Cenozoic record of elongate,cylindrical, deep-sea benthic foraminifera in the North Atlantic and equatorial Pacific Oceans

In the late Pliocene–middle Pleistocene a group of 95 species of elongate, cylindrical, deep-sea (lower bathyal–abyssal) benthic foraminifera became extinct. This Extinction Group (Ext. Gp), belonging to three families (all the Stilostomellidae and Pleurostomellidae, some of the Nodosariidae), was a major component (20–70%) of deep-sea foraminiferal assemblages in the middle Cenozoic and subsequently declined in abundance and species richness before finally disappearing almost completely during the mid-Pleistocene Climatic Transition (MPT). So what caused these declines and extinction?In this study 127 Ext. Gp species are identified from eight Cenozoic bathyal and abyssal sequences in the North Atlantic and equatorial Pacific Oceans. Most species are long-ranging with 80% originating in the Eocene or earlier. The greatest abundance and diversity of the Ext. Gp was in the warm oceanic conditions of the middle Eocene–early Oligocene. The group was subjected to significant changes in the composition of the faunal dominants and slightly enhanced species turnover during and soon after the rapid Eocene–Oligocene cooling event. Declines in the relative abundance and flux of the Ext. Gp, together with enhanced species loss, occurred during middle–late Miocene cooling, particularly at abyssal sites. The overall number of Ext. Gp species present began declining earlier at mid abyssal depths (in middle Miocene) than at upper abyssal (in late Pliocene–early Pleistocene) and then lower bathyal depths (in MPT). By far the most significant Ext. Gp declines in abundance and species loss occurred during the more severe glacial stages of the late Pliocene–middle Pleistocene.Clearly, the decline and extinction of this group of deep-sea foraminifera was related to the function of their specialized apertures and the stepwise cooling of global climate and deep water. We infer that the apertural modifications may be related to the method of food collection or processing, and that the extinctions may have resulted from the decline or loss of their specific phytoplankton or prokaryote food source, that was more directly impacted than the foraminifera by the cooling temperatures.     

Tasman Front shifts and associated paleoceanographic changes during the last 250,000 years: foraminiferal evidence from the Lord Howe Rise

The paleoceanography of the Tasman Sea over the past 250,000 years was studied using benthic (>75 μm size fraction) and planktonic foraminifera (>149 μm size fraction) from three cores collected along 162°E traverse between 25°S and 30°S on the Lord Howe Rise. Planktonic foraminiferal oxygen isotope stratigraphy dates the cores between OIS 1 and 11. R-mode cluster and Q-mode factor analyses were carried out on benthic foraminiferal faunas, and Q-mode factor analysis and the modern analog technique (MAT) were used in analyzing planktonic foraminiferal faunas. Distinct benthic faunas across latitude from north (25°S) to south (30°S and 35°S) reflects the difference in primary productivity level in the overlying surface water. The MAT result is thought to express latitudinal shifts of the Tasman Front over the last 250,000 years with: (1) the Tasman Front at 35°S during the oxygen isotope stage (OIS) 1 (post-glacial period); (2) migration of the front nearby 25°S during the last glacial period (OIS 2–OIS 4) and slightly northward of its present position during the penultimate glacial period (OIS 6); and (3) a return of the front to near 35°S during OIS 5 and OIS 7. Based on time-series and spatial variations of benthic foraminiferal factor typified by Pseudoparrella exigua and Uvigerina peregrina and one variety, southern-winter mixing and convection along the Tasman Front may have strengthened during the interglacial OIS 7 in particular.     

CaMKII activates ASK1 and NF-kappaB to induce cardiomyocyte hypertrophy

Ca2+/calmodulin-dependent protein kinase (CaMK) is an important downstream target of Ca2+ in the hypertrophic signaling pathways. We previously showed that the activation of apoptosis signal-regulating kinase 1 (ASK1) or NF-kappaB is sufficient for cardiomyocyte hypertrophy. Infection of isolated neonatal cardiomyocytes with an adenoviral vector expressing CaMKIIdelta3 (AdCaMKIIdelta3) induced the activation of ASK1, while KN93, an inhibitor of CaMKII, inhibited phenylephrine-induced ASK1 activation. Overexpression of CaMKIIdelta3 induced characteristic features of in vitro cardiomyocyte hypertrophy. Infection of cardiomyocytes with an adenoviral vector expressing a dominant negative mutant of ASK1 (AdASK(KM)) inhibited the CaMKIIdelta3-induced hypertrophic responses. Overexpression of CaMKIIdelta3 increased the kappaB-dependent promoter/luciferase activity and induced IkappaBalpha degradation. Coinfection with AdCaMKIIdelta3 and AdASK(KM), and pre-incubation with KN93 attenuated CaMKIIdelta3- and phenylephrine-induced NF-kappaB activation, respectively. Expression of a degradation resistant mutant of IkappaBalpha inhibited CaMKIIdelta3-induced hypertrophic responses. These results indicate that CaMKIIdelta3 induces cardiomyocyte hypertrophy mediated through ASK1-NF-kappaB signal transduction pathway.     

Midline signaling and evolution of the forebrain in chordates: a focus on the lamprey Hedgehog case

Lampreys are agnathans (vertebrates without jaws). They occupy a key phylogenetic position in the emergence of novelties and in the diversification of morphology at the dawn of vertebrates. We have used lampreys to investigate the possibility that embryonic midline signaling systems have been a driving force for the evolution of the forebrain in vertebrates. We have focused on Sonic Hedgehog/Hedgehog (Shh/Hh) signaling. In this article, we first review and summarize our recent work on the comparative analysis of embryonic expression patterns for Shh/Hh, together with Fgf8 (fibroblast growth factor 8) and Wnt (wingless-Int) pathway components, in the embryonic lamprey forebrain. Comparison with nonvertebrate chordates on one hand, and jawed vertebrates on the other hand, shows that these morphogens/growth factors acquired new expression domains in the most rostral part of the neural tube in lampreys compared to nonvertebrate chordates, and in jawed vertebrates compared to lampreys. These data are consistent with the idea that changes in Shh, Fgf8 or Wnt signaling in the course of evolution have been instrumental for the emergence and diversification of the telencephalon, a part of the forebrain that is unique to vertebrates. We have then used comparative genomics on Shh/Hh loci to identify commonalities and differences in noncoding regulatory sequences across species and phyla. Conserved noncoding elements (CNEs) can be detected in lamprey Hh introns, even though they display unique structural features and need adjustments of parameters used for in silico alignments to be detected, because of lamprey-specific properties of the genome. The data also show conservation of a ventral midline enhancer located in Shh/Hh intron 2 of all chordates, the very species which possess a notochord and a floor plate, but not in earlier emerged deuterostomes or protostomes. These findings exemplify how the Shh/Hh locus is one of the best loci to study genome evolution with regards to developmental events.     

Failure to Degrade CAT-Tailed Proteins Disrupts Neuronal Morphogenesis and Cell Survival

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Meningitis patients with Angiostrongylus cantonensis may present without eosinophilia in the cerebrospinal fluid in northern Vietnam

BackgroundEosinophilic meningitis (EM) is a rare clinical syndrome caused by both infectious and noninfectious diseases. In tropical pacific countries, Angiostrongylus cantonensis is the most common cause. However, the EM definition varies in the literature, and its relation to parasitic meningitis (PM) remains unclear.Methodology/Principal findingsAdult and adolescent patients of 13 years old or above with suspected central nervous system (CNS) infections with abnormal CSF findings were prospectively enrolled at a tertiary referral hospital in Hanoi, Vietnam from June 2012 to May 2014. Patients with EM or suspected PM (EM/PM) were defined by the presence of either ≥10% eosinophils or an absolute eosinophil cell counts of ≥10/mm³ in the CSF or blood eosinophilia (>16% of WBCs) without CSF eosinophils. In total 679 patients were enrolled: 7 (1.03%) had ≥10% CSF eosinophilia, 20 (2.95%) had ≥10/mm³ CSF eosinophilia, and 7 (1.03%) had >16% blood eosinophilia. The patients with ≥10% CSF eosinophilia were significantly younger (p = 0.017), had a lower body temperature (p = 0.036) than patients with ≥10/mm³ CSF eosinophilia among whom bacterial pathogens were detected in 72.2% (13/18) of those who were tested by culture and/or PCR. In contrast, the characteristics of the patients with >16% blood eosinophilia resembled those of patients with ≥10% CSF eosinophilia. We further conducted serological tests and real-time PCR to identify A. cantonensis. Serology or real-time PCR was positive in 3 (42.8%) patients with ≥10% CSF eosinophilia and 6 (85.7%) patients with >16% blood eosinophilia without CSF eosinophils but none of patients with ≥10/mm³ CSF eosinophilia.ConclusionsThe etiology of PM in northern Vietnam is A. cantonensis. The eosinophil percentage is a more reliable predictor of parasitic EM than absolute eosinophil count in the CSF. Patients with PM may present with a high percentage of eosinophils in the peripheral blood but not in the CSF.