Tuesday, November 11, 2025

CRISPR CRITTERS

CRISPR enabled precision oncology: from gene editing to tumor microenvironment remodeling




FAR Publishing Limited
Timeline of CRISPR Evolution: From DNA Editing to Applications in Precision Oncology. 

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This figure illustrates the evolution of CRISPR technology from 1987 to 2019, presented in a horizontal timeline format and categorized into four generations, each denoted by a distinct color: The first generation (blue) represents DNA double-strand break editing technology, initiated with the establishment of the SpCas9 system in 2007 and subsequently refined for precision through advances such as the Cas9-D10A nickase and the high-fidelity SpCas9-HF1 in 2015; The second generation (orange) refers to targeted DNA cutting technology, including Cas12, developed in 2015, and Cas14, invented in 2018, which overcame PAM sequence restrictions, thereby enabling a broader target range and expanding applications from gene editing to molecular-level diagnostics; The third generation (green) involves targeted RNA regulation technology, encompassing the CRISPRi/a system for transcriptional regulation, the Cas13 system, invented in 2016, for the specific degradation and modification of cancer-related mRNA, and dCas9-DNMT3A/TET1-mediated DNA methylation editing developed between 2022 and 2023; The fourth generation (yellow) encompasses precise editing technologies that avoid double-strand breaks, including base editors (CBE/ABE), developed in 2016, and the Prime Editor, introduced in 2019, which have broadened applications to include the repair of diverse point mutations and the correction of tumor driver genes such as EGFR.

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Credit: Kailai Li,Peixin Huang,Yue Qian,Anqi Lin,Jingjun He,Junyi Shen,Li Chen,Kai Miao,Jian Zhang





CRISPR gene-editing technology, renowned for its precision, is revolutionizing oncology research and treatment. Its evolution spans from the initial DNA double-strand break-inducing Cas9 to more advanced systems like Cas12, Cas13, base editors, and prime editors. These tools have expanded the scope of CRISPR beyond simple gene knockout to include RNA editing, transcriptional regulation, and epigenetic reprogramming, establishing a versatile platform for precision cancer interventions.

 

The generational progression of CRISPR systems has directly fueled innovations in cancer research. First-generation Cas9 enabled foundational gene knockout studies. Subsequent generations introduced Cas12 for DNA targeting with different PAM requirements, Cas13 for RNA degradation, and base/prime editors for precise nucleotide changes without inducing double-strand breaks. This functional expansion allows researchers to systematically investigate cancer mechanisms, from identifying driver genes to modeling drug resistance.

 

A primary application of CRISPR in oncology is the systematic identification of tumor driver genes and synthetic lethal targets through high-throughput screening. Genome-wide CRISPR libraries, such as GeCKO, have been instrumental in pinpointing genes essential for cancer progression, metastasis, and drug resistance across various cancer types. Furthermore, technologies like Perturb-seq, which combines CRISPR perturbation with single-cell RNA sequencing, enable the mapping of gene regulatory networks and heterogeneous cellular responses at single-cell resolution. CRISPR is also pivotal in dissecting the tumor microenvironment (TME) and immune evasion mechanisms. It is used to study metabolic reprogramming by targeting enzymes like LDHA, modulate angiogenesis via genes like VHL, and disrupt immune checkpoints such as PD-L1 and CD47. By editing these components, CRISPR helps reveal how tumors evade immune surveillance and suggests strategies for TME remodeling to enhance anti-tumor immunity.

 

In therapeutic development, CRISPR enables precise targeting of oncogenes and reactivation of tumor suppressor genes. Strategies include inactivating fusion oncogenes like BCR-ABL and EML4-ALK, or restoring the function of TP53 and PTEN. A major focus is engineering immune effector cells; CRISPR enhances CAR-T and NK cell therapies by knocking out inhibitory receptors (e.g., PD-1, TGFBR2) to improve persistence and cytotoxicity within the immunosuppressive TME, and facilitates the development of universal allogeneic cell products.

 

The effective delivery of CRISPR components remains a critical challenge. Viral vectors, such as AAV and lentivirus, offer high efficiency but face issues like immunogenicity and limited packaging capacity. Non-viral vectors, particularly lipid nanoparticles (LNPs), provide a safer alternative with lower immunogenicity and reduced risk of genomic integration, though their transfection efficiency needs improvement. Innovations in smart delivery systems, including microenvironment-responsive and spatiotemporally controlled nanocarriers, are being developed to enhance targeting specificity and safety.

 

In summary, the field is advancing through the development of next-generation tools like compact Cas enzymes (e.g., CasΦ, Cas12f) for easier delivery, and AI-guided sgRNA design platforms (e.g., DeepCRISPR) to optimize efficiency and minimize off-target effects. Clinical trials are already evaluating the safety and efficacy of CRISPR-edited CAR-T cells and PD-1 knockout T cells. The future of CRISPR in oncology lies in integrating it with combination therapies, multimodal editing approaches, and personalized treatment strategies informed by genomic and single-cell data, ultimately driving the transition towards smarter, safer, and more precise cancer therapeutics.

 

Extreme dry-hot in North America and Europe: the amplified role of warming-enhanced land-air coupling




Science China Press
Effect of increased GHG emissions on surface air temperature, extreme high-temperature, and aridity index. 

