The life history of the tropical shad Tenualosa toli from Sarawak: first evidence of protandry in the Clupeiformes?

Synopsis Sharp declines in catches prompted a detailed study of the commercially and culturally important terubok Tenualosa toli, which lives in the fast-flowing, turbid estuaries and adjacent shallow coastal waters of Sarawak. Its reproduction, diet, age and growth were investigated. An absence of small females and large males, together with histological data showing transitional gonads, suggest that T. toli is a protandrous hermaphrodite. Ageing based on otoliths indicates that individuals may not live more than about two years. Male fish spawn towards the end of their first year, change sex (transitional gonads were recorded in fish from 14 to 31 cm SL) and spawn as females in their second year. Spawning takes place in the middle reaches of estuaries and females deposit all their eggs at once. Fecundity is linearly related to fish length but shows significant seasonal and site variations. Hermaphroditism is discussed in relation to possible environmental and isolating mechanisms. T. toli is a zooplanktivore eating mainly calanoid copepods. Laser-ablation inductively-coupled plasma mass spectroscopy of trace elements across otoliths revealed that the species does not move into full seawater or freshwater, but completes its life cycle in estuarine and adjacent coastal waters. Therefore T. toli populations in each estuary and adjacent coastal waters may be relatively isolated from one another, and hence particularly susceptible to overfishing.     

The origin of life and the left-handed amino-acid excess: the furthest heavens and the deepest seas?

The origin of life is an extraordinary problem that leads back to the structure and dynamics of the cosmos and early development of organic molecules. Within that wider question lies an unsolved problem that has troubled biologists for 150 years. What is the origin of the dominant presence of left-handed stereoisomers of amino acids in nature even though their synthesis normally results in an equal mixture of the right- and left-handed molecular forms? We propose that asymmetric Earth rotation caused at dawn and dusk circularly polarized UV light (CPUVL) of opposite polarity and reversed temperature profiles in the oceans. Destruction of the d-isomer by CPUVL at dusk in a sea surface hotter than at dawn created a daily l-isomer excess protected from radiation by nightfall, preserved by down-flow (diffusive, mechanical) into cold, darker regions, eventually initiating an l-amino-acid excess embodied in early marine forms. Innumerable mechanisms have been proposed for the origin of l-chiral dominance in amino acids and none proven. Since the thalidomide tragedy, homochirality of amino acids has been a growing practical issue for medicine. Understanding its origin may bring further and unexpected benefits. It may also be a modest pointer to the possibility of positive answers to whether intelligent life will have the capacity to continue to protect itself from conditions inimical to survival.     

The origin of interlocus sexual conflict: is sex‐linkage important?

Sexual conflict has been proposed as a potential selective agent in the evolution of a variety of traits. Here, we present a simple model that investigates the initial conditions under which sex-linked and sex-limited harming alleles can invade a population. In this paper, we expand previous threshold models to study how sex-linkage and sex determination mechanisms affect the spreading conditions of a harming allele. Our models provide new insights into how sexual conflict could originate, showing that in diploid organisms the probability of a new harming allele spreading is independent of both the genetic sex determination system and the dominance relationships. However, the incidence of interlocus sexual conflicts in the initial steps of the invasion critically depends on the inheritance system.     

The origin of the Hominidae: Africa or Asia?

The authors review the evidence for the evolution of the apes and their geographical expansion out of Africa during the Miocene. The ecological background is discussed at each period.From this it is concluded that Dryopithecines in either Africa or Eurasia could have given rise to early Hominidae and that the ecological conditions in both continents were suitable for the appearance of Hominid adaptations.The evidence for early Hominids is at present more impressive in Eurasia than in Africa, though the African find from Fort Ternan, Kenya, is the earliest. On present evidence, neither continent can be precluded as the place of origin of the Hominidae and it appears to be a possibility that Hominidae evolved in both continents with intermittent gene exchange.     

Immunology: the origin of sweetbreads in lampreys?

The thymus is required for the differentiation of T lymphocytes. A new study in lampreys indicates that the pharyngeal epithelium of the gill basket supports the development of T-like cells, suggesting the existence of a primitive thymus in these oldest of vertebrates.     

The shape of things to come in the study of the origin of species?

