Oxic Horizon - Soil Geography of the USA: A Diagnostic-Horizon Approach - page 211

Table 19.2 Soil series with an oxic horizon in the USA and its territories
Order Suborder Great group Subgroup Series

Andