulk of the cytoplasm is consumed by expansion of the lysosomal system well before nuclear collapse is manifest. This form of cell death has been termed Type II cell death, and we revert to this terminology. The requirement for protein synthesis is more characteristic of Type II cell death in developmental situations than it is for Type I cell death. The variations seen force a reassessment of those aspects of physiological cell death that are truly universal, thereby focusing attention on the biology of the process. A better understanding of the biology and morphology of dying cells will help clarify the significance of the molecular and biochemical findings.     

Margaret C. Etter (Wilmington,DE: September 12, 1943 – Minneapolis,MN: June 10, 1992)

In Memoriam

Margaret C. Etter (Wilmington, DE: September 12, 1943 – Minneapolis, MN: June 10, 1992)     

Schistosome monogamy: who,how, and why?

Schistosomes represent a unique animal model for comparative analyses of monogamy. Indeed, schistosomes are classified at the lowest taxonomical level of monogamous species and lack complex social interactions, which could alter our understanding of their unusual mating system. Elements discussed here include the fact that monogamy in schistosomes could be an ancestral state between hermaphroditism and polygyny or polygynandry and the occurrence of mate changes. In addition, hypotheses are proposed to explain monogamy in schistosomes (e.g. female dispersion, the need for paternal care, oviposition site limitation or aggressiveness, and mate guarding). We also propose future experimental and analytical approaches to improve our understanding of the schistosomes' mating system.     

Plant species radiations: where,when, why?

The spatial and temporal patterns of plant species radiations are largely unknown. I used a nonlinear regression to estimate speciation and extinction rates from all relevant dated clades. Both are surprisingly high. A high species richness can be the result of either little extinction, thus preserving the diversity that dates from older radiations (a 'mature radiation'), or a 'recent and rapid radiation'. The analysis of radiations from different regions (Andes, New Zealand, Australia, southwest Africa, tropics and Eurasia) revealed that the diversity of Australia may be largely the result of mature radiations. This is in sharp contrast to New Zealand, where the flora appears to be largely the result of recent and rapid radiations. Mature radiations are characteristic of regions that have been climatically and geologically stable throughout the Neogene, whereas recent and rapid radiations are more typical of younger (Pliocene) environments. The hyperdiverse Cape and Neotropical floras are the result of the combinations of mature as well as recent and rapid radiations. Both the areas contain stable environments (the Amazon basin and the Cape Fold Mountains) as well as dynamic landscapes (the Andes and the South African west coast). The evolution of diversity can only be understood in the context of the local environment.     

气候变化科学:适应,减缓,还是漠视?

气候变化是真实的,并且与增加的温室气体排放密切相关。有记载以来,地球上最热的十年出现在1 991年之后,上个世纪,气温大概升高了0 .6℃[1 ]。在同一时期,全球的海平面大约上升了2 0 cm,其中部分来自于陆地冰的融化,部分来自于海洋的受热膨胀。许多山顶上覆盖的冰冠也正在消失[2 ,3] ,数十年来,北极地区夏季及秋季的海冰已经减少为原来的4 0 % ,尽管其已有稳定的趋势[4 ,5] 。在英国,为防止伦敦被泰晤士河的洪水淹没,泰晤士河防洪措施的使用次数,已经由2 0世纪80年代的每年不到1图1　泰晤士河防洪措施的使用次数次增加至年均6次以上(图1 ) […