Perhaps Darwin would agree that speciation is no longer the mystery of mysteries that it used to be. It is now generally accepted that evolution by natural selection can contribute to ecological adaptation, resulting in the evolution of reproductive barriers and, hence, to the evolution of new species (Schluter & Conte 2009 ; Meyer 2011 ; Nosil 2012 ). From genes that encode silencing proteins that cause infertility in hybrid mice (Mihola et al. 2009 ), to segregation distorters linked to speciation in fruit flies (Phadnis & Orr 2009 ), or pollinator‐mediated selection on flower colour alleles driving reinforcement in Texan wildflowers (Hopkins & Rausher 2012 ), characterization of the genes that drive speciation is providing clues to the origin of species (Nosil & Schluter 2011 ). It is becoming apparent that, while recent work continues to overturn historical ideas about sympatric speciation (e.g. Barluenga et al. 2006 ), ecological circumstances strongly influence patterns of genomic divergence, and ultimately the establishment of reproductive isolation when gene flow is present (Elmer & Meyer 2011 ). Less clear, however, are the genetic mechanisms that cause speciation, particularly when ongoing gene flow is occurring. Now, in this issue, Franchini et al. ( 2014 ) employ a classic genetic mapping approach augmented with new genomic tools to elucidate the genomic architecture of ecologically divergent body shapes in a pair of sympatric crater lake cichlid fishes. From over 450 segregating SNPs in an F2 cross, 72 SNPs were linked to 11 QTL associated with external morphology measured by means of traditional and geometric morphometrics. Annotation of two highly supported QTL further pointed to genes that might contribute to ecological divergence in body shape in Midas cichlids, overall supporting the hypothesis that genomic regions of large phenotypic effect may be contributing to early‐stage divergence in Midas cichlids.     

The terrestrial evolution of metabolism and life – by the numbers

Background  

Allometric scaling relating body mass to metabolic rate by an exponent of the former (Kleiber's Law), commonly known as quarter-power scaling (QPS), is controversial for claims made on its behalf, especially that of its universality for all life. As originally formulated, Kleiber was based upon the study of heat; metabolic rate is quantified in watts (or calories per unit time). Techniques and technology for metabolic energy measurement have been refined but the math has not. QPS is susceptible to increasing deviations from theoretical predictions to data, suggesting that there is no single, universal exponent relevant to all of life. QPS's major proponents continue to fail to make good on hints of the power of the equation for understanding aging.     

The origin of the pelagobenthic metazoan life cycle: what's sex got to do with it?

The biphasic (pelagobenthic) life cycle is found throughoutthe animal kingdom, and includes gametogenesis, embryogenesis,and metamorphosis. From a tangled web of hypotheses on the originand evolution of the metazoan pelagobenthic life cycle, currentopinion appears to favor a simple, larval-like holopelagic ancestorthat independently settled multiple times to incorporate a benthicphase into the life cycle. This hypothesis derives originallyfrom Haeckel's (1874) Gastraea theory of ontogeny recapitulatingphylogeny, in which the gastrula is viewed as the recapitulationof a gastraean ancestor that evolved via selection on a simple,planktonic hollow ball of cells to develop the capacity to feed.Here, we propose an equally plausible hypothesis that the originof the metazoan pelagobenthic life cycle was a direct consequenceof sexual reproduction in a likely holobenthic ancestor. Indoing so, we take into account new insights from poriferan developmentand from molecular phylogenies. In this scenario, the gastruladoes not represent a recapitulation, but simply an embryologicalstage that is an outcome of sexual reproduction. The embryocan itself be considered as the precursor to a biphasic lifestyle,with the embryo representing one phase and the adult anotherphase. This hypothesis is more parsimonious because it precludesthe need for multiple, independent origins of the benthic form.It is then reasonable to consider that multilayered, ciliatedembryos ultimately released into the water column are subjectto natural selection for dispersal/longevity/feeding that setsthem on the evolutionary trajectory towards the crown metazoanplanktonic larvae. These new insights from poriferan developmentthus clearly support the intercalation hypothesis of bilaterianlarval evolution, which we now believe should be extended todiscussions of the origin of biphasy in the metazoan last commonancestor.     