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a, Spatial distribution of the summer SAT (°C) difference between high- and low-emission scenarios (SSP5-8.5 and SSP1-2.6, respectively) for 2060‒2099. Vertical colored strips represent the temporal evolution of summer SAT (°C) difference between high- and low-emission scenarios over central North America (NA: 36°‒53°N, 92°‒115°W), mid-latitudes of western and central Eurasia (EUR: most of Europe and western Siberia, covering [36°‒49°N, 8°W‒30°E], [36°‒55°N, 30°‒48°E], and [48°‒55°N, 48°‒86°E]), and other regions of the world (Other) for 2015‒2099. b,c, Same as a, but for extreme high-temperature and aridity index, respectively. Red, blue, and black bars show the latitude-weighted regional averages of SAT, extreme high-temperature, and aridity index over NA, EUR, and Other for 2060‒2099. Black lines delineate the regions of NA and EUR. Areas are marked with stippling where the GHG-driven changes (SSP5-8.5 minus SSP1-2.6) are deemed robust: specifically, where at least 80% of the models project a local change greater than the global land average.

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Credit: ©Science China Press






Intensified GHG Emissions Drive Extreme Dry-Hot Extremes in North America and Europe

Although GHG are distributed relatively uniformly worldwide, the warming and climate effects they trigger exhibit significant regional differences. This phenomenon is closely linked to local climate backgrounds and feedback processes activated by rising temperatures. Our study clearly reveals that if GHG emissions remain uncontrolled, North America and Europe will experience warming amplitudes of 3.7°C ± 0.7°C and 3.8°C ± 0.5°C, respectively, by the end of the 21st century—significantly higher than the global average warming level of 2.7°C ± 0.4°C. Concurrently, the extent of drought in these two regions is projected to expand by 45.9% ± 11.9% and 13.4% ± 6.7%, respectively, highlighting the regional concentration and severity of extreme dry-hot trends.

 

Land–Air “Dry-Hot” Feedback as a Key Mechanism for Extreme Dry-Hot Conditions in North America and Europe

GHG forcing and local land–air “dry–hot” feedback are the primary drivers of the nonlinear intensification of drought and warming in North America and Europe. The study shows that enhanced land–air coupling, triggered by GHG forcing, contributes  23.0±9.8%  and  22.4±10.5%  of the total warming in North America and Europe, respectively—significantly higher than in other regions (7.9±4.5%). At the same time, land–air coupling expands the extent of drought-prone areas in North America and Europe by 44.2±18.7% and 22.6±12.6%, respectively, while this effect is nearly negligible in other regions (1.6±2.1%). The study further indicates that if the contribution of land–air coupling were excluded from GHG forcing, North America and Europe would no longer stand out as notable hotspots of warming and aridification. More importantly, the extreme dry–hot climate induced by land–air coupling is projected to significantly suppress Gross Primary Productivity (GPP): GPP in North America and Europe is expected to decrease by 27.1±20.1 and 28.8±16.9 g C·m⁻²·month⁻¹, respectively, whereas other regions remain largely unaffected. This impact would partially offset the positive effect of CO₂ fertilization on vegetation growth, weaken the ecosystem’s responsiveness to increasing GHG, and thereby heighten the risk of regional ecological degradation.

 

Physical Mechanism Behind the "Dry-Hot" Feedback

The physical mechanism through which intensified land–air coupling leads to extreme dry–hot conditions in North America and Europe can be summarized as follows: under global warming, persistent decline in soil moisture in these regions reduces actual evapotranspiration. This reduces cloud cover, thereby increasing the shortwave radiation reaching the land surface. At the same time, weakened evapotranspiration significantly alters the distribution of surface energy fluxes—latent heat flux decreases while sensible heat flux increases. Overall, the land surface receives more net energy, and a greater proportion of this energy is transferred to the atmosphere as sensible heat. These two effects jointly enhance the land surface's capacity to heat the lower atmosphere, which not only raises surface air temperatures directly but also increases potential evapotranspiration, further aggravating soil aridity and thereby sustaining a positive "dry–hot" feedback loop.

 

Outlook

The findings of this study indicate that if uncontrolled GHG emissions continue, the triggered "dry-hot" feedback will make North America and Europe the most prominent regions globally in terms of dry-hot amplification and expose them to the most severe climate risks. In fact, these regions are already frequently experiencing more intense heatwaves and flash droughts. In contrast, if stringent GHG mitigation is implemented worldwide, the warming and drying trends in these areas would be significantly alleviated, thereby delivering the greatest climate benefits. Therefore, countries in North America and Europe should be strongly motivated not only to actively advance their own emission reduction efforts but also to assist other nations in implementing climate actions, accelerating global achievement of carbon peak and carbon neutrality goals.

 

Highlights

This study is the first to clearly indicate that under an uncontrolled high-emissions scenario, GHG forcing would make North America and Europe the regions with the highest risk of extreme dry-hot events worldwide. It confirms that intensified land–air coupling is the key physical mechanism responsible for the anomalous warming and aridification in these regions, and it quantitatively assesses the magnitude of this contribution. These findings underscore the indispensable role of GHG mitigation in alleviating extreme climate disasters triggered by land–air coupling.

 

The research team, led by academician Zhang Renhe's team from Fudan University, the corresponding authors are Professor Zhiyan Zuo and Academician Renhe Zhang from the Department of Atmospheric and Oceanic Sciences at Fudan University, Associate Professor Liang Qiao from the College of Atmospheric Sciences at Lanzhou University is the first author. The co-authors include Professor Wei Mei (Department of Atmospheric and Oceanic Sciences, Fudan University), Professor Deliang Chen (Foreign Member of the Chinese Academy of Sciences, Department of Earth System Science, Tsinghua University), Ph.D. student Meiyu Chang, and postdoctoral researcher Kaiwen Zhang (both from the Department of Atmospheric and Oceanic Sciences, Fudan University).