scholarly journals Low Serum Erythropoietin Levels are Associated with Fatal COVID-19 Cases at 4,150 meters above sea level

Author(s):  
Antonio Viruez-Soto ◽  
Mónica Marlene López-Dávalos ◽  
Gabriel Rada-Barrera ◽  
Alfredo Merino-Luna ◽  
Daniel Molano-Franco ◽  
...  
1996 ◽  
Vol 72 (4) ◽  
pp. 297-302 ◽  
Author(s):  
Tom Klausen ◽  
Troels Dirch Poulsen ◽  
Niels Fogh-Andersen ◽  
Jean-Paul Richalet ◽  
Ove Juel Nielsen ◽  
...  

2015 ◽  
Vol 24 (6) ◽  
pp. 544-547 ◽  
Author(s):  
Ibrahim Kocaoglu ◽  
Ugur Arslan ◽  
Yavuzer Koza ◽  
Mustafa M�cahit Balci ◽  
Gizem �elik ◽  
...  

Haematologica ◽  
2007 ◽  
Vol 92 (12) ◽  
pp. 1607-1614 ◽  
Author(s):  
M. J. Percy ◽  
L. M. Scott ◽  
W. N. Erber ◽  
C. N. Harrison ◽  
J. T. Reilly ◽  
...  

1985 ◽  
Vol 59 (2) ◽  
pp. 360-364 ◽  
Author(s):  
J. S. Milledge ◽  
P. M. Cotes

Serum immunoreactive erythropoietin (siEp) was estimated in samples collected from members of two scientific and mountaineering expeditions, to Mount Kongur in Western China and to Mount Everest in Nepal. SiEp was increased above sea-level control values 1 and 2 days after arrival at 3,500 m and remained high on ascent to 4,500 m. Thereafter, while subjects remained at or above 4,500 m, siEp declined, and by 22 days after the ascent to 4,500 m was at control values but increased on ascent to higher altitude. Thus siEp was at a normal level during the maintenance of secondary polycythemia from high-altitude exposure. On descent, with removal of altitude hypoxia, siEp decreased, but despite secondary polycythemia levels remained measurable and in the range found in subjects normally resident at sea level. On Mount Everest, siEp was significantly (P less than 0.01) elevated above preexpedition sea-level controls after 2–4 wk at or above 6,300 m. There was no correlation between estimates of siEp and plasma renin activity in samples collected before and during both expeditions.


Blood ◽  
2007 ◽  
Vol 110 (11) ◽  
pp. 263-263
Author(s):  
Daniela Pietra ◽  
Sai Li ◽  
Angela Brisci ◽  
Francesco Passamonti ◽  
Elisa Rumi ◽  
...  

