耐梅蓋特層

耐梅蓋特層（Nemegt Formation／Nemegtskaya Svita）是蒙古戈壁沙漠晚白堊世的一個沉積層。由河道沉積物構成，出產魚、龜、鱷及高多樣性的恐龍（含鳥類）化石。 耐梅蓋特層由古湖泊、溪流、氾濫平原沉積的泥岩和砂岩所構成。邁可·諾瓦切克（Michael Novacek）形容奧譚烏爾（Altan Uul）地區為「由一系列蘊含豐富的沉積岩雕琢而成的峽谷，並具有陡峭懸崖及狹窄沖刷」。該地層氣候與其下較老的地層相比起來濕潤程度更高，似乎至少曾有一定程度的森林覆蓋；已發現許多化石化的樹幹；這些石化木和南洋杉科針葉樹的遺骸，顯示耐梅蓋特曾經樹林茂密，高聳針葉樹形成廣闊的樹冠層。透過檢驗發現其岩相顯示出溪流、河道、泥灘、淺湖的存在，沉積物也表明這裡蘊含資源豐富的棲地，提供多樣化且充沛的食物來源，足以維持大量白堊紀恐龍物種的生存。 近期地層研究將耐梅蓋特區分為三段（非正式）層位。下部層位以河流沉積為主，中、上部層位由沖積平原、沼澤、湖積（英语：Lacustrine deposits）、河道沉積構成。相較於其下方的西戈約特層為典型的紅色，耐梅蓋特沉積物的顏色通常介於淺灰色至棕褐色。耐梅蓋特覆蓋於西戈約特之上並有時互接，在層型（紅牆）與赫明察夫（Hermiin Tsav）位點可觀察到互接狀況。耐梅蓋特層並沒有明確的年代定義。研究史上，根據所產化石的比較來推測，耐梅蓋特層應該介於坎潘期之末至馬斯垂克期，但更精確的定年檢驗從未執行。底下的西戈約特層年代估計為桑托期至坎潘期，而Shuvalov（2000）對其玄武岩進行鉀氬定年法的結果顯示西戈約特層中上部層位的年代約落在7500萬至8000萬年前。 層位參照Eberth（2018）的定義，他將各地區與在岩層中的大致位置關聯起來。 發現一種非常大型的泰坦巨龍類足跡，非正式稱呼為「蒙古巨龍」（Mongolian titan）。 德加多克塔層（英语：Djadochta Formation） 出產恐龍的地層列表（英语：List of dinosaur-bearing rock formations） 化石點列表（英语：List of fossil sites） 耐梅蓋特盆地（英语：Nemegt Basin） Novacek, M. (1996). Dinosaurs of the Flaming Cliffs. 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