Is biofilm formation intrinsic to the origin of life?

Biofilms are multicellular, often surface-associated, communities of autonomous cells. Their formation is the natural mode of growth of up to 80% of microorganisms living on this planet. Biofilms refractory towards antimicrobial agents and the actions of the immune system due to their tolerance against multiple environmental stresses. But how did biofilm formation arise? Here, I argue that the biofilm lifestyle has its foundation already in the fundamental, surface-triggered chemical reactions and energy preserving mechanisms that enabled the development of life on earth. Subsequently, prototypical biofilm formation has evolved and diversified concomitantly in composition, cell morphology and regulation with the expansion of prokaryotic organisms and their radiation by occupation of diverse ecological niches. This ancient origin of biofilm formation thus mirrors the harnessing environmental conditions that have been the rule rather than the exception in microbial life. The subsequent emergence of the association of microbes, including recent human pathogens, with higher organisms can be considered as the entry into a nutritional and largely stress-protecting heaven. Nevertheless, basic mechanisms of biofilm formation have surprisingly been conserved and refunctionalized to promote sustained survival in new environments.     

Possible origin of life between mica sheets: does life imitate mica?

The mica hypothesis for the origin of life proposes that life originated between the sheets of muscovite mica. This paper elaborates on two ways that life resembles what might have originated between mica sheets. First, enzymes: The configurations and dynamics of enzymes, with their substrates, cofactors, and sometimes transition metal ions, often resemble mica sheets, with their open-and-shut motions, acting on small molecules between them, sometimes assisted by transition metal ions. Second, organisms: Mica world had the potential to be a community or ecosystem of prebiotic organisms in a way unlike other models for the origin of life.     

The hemolymph proteome of the honeybee: Gel‐based or gel‐free?

The honeybee has an invaluable economic impact and is a model for studying immunity, development and social behavior. The recent sequencing and annotation of the honeybee genome facilitates the study of its hemolymph, which reflects the physiological condition and mediates immune responses. We aimed at making a proteomic reference map of honeybee hemolymph and compared gel‐free and gel‐based techniques. One hundered and four 2‐DE spots corresponding to 62 different proteins were identified. Eight identical 2‐DLC experiments resulted in the identification of 32 unique proteins. One repeat was clearly not representative for the potential of the given 2‐DLC setup. Only 27% of the identified hemolymph proteins were found by both techniques. In addition, we found proteins of three different viruses which creates possibilities for biomarker design. Future hemolymph studies will benefit from this work.     

Longitudinal growth during the first years of life: what is normal?

The anthropometric data of a longitudinal growth study on healthy infants, followed from birth until the age of 4 years and performed during 1995-1999 in The Netherlands, were used to analyze the general growth patterns in terms of height, weight and head circumference, based on z-scores, during the first 4 years of life. The well-known phenomenon where each infant or child tends to decelerate or accelerate its growth velocity depending on its starting position on the reference curve is obvious in this study too. This phenomenon, known as the regression to the mean, is a strong phenomenon especially during the first year. Regression to the mean is calculated for the different age groups as factor. With the given alpha, it is possible to estimate the individual expectation of growth.     

The origin of recent introns: transposons?

The long-standing question of how genes acquire introns has provoked much debate. A recent study makes considerable progress by identifying numerous recently gained introns in nematodes - although it remains difficult to distinguish definitively between models of intron gain.     

The origin of life—did it occur at high temperatures?

A high-temperature origin of life has been proposed, largely for the reason that the hyperthermophiles are claimed to be the last common ancestor of modern organisms. Even if they are the oldest extant organisms, which is in dispute, their existence can say nothing about the temperatures of the origin of life, the RNA world, and organisms preceding the hyperthermophiles. There is no geological evidence for the physical setting of the origin of life because there are no unmetamorphosed rocks from that period. Prebiotic chemistry points to a low-temperature origin because most biochemicals decompose rather rapidly at temperatures of 100°C (e.g., half-lives are 73 min for ribose, 21 days for cytosine, and 204 days for adenine). Hyperthermophiles may appear at the base of some phylogenetic trees because they outcompeted the mesophiles when they adapted to lower temperatures, possibly due to enhanced production of heat-shock proteins. Correspondence to: S.L. Miller     

Calcium: Just Another Regulator in the Machinery of Life?