Abstract About 95% of patients with polycythemia vera (PV) carry the unique V617F mutation in JAK2 exon 14, which encodes a portion of the JH2 auto-inhibitory domain of the Jak2 kinase. Mutations in exon 12 have been recently reported in JAK2 (V617F)-negative patients with PV or idiopathic erythrocytosis. We searched for exon 12 mutations in 168 patients with JAK2 (V617F)-negative myeloproliferative disorders. The 2001 WHO criteria were employed for diagnosis. Of the 168 patients studied, 47 had sporadic PV, 11 had familial PV, 75 had essential thrombocythemia (ET), and 35 had primary myelofibrosis (PM). Seventeen patients with PV, including 15/47 sporadic cases and 2/11 familial cases, were found to carry deletions (n=15) or duplications (n=2) of exon 12 in circulating granulocytes but not in T-lymphocytes. None of the 110 patients with ET or PM was found to be positive. Mutations were detected by sequencing, and were then confirmed by sub-cloning in bacteria in 7/17 cases. Four of the 8 mutations detected were novel, while the most frequent ones were N542–E543del and E543–D544del. Mutations spanned from base 1606 to 1640, and the two duplications modified the rest of the sequence by adding 33 bp. In terms of protein, deletions predicted aminoacid changes spanning from phenylalanine 537 to aspartic acid 544, while duplications predicted changes from phenylalanine 547 onwards within the JH2 pseudokinase domain. Three categories of molecular lesions were identified: those involving a K539L substitution; those involving the E543del; and aminoacid duplications involving a substitution of phenylalanine 547. At clinical onset, 16/17 (94%) patients carrying a JAK2 exon 12 mutation had low serum erythropoietin (Epo) levels, indicating a combination of absolute erythrocytosis and suppressed endogenous Epo production. Moreover, 12/17 patients had erythrocytosis associated with normal white blood cell and platelet counts, i.e., isolated erythrocytosis. This frequency (71%) was significantly higher than that observed in 92 patients diagnosed with JAK2 (V617F)-positive PV at the Department of Hematology, IRCCS Policlinico San Matteo, Pavia, Italy (P<0.001). Most of these latter patients, in fact, had erythrocytosis combined with leukocytosis (WBC>12 x 109/L) and/or thrombocytosis (PLT>400 x 109/L), and only 22% of them had isolated erythrocytosis. Both patients with familial PV carrying an exon 12 mutation had an affected sibling with JAK2 (V617F)-positive PV. While the former showed isolated erythrocytosis, their JAK2 (V617F)-positive siblings had also thrombocytosis. In conclusion: several somatic mutations of JAK2 exon 12 - mostly 6 bp deletions - can be found in patients with a myeloproliferative disorder that is mainly characterized by erythrocytosis associated with low serum Epo levels; a genetic predisposition to acquisition of different JAK2 mutations is inherited in families with myeloproliferative disorders, and the mutation type (exon 12 vs exon 14) contributes to determining their variable clinical phenotype.


2018 ◽  
Vol 139 (4) ◽  
pp. 217-219 ◽  
Author(s):  
Mark A. Catherwood ◽  
Amy Graham ◽  
Robert J.G. Cuthbert ◽  
Celine Garrec ◽  
Betty Gardie ◽  
...  

1975 ◽  
Vol 26 ◽  
pp. 395-407
Author(s):  
S. Henriksen

The first question to be answered, in seeking coordinate systems for geodynamics, is: what is geodynamics? The answer is, of course, that geodynamics is that part of geophysics which is concerned with movements of the Earth, as opposed to geostatics which is the physics of the stationary Earth. But as far as we know, there is no stationary Earth – epur sic monere. So geodynamics is actually coextensive with geophysics, and coordinate systems suitable for the one should be suitable for the other. At the present time, there are not many coordinate systems, if any, that can be identified with a static Earth. Certainly the only coordinate of aeronomic (atmospheric) interest is the height, and this is usually either as geodynamic height or as pressure. In oceanology, the most important coordinate is depth, and this, like heights in the atmosphere, is expressed as metric depth from mean sea level, as geodynamic depth, or as pressure. Only for the earth do we find “static” systems in use, ana even here there is real question as to whether the systems are dynamic or static. So it would seem that our answer to the question, of what kind, of coordinate systems are we seeking, must be that we are looking for the same systems as are used in geophysics, and these systems are dynamic in nature already – that is, their definition involvestime.


Author(s):  
Irwin I. Singer

Our previous results indicate that two types of fibronectin-cytoskeletal associations may be formed at the fibroblast surface: dorsal matrixbinding fibronexuses generated in high serum (5% FBS) cultures, and ventral substrate-adhering units formed in low serum (0.3% FBS) cultures. The substrate-adhering fibronexus consists of at least vinculin (VN) and actin in its cytoplasmic leg, and fibronectin (FN) as one of its major extracellular components. This substrate-adhesion complex is localized in focal contacts, the sites of closest substratum approach visualized with interference reflection microscopy, which appear to be the major points of cell-tosubstrate adhesion. In fibroblasts, the latter substrate-binding complex is characteristic of cultures that are arrested at the G1 phase of the cell cycle due to the low serum concentration in their medium. These arrested fibroblasts are very well spread, flattened, and immobile.


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