48 research outputs found
A phase 1/2, open-label, dose-escalation study of midostaurin in children with relapsed or refractory acute leukaemia
State of the climate in 2018
In 2018, the dominant greenhouse gases released into Earth’s atmosphere—carbon dioxide, methane, and nitrous oxide—continued their increase. The annual global average carbon dioxide concentration at Earth’s surface was 407.4 ± 0.1 ppm, the highest in the modern instrumental record and in ice core records dating back 800 000 years. Combined, greenhouse gases and several halogenated gases contribute just over 3 W m−2 to radiative forcing and represent a nearly 43% increase since 1990. Carbon dioxide is responsible for about 65% of this radiative forcing. With a weak La Niña in early 2018 transitioning to a weak El Niño by the year’s end, the global surface (land and ocean) temperature was the fourth highest on record, with only 2015 through 2017 being warmer. Several European countries reported record high annual temperatures. There were also more high, and fewer low, temperature extremes than in nearly all of the 68-year extremes record. Madagascar recorded a record daily temperature of 40.5°C in Morondava in March, while South Korea set its record high of 41.0°C in August in Hongcheon. Nawabshah, Pakistan, recorded its highest temperature of 50.2°C, which may be a new daily world record for April. Globally, the annual lower troposphere temperature was third to seventh highest, depending on the dataset analyzed. The lower stratospheric temperature was approximately fifth lowest. The 2018 Arctic land surface temperature was 1.2°C above the 1981–2010 average, tying for third highest in the 118-year record, following 2016 and 2017. June’s Arctic snow cover extent was almost half of what it was 35 years ago. Across Greenland, however, regional summer temperatures were generally below or near average. Additionally, a satellite survey of 47 glaciers in Greenland indicated a net increase in area for the first time since records began in 1999. Increasing permafrost temperatures were reported at most observation sites in the Arctic, with the overall increase of 0.1°–0.2°C between 2017 and 2018 being comparable to the highest rate of warming ever observed in the region. On 17 March, Arctic sea ice extent marked the second smallest annual maximum in the 38-year record, larger than only 2017. The minimum extent in 2018 was reached on 19 September and again on 23 September, tying 2008 and 2010 for the sixth lowest extent on record. The 23 September date tied 1997 as the latest sea ice minimum date on record. First-year ice now dominates the ice cover, comprising 77% of the March 2018 ice pack compared to 55% during the 1980s. Because thinner, younger ice is more vulnerable to melting out in summer, this shift in sea ice age has contributed to the decreasing trend in minimum ice extent. Regionally, Bering Sea ice extent was at record lows for almost the entire 2017/18 ice season. For the Antarctic continent as a whole, 2018 was warmer than average. On the highest points of the Antarctic Plateau, the automatic weather station Relay (74°S) broke or tied six monthly temperature records throughout the year, with August breaking its record by nearly 8°C. However, cool conditions in the western Bellingshausen Sea and Amundsen Sea sector contributed to a low melt season overall for 2017/18. High SSTs contributed to low summer sea ice extent in the Ross and Weddell Seas in 2018, underpinning the second lowest Antarctic summer minimum sea ice extent on record. Despite conducive conditions for its formation, the ozone hole at its maximum extent in September was near the 2000–18 mean, likely due to an ongoing slow decline in stratospheric chlorine monoxide concentration. Across the oceans, globally averaged SST decreased slightly since the record El Niño year of 2016 but was still far above the climatological mean. On average, SST is increasing at a rate of 0.10° ± 0.01°C decade−1 since 1950. The warming appeared largest in the tropical Indian Ocean and smallest in the North Pacific. The deeper ocean continues to warm year after year. For the seventh consecutive year, global annual mean sea level became the highest in the 26-year record, rising to 81 mm above the 1993 average. As anticipated in a warming climate, the hydrological cycle over the ocean is accelerating: dry regions are becoming drier and wet regions rainier. Closer to the equator, 95 named tropical storms were observed during 2018, well above the 1981–2010 average of 82. Eleven tropical cyclones reached Saffir–Simpson scale Category 5 intensity. North Atlantic Major Hurricane Michael’s landfall intensity of 140 kt was the fourth strongest for any continental U.S. hurricane landfall in the 168-year record. Michael caused more than 30 fatalities and 6 billion (U.S. dollars) in damages across the Philippines, Hong Kong, Macau, mainland China, Guam, and the Northern Mariana Islands. Tropical Storm Son-Tinh was responsible for 170 fatalities in Vietnam and Laos. Nearly all the islands of Micronesia experienced at least moderate impacts from various tropical cyclones. Across land, many areas around the globe received copious precipitation, notable at different time scales. Rodrigues and Réunion Island near southern Africa each reported their third wettest year on record. In Hawaii, 1262 mm precipitation at Waipā Gardens (Kauai) on 14–15 April set a new U.S. record for 24-h precipitation. In Brazil, the city of Belo Horizonte received nearly 75 mm of rain in just 20 minutes, nearly half its monthly average. Globally, fire activity during 2018 was the lowest since the start of the record in 1997, with a combined burned area of about 500 million hectares. This reinforced the long-term downward trend in fire emissions driven by changes in land use in frequently burning savannas. However, wildfires burned 3.5 million hectares across the United States, well above the 2000–10 average of 2.7 million hectares. Combined, U.S. wildfire damages for the 2017 and 2018 wildfire seasons exceeded $40 billion (U.S. dollars)
High EVI1 expression Is Associated with MLL rearrangements and Predicts Decreased Survival in Pediatric AML: A Report From the Children's Oncology Group.
