Watermelon, Citrullus lanatus, is an important cucurbit crop grown throughout the world. Here we report a high-quality draft genome sequence of the east Asia watermelon cultivar 97103 (2n = 2x = 22) containing 23,440 predicted protein-coding genes. Comparative genomics analysis provided an evolutionary scenario for the origin of the 11 watermelon chromosomes derived from a 7-chromosome paleohexaploid eudicot ancestor. Resequencing of 20 watermelon accessions representing three different C. lanatus subspecies produced numerous haplotypes and identified the extent of genetic diversity and population structure of watermelon germplasm. Genomic regions that were preferentially selected during domestication were identified. Many disease-resistance genes were also found to be lost during domestication. In addition, integrative genomic and transcriptomic analyses yielded important insights into aspects of phloem-based vascular signaling in common between watermelon and cucumber and identified genes crucial to valuable fruit-quality traits, including sugar accumulation and citrulline metabolism
Fruit characteristics of sweet watermelon are largely the result of human selection. Here we report an improved watermelon reference genome and whole-genome resequencing of 414 accessions representing all extant species in the Citrullus genus. Population genomic analyses reveal the evolutionary history of Citrullus, suggesting independent evolutions in Citrullus amarus and the lineage containing Citrullus lanatus and Citrullus mucosospermus. Our findings indicate that different loci affecting watermelon fruit size have been under selection during speciation, domestication and improvement. A non-bitter allele, arising in the progenitor of sweet watermelon, is largely fixed in C. lanatus. Selection for flesh sweetness started in the progenitor of C. lanatus and continues through modern breeding on loci controlling raffinose catabolism and sugar transport. Fruit flesh coloration and sugar accumulation might have co-evolved through shared genetic components including a sugar transporter gene. This study provides valuable genomic resources and sheds light on watermelon speciation and breeding history.
Oxygen isotopic ratios (5180) of precipitation samples collected over several years at three meteorological stations on the northern Tibetan Plateau were used to conduct the first investigation of the relationship between i•lgO and contemporaneous air temperatures (To). Inferring past temperatures from i•180 measured in recently acquired Tibetan ice cores necessitates establishing whether a i•lgO-To relationship exists. For each station a strong temporal relationship is found between i•180 and To, particularly for monthly averages which remove synoptic-scale influences such as changes in condensation level, condensation temperature, and moisture sources. Moisture source is identified as a major factor in the spatial distribution of i•180, but air temperature determines the temporal fluctuations of i•lSO at individual sites on the northern Tibetan Plateau. The 30-year records of annually averaged i•lSO from three different ice coring sites are not correlated significantly with contemporaneous air temperature records from their closest meteorological station (150 to 200 km). However, since 1960 the three air temperature records reveal a modest warming trend, while the three contemporaneous i•lSO records show a modest •O enrichment. 1. Introduction Oxygen isotopic ratios (5•80) have been used extensively in palcoclimatic reconstructions [Dansgaard, 1953; Craig, 1961; Lorius et al., 1985; Thompson et al., 1989, 1995a; Yao et al., 1991; Jouzel et al., 1994] as a proxy for air temperature. The relationship between •80 and air temperature (To) has been investigated most thoroughly in the polar regions. In Antarctica, various studies [Aldaz and Deutsch, 1967; Lorius and Merlivat, 1977; Kotlyakov et al., 1982; Jouzel and Merlivat, 1984; Mosley-Thompson et al., 1990; Peel, 1992] have demonstrated a strong linear relationship between •O and To with slopes ranging from 0.76 to 0.92. In Greenland snow, Dansgaard et al. [1973] and Johnsen et al. [1989] obtained slopes from 0.62 to 0.67. Palcoclimatic reconstructions rely on the robustness of the assumption that the 5•80-To relationship can be used to reconstruct accurately the climatic record (e.g,. temperature trends) preserved in ice cores [Jouzel et a/.,1983]. A recent study by Joussaume and Jouzel [1993] demonstrated that using currently measured 5•O-To relationships to reconstruct temporal variations in To from 5•O may result in errors of 20% to 30% over Greenland and Antarctica. Outside the polar regions these studies are more limited. A comprehensive study of the long-term 5•80-To relationship was conducted in midlatitude, low-elevation regions {Rozanski et al., 1992] using the relatively long •O and meteorological records from stations in the International Atomic Energy Agency (IAEA)/World Meteorological Organization (WMO) precipitation network. Three different changes in the 5•O-To relationship were identified: spatial changes, short-term changes, and long-term changes. Spatially, the 5l•O/Ta slope values varied from 0.719/oo per
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.
hi@scite.ai
10624 S. Eastern Ave., Ste. A-614
Henderson, NV 89052, USA
Copyright © 2024 scite LLC. All rights reserved.
Made with 💙 for researchers
Part of the Research Solutions Family.