PNZIP Is a Novel Mesophyll-Specific cDNA That Is Regulated by Phytochrome and a Circadian Rhythm and Encodes a Protein with a Leucine Zipper Motif1

We isolated and characterized a novel light-regulated cDNA from the short-day plant Pharbitis nil that encodes a protein with a leucine (Leu) zipper motif, designated PNZIP (Pharbitis nil Leu zipper). The PNZIP cDNA is not similar to any other gene with a known function in the database, but it shares high sequence homology with an Arabidopsis expressed sequence tag and to two other sequences of unknown function from the cyanobacterium Synechocystis spp. and the red alga Porphyra purpurea, which together define a new family of evolutionarily conserved Leu zipper proteins. PNZIP is a single-copy gene that is expressed specifically in leaf photosynthetically active mesophyll cells but not in other nonphotosynthetic tissues such as the epidermis, trichomes, and vascular tissues. When plants were exposed to continuous darkness, PNZIP exhibited a rhythmic pattern of mRNA accumulation with a circadian periodicity of approximately 24 h, suggesting that its expression is under the control of an endogenous clock. However, the expression of PNZIP was unusual in that darkness rather than light promoted its mRNA accumulation. Accumulation of PNZIP mRNA during the dark is also regulated by phytochrome, since a brief exposure to red light in the middle of the night reduced its mRNA levels. Moreover, a far-red-light treatment at the end of day also reduced PNZIP mRNA accumulation during the dark, and that effect could be inhibited by a subsequent exposure to red light, showing the photoreversible response attributable to control through the phytochrome system.

A family of transmembrane proteins with homology to the MET-hepatocyte growth factor receptor.

In hunting for unknown genes on the human X chromosome, we identified a cDNA in Xq28 encoding a transmembrane protein (SEX) of 1871 amino acids. SEX shares significant homology with the extracellular domain of the receptors encoded by the oncogenes MET, RON, and SEA [hepatocyte growth factor (HGF) receptor family]. Further screenings of cDNA libraries identified three additional sequences closely related to SEX: these were named SEP, OCT, and NOV and were located on human chromosomes 3p, 1, and 3q, respectively. The proteins encoded by these genes contain large cytoplasmic domains characterized by a distinctive highly conserved sequence (SEX domain). Northern blot analysis revealed different expression of the SEX family of genes in fetal tissues, with SEX, OCT, and NOV predominantly expressed in brain, and SEP expressed at highest levels in kidney. In situ hybridization analysis revealed that SEX has a distinctive pattern of expression in the developing nervous system of the mouse, where it is found in postmitotic neurons from the first stages of neuronal differentiation (9.5 day postcoitus). The SEX protein (220 kDa) is glycosylated and exposed at the cell surface. Unlike the receptors of the HGF family, p220SEX, a MET-SEX chimera or a constitutively dimerized TPR-SEX does not show tyrosine kinase activity. These data define a gene family (SEX family) involved in the development of neural and epithelial tissues, which encodes putative receptors with unexpected enzymatic or binding properties.

The murine stk gene product, a transmembrane protein tyrosine kinase, is a receptor for macrophage-stimulating protein.

Macrophage-stimulating protein (MSP) was originally identified as an inducer of murine resident peritoneal macrophage responsiveness to chemoattractants. We recently showed that the product of RON, a protein tyrosine kinase cloned from a human keratinocyte library, is the receptor for MSP. Similarity of murine stk to RON led us to determine if the stk gene product is the murine receptor for MSP. Radiolabeled MSP could bind to NIH 3T3 cells transfected with murine stk cDNA (3T3/stk). Binding was saturable and was inhibited by unlabeled MSP but not by structurally related proteins, including hepatocyte growth factor and plasminogen. Specific binding to STK was demonstrated by cross-linking of 125I-labeled MSP to membrane proteins of 3T3/stk cells, which resulted in a protein complex with a molecular mass of 220 kDa. This radiolabeled complex comprised 125I-MSP and STK, since it could be immunoprecipitated by antibodies to the STK beta chain. Binding of MSP to stk cDNA-transfected cells induced tyrosine phosphorylation of the 150-kDa STK beta chain within 1 min and caused increased motile activity. These results establish the murine stk gene product as a specific transmembrane protein tyrosine kinase receptor for MSP. Inasmuch as the stk cDNA was cloned from a hematopoietic stem cell, our data suggest that in addition to macrophages and keratinocytes, a cell in the hematopoietic lineage may also be a target for MSP.

The Relationship Between Cadwaladerite Al(OH)2Cl∙4H2O and Lesukite Al2(OH)5Cl∙2H2O as Investigated by SEM, PXRD, FTIR and Raman Spectroscopy

Cadwaladerite (Al(OH)2Cl∙4H2O) collected from Cerro Pintados, Chile described by Gordon in 1941 is designated as “doubtful” by the IMA. Material collected from the same locality in 2015 resembling the description of cadwaladerite gave a powder XRD pattern similar to lesukite (Al2(OH)5Cl∙2H2O). However, Gordon provided no X-ray data for his material from Cerro Pintados. In order to determine whether cadwaladerite and lesukite are the same mineral species, measurements were made on a suite of samples from various localities. A portion of the material collected by Gordon in 1941 was also obtained from the Mineralogical Museum of Harvard University. Type material of lesukite from a fumarolic environment at the Tolbachik Fissure in Kamchatka, Russia was obtained as well as lesukite from the Maria Mine, Chile (Arica Province) and a previously undescribed locality for lesukite (Barranaca del Sulfato, Mejillones Peninsula, Antofagasta Province). All samples are yellow to yellow-orange in colour and all exhibit small cubic crystals (up to 50µm), even Gordon’s cadwaladerite which was thought to be amorphous. The Chilean samples are all associated with halite and sometimes with anhydrite. These five samples were studied by SEM, FTIR, powder XRD, and Raman spectroscopy. A ratio of Al:Cl less than or equal to 1.3:1 was observed for all the samples, including measurements made on lesukite from the Russian locality Vergasova et al. studied in 1997, and determined to have a 2:1 ratio. SEM-EDS analyses also show all samples to have minor iron substitution, as well as copper substitution in two samples. FTIR spectra are very similar for all samples. Raman spectroscopy done on both samples collected in Cerro Pintados and the Russian lesukite gave similar spectra. Powder XRD analyses on all samples showed spectra identified to be lesukite, including Gordon’s cadwaladerite. Crystal cell parameters calculated from powder XRD ranged from 19.778Å to 19.878Å. Results using modern instrumental techniques confirm Gordon’s cadwaladerite, collected in 1939 and described in 1941, and lesukite are the same mineral species.

(Table 2) Age determination of sediment cores from the Panama Basin

Application of the 230Th normalization method to estimate sediment burial fluxes in six cores from the eastern equatorial Pacific (EEP) reveals that bulk sediment and organic carbon fluxes display a coherent regional pattern during the Holocene that is consistent with modern oceanographic conditions, in contrast with estimates of bulk mass accumulation rates (MARs) derived from core chronologies. Two nearby sites (less than 10 km apart), which have different MARs, show nearly identical 230Th-normalized bulk fluxes. Focusing factors derived from the 230Th data at the foot of the Carnegie Ridge in the Panama Basin are >2 in the Holocene, implying that lateral sediment addition is significant in this part of the basin. New geochemical data and existing literature provide evidence for a hydrothermal source of sediment in the southern part of the Panama Basin and for downslope transport from the top of the Carnegie Ridge. The compilation of core records suggests that sediment focusing is spatially and temporally variable in the EEP. During oxygen isotope stage 2 (OIS 2, from 13-27 ka BP), focusing appears even higher compared to the Holocene at most sites, similar to earlier findings in the eastern and central equatorial Pacific. The magnitude of the glacial increase in focusing factors, however, is strongly dependent on the accuracy of age models. We offer two possible explanations for the increase in glacial focusing compared to the Holocene. The first one is that the apparent increase in lateral sediment redistribution is partly or even largely an artifact of insufficient age control in the EEP, while the second explanation, which assumes that the observed increase is real, involves enhanced deep sea tidal current flow during periods of low sea level stand.

(Table 1) Magnetic properties and Curie temperatures of basalts from DSDP Leg 65 holes

During DSDP Leg 65, we achieved significant basement penetration at three sites (482, 483, and 485) in the mouth of the Gulf of California (Lewis and Robinson, 1983, doi:10.2973/dsdp.proc.65.1983). Since these holes were all drilled into extremely young crust near the crest of the East Pacific Rise, the rocks we recovered present an unusual opportunity to study the magnetic properties of submarine basalts before alteration has become pervasive. To take advantage of this opportunity and to complement the paleomagnetic studies conducted on these basalts by Day (1983, doi:10.2973/dsdp.proc.65.138.1983), we have studied, in the same samples, the following properties: saturation magnetization (Js); intensity and stability of isothermal remanent magnetization (IRM); hysteresis parameters, such as the coercive force (Hc), the remanent coercive force (HRC), and the ratio of saturation remanence (JRS) to saturation magnetization; susceptibility (x); and Curie temperature (Tc). In this chapter we will discuss the results of these studies in conjunction with the opaque mineralogy of the samples.

1971 University of Michigan Football Team

1972 University of Michigan Football Team

1973 University of Michigan Football Team

1976 University of Michigan Football Team

1977 University of Michigan Football Team