The Prognostic Effect of High WT1 Gene Expression in Pediatric AML Depends on WT1 SNP rs16754 Status: A Report From the Children's Oncology Group (COG)
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Sea-BCMA Mono- and Combination Therapy in Patients with Relapsed/Refractory Multiple Myeloma: Updated Results of a Phase 1 Study (SGNBCMA-001)
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SEA-BCMA, an Investigational Nonfucosylated Monoclonal Antibody: Ongoing Results of a Phase 1 Study in Patients with Relapsed/Refractory Multiple Myeloma (SGNBCMA-001)
Abstract
Background
Patients (pts) with relapsed/triple-class refractory (R/R; refractory to a proteasome inhibitor, immunomodulatory drug or anti-CD38 antibody) multiple myeloma (MM) have limited treatment options. A need remains for novel combination therapies with manageable toxicity and non-cross-resistant mechanisms of action. B-cell maturation antigen (BCMA) is expressed in most MM pt tumors. SEA-BCMA is an investigational, humanized, nonfucosylated IgG1 monoclonal anti-BCMA antibody. Proposed mechanisms of action of SEA-BCMA include blocking of BCMA-mediated pro-survival and proliferative signaling, mediating antibody-dependent cellular phagocytosis, and displaying enhanced antibody-dependent cellular cytotoxicity. Preclinical data demonstrate promising antitumor activity and versatile combinability. Here, we present preliminary data from the first-in-human Phase 1 clinical trial.
Methods
SGNBCMA-001 (NCT03582033) is an ongoing phase 1, open-label, multicenter, dose-escalation and expansion study to evaluate the safety, tolerability and antitumor activity of SEA-BCMA in adults with R/R MM not previously exposed to any other BCMA-directed therapy. Part A tested monotherapy safety and tolerability with dose escalation (100-1600 mg flat dosing once every 2 weeks [Q2W] by intravenous infusion), and dose expansion at the highest tolerated dose. Parts B and C aim to optimize efficacy by testing intensified dosing (Part B; weekly [Q1W] induction dosing of SEA BCMA for 8 weeks is followed by Q2W maintenance dosing) and dexamethasone (DEX) combination therapy (Part C) in pts who have received ≥3 prior lines of therapy for MM and are triple-class refractory. Responses are assessed per the 2016 International Myeloma Working Group criteria.
Results
As of June 15, 2021, Part A completed enrollment. A total of 55 pts received SEA-BCMA (see Table 1 for pt characteristics).
SEA-BCMA was generally well tolerated, and the maximum tolerated dose was not reached in the 5 dose levels tested in Part A (100, 200, 400, 800, or 1600 mg Q2W; n=2, 2, 2, 7, and 7, respectively). At 800 mg, 1 of 7 pts reported a Grade 3 infusion-related reaction (IRR), which met dose-limiting toxicity (DLT) criteria by lasting >24 hours despite supportive care. This constituted the single DLT observed during dose escalation. Subsequently, dose expansion (n=15) proceeded at 1600 mg Q2W. The most common treatment-emergent adverse events (TEAEs) observed with 1600 mg Q2W (n=22) were fatigue (32%), pyrexia (23%), IRR (23%), and hypertension (23%) for non-hematological events, and anemia (14%) for hematologic events. The most common ≥Grade 3 TEAEs with 1600 mg Q2W were anemia and syncope (9% each). Following a safety monitoring review, premedication with acetaminophen + antihistamine was introduced to mitigate IRRs in expansion cohorts. Parts B and C completed parallel safety run-ins (n=6 each) at the 1600 mg dose with no DLTs observed and with similar tolerability.