*BACKGROUND: Current hypotheses imply that stimulus-response systems in plants are networks of signal transduction pathways. It is usually assumed that these pathways connect receptors with effectors via chains of molecular events. Diverse intermediate signalling components (transducers) participate in these processes. However, many cellular transducers respond to several stimuli. Hence, there are no discrete chains but rather pathways that interconnect network-modules of different command structure. In particular, the cytosolic free Ca2+ concentration ([Ca2+](cyt)) is thought to perform many different tasks in a wide range of cellular events. However, this range of putative functions is so wide that it is often questioned how Ca2+ can comply with the definition of a second messenger. *THE Ca2+ SIGNATURE HYPOTHESIS: Some authors have suggested the concept of a specific signature of the ([Ca2+](cyt)) response. This implies that characteristics of the time course of changes in ([Ca2+](cyt)) and their localized sites of appearance in cells are used by the plant to identify the type and intensity of the stimulus. This hypothesis has triggered many investigations, which have yielded contradictory results. * THE CURRENT PICTURE: Much evidence suggests that the functions of calcium can be grouped into three classes: Ca2+ as a protective agent, Ca2+ as a chemical switch and Ca2+ as a 'digital' information carrier. Examples of the first two classes are presented here. The third is more controversial; while some investigations seem to support this idea, others call the Ca2+ signature hypothesis into question. Further investigations are needed to shed more light on Ca(2+)-driven signalling cascades.     

Microbial hydantoinases – industrial enzymes from the origin of life?

Hydantoinases are valuable enzymes for the production of optically pure d- and l-amino acids. They catalyse the reversible hydrolytic ring cleavage of hydantoin or 5′-monosubstituted hydantoins and are therefore classified in the EC nomenclature as cyclic amidases (EC 3.5.2.). In the EC nomenclature, four different hydantoin-cleaving enzymes are described: dihydropyrimidinase (3.5.2.2), allantoinase (EC 3.5.2.5), carboxymethylhydantoinase (EC 3.5.2.4), and N-methylhydantoinase (EC 3.5.2.14). Beside these, other hydantoinases with known metabolic functions, such as imidase and carboxyethylhydantoinase and enzymes with unknown metabolic function, are described in the literature and have not yet been classified. An important question is whether the distinct hydantoinases, which are frequently classified as l-, d-, and non-selective hydantoinases depending on their substrate specificity and stereoselectivity, are related to each other. In order to investigate the evolutionary relationship, amino acid sequence data can be used for a phylogenetic analysis. Although most of these enzymes only share limited sequence homology (identity<15%) and therefore are only distantly related, it can be shown (i) that most of them are members of a broad set of amidases with similarities to ureases and build a protein superfamily, whereas ATP-dependent hydantoinases are not related, (ii) that the urease-related amidases have evolved divergently from a common ancestor and (iii) that they share a metal-binding motif consisting of conserved histidine residues. The difference in enantioselectivity used for the classification of hydantoinases on the basis of their biotechnological value does not reflect their evolutionary relationship, which is to a more diverse group of enzymes than was assumed earlier. This protein superfamily probably has its origin in the prebiotic conditions of the primitive earth. Received: 24 August 1998 / Received revision: 9 November 1998 / Accepted: 21 November 1998     

The ‘kinetochore maintenance loop’—The mark of regulation?

Kinetochores can form and be maintained on DNA sequences that are normally non‐centromeric. The existence of these so‐called neo‐centromeres has posed the problem as to the nature of the epigenetic mechanisms that maintain the centromere. Here we highlight results that indicate that the amount of CENP‐A at human centromeres is tightly regulated. It is also known that kinetochore assembly requires sister chromatid cohesion at mitosis. We therefore suggest that separation or stretching between the sister chromatids at metaphase reciprocally determines the amount of centromere assembly in the subsequent interphase. This reciprocal relationship forms the basis of a negative feedback loop that could precisely control the amount of CENP‐A and faithfully maintain the presence of a kinetochore over many cell divisions. We describe how the feedback loop would work, propose how it could be tested experimentally and suggest possible components of its mechanism.