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We report a world record of lidar profiling of metallic Ca+ions up to 300 km in the midlatitude nighttime ionosphere during geomagnetic quiet time. Ca+measurements (∼80–300 km) were made over Beijing (40.42°N, 116.02°E) with an Optical‐Parametric‐Oscillator‐based lidar from March 2020 through June 2021. Main Ca+layers (80–100 km) persist through all nights, and high‐density sporadic Ca+layers (∼100–120 km) frequently occur in summer. Thermosphere‐ionosphere Ca+(TICa+) layers (∼110–300 km) are likely formed via Ca+uplifting from these sporadic layers. The lidar observations capture the complete evolution of TICa+layers from onset to ending, revealing intriguing features. Concurrent ionosonde measurements show strong sporadic E layers developed before TICa+and spread F onset. Neutral winds can partially account for observed vertical transport but enhanced electric fields are required to explain the results. Such lidar observations promise new insights into E‐ and F‐region coupling and plasma inhomogeneities. Inhomogeneities (also called irregularities) in the ionospheric plasma distribution can significantly degrade satellite communications and negatively impact Global Positioning System‐based navigation systems that rely on the trans‐ionospheric radio‐wave propagation. Understanding the formation mechanisms of, thus predicting, ionospheric inhomogeneities is still a huge challenge in space weather research. Long‐lived meteoric metal ions (≫$\gg $1 day above 100 km altitude) converge to form dense ion layers, causing plasma irregularities in the ionosphere. Therefore, it is imperative to observe and understand the transport and formation of metallic ion layers. However, it is technically challenging to detect specific ion species, especially tracing ion transport over large vertical ranges and time durations. Numerous instruments detect electron density but cannot distinguish ion species. Rocket‐borne mass spectrometers can distinguish ion species but provide only snapshots. Lidars provide a powerful tool to profile and trace metallic species over extended periods by exciting specific resonance fluorescence. The only metal ions detectable by ground‐based lidars are Ca+, and previous lidar measurements reached ∼180 km. Our Ca+lidar upgraded with narrowband lasers has achieved high detection sensitivity, enabling the Ca+profiling up to 300 km. Such lidar measurements of dynamical Ca+layers open a new window to study plasma irregularities. First lidar profiling of Ca+ions from ∼80 to 300 km was made over Beijing in the nighttime ionosphere during geomagnetic quiet timeThermosphere‐ionosphere Ca+layers (∼10 s cm−3) are likely formed by uplifting ions from sporadic Ca+at ∼110 km & show complex structuresSpread F occurs concurrently with Thermosphere‐ionosphere Ca+& strong sporadic E layers occur before the onset of TICa+and spread F, suggesting E‐ and F‐region coupling First lidar profiling of Ca+ions from ∼80 to 300 km was made over Beijing in the nighttime ionosphere during geomagnetic quiet time Thermosphere‐ionosphere Ca+layers (∼10 s cm−3) are likely formed by uplifting ions from sporadic Ca+at ∼110 km & show complex structures Spread F occurs concurrently with Thermosphere‐ionosphere Ca+& strong sporadic E layers occur before the onset of TICa+and spread F, suggesting E‐ and F‐region coupling