Pharmacokinetic (PK) analyses indicate serum SEA-BCMA exposures increased proportionally with increasing dose with a half-life of approximately 10 days. Preliminary analyses suggest the PK profile of SEA-BCMA in combination therapy with DEX (n=5) is comparable to monotherapy and is unaltered with a change in schedule from Q2W to Q1W.
Three of 22 pts who received 1600 mg SEA-BCMA Q2W monotherapy (Part A) achieved a confirmed objective response (OR; OR rate: 14% [95% confidence interval: 2.91, 34.91]; 2 partial responses [PR], 1 very good PR [VGPR]). To date, 3 pts remain on treatment (2 PRs and 1 stable disease). The median duration of treatment was 12 weeks (Figure 1; range 4-88).
In Parts B and C, 2 of 8 (2 PR) and 2 of 12 (1 VGPR, 1 PR) pts reported a confirmed OR; 3 of the 4 responding pts remain on treatment in cycle 7, 8, and 9, respectively.
Conclusions
Preliminary results for SGNBCMA-001 suggest a favorable safety profile and combination potential. SEA-BCMA also showed encouraging duration on treatment and initial antitumor activity in a heavily pre-treated late-line R/R MM pt population. Expansion cohorts testing intensified SEA-BCMA dosing and the addition of DEX are underway to further assess the safety, tolerability, and estimate of SEA-BCMA activity in the context of these treatment approaches. An additional expansion cohort (Part D), testing the combination of SEA-BCMA with pomalidomide and DEX in pts who have received ≥2 prior lines of therapy, is now enrolling.
Figure 1 Figure 1.
Disclosures
Hoffman: BMS, Celgene: Honoraria. Lipe: Seagen Inc.: Research Funding; BMS: Consultancy, Research Funding; Janssen: Consultancy, Research Funding; sanofi: Consultancy; GlaxoSmithKline: Consultancy; amgen: Research Funding; Cellectar: Research Funding; Karyopharm: Research Funding; Harpoon: Research Funding. Melear: Astrazeneca: Speakers Bureau; TG Therapeutics: Speakers Bureau; Janssen: Speakers Bureau. Liedtke: Pfizer: Honoraria; Janssen Pharmaceuticals: Membership on an entity's Board of Directors or advisory committees; Bristol Myers Squibb: Membership on an entity's Board of Directors or advisory committees; Alnylam: Membership on an entity's Board of Directors or advisory committees; Celgene: Membership on an entity's Board of Directors or advisory committees; Kura Oncology: Membership on an entity's Board of Directors or advisory committees; Caelum: Membership on an entity's Board of Directors or advisory committees, Other: Clinical Trial Funding; Kite: Membership on an entity's Board of Directors or advisory committees; Karyopharm: Membership on an entity's Board of Directors or advisory committees; Sanofi: Membership on an entity's Board of Directors or advisory committees; Takeda: Membership on an entity's Board of Directors or advisory committees; Oncopeptides: Membership on an entity's Board of Directors or advisory committees; GlaxoSmithKline: Membership on an entity's Board of Directors or advisory committees. Niesvizky: Takeda: Consultancy, Research Funding; Janssen: Consultancy, Research Funding; GSK: Consultancy, Research Funding; BMS: Consultancy, Research Funding; Karyopharm: Consultancy, Research Funding. Tomasson: Pfizer, Inc.: Research Funding; Rafael Pharmaceuticals: Research Funding; syros Pharmaceuticals: Research Funding; Janssen R&D: Research Funding; Seagen, Inc.: Research Funding. Yasenchak: Seagen Inc.: Research Funding. Green: Seagen Inc.: Research Funding; bristol myers squibb: Membership on an entity's Board of Directors or advisory committees, Patents & Royalties, Research Funding; Cellectar Biosciences: Research Funding; GSK: Membership on an entity's Board of Directors or advisory committees; Janssen Biotech: Membership on an entity's Board of Directors or advisory committees, Research Funding; Juno Therapeutics: Patents & Royalties, Research Funding; Legend Biotech: Consultancy; Neoleukin Therapeutics: Membership on an entity's Board of Directors or advisory committees; Seattle Genetics: Membership on an entity's Board of Directors or advisory committees, Research Funding; SpringWorks Therapeutics: Research Funding. Li: Seagen Inc.: Current Employment, Current equity holder in publicly-traded company. Wang: Seagen Inc.: Current Employment, Current equity holder in publicly-traded company. Ho: Seagen Inc.: Current Employment, Current equity holder in publicly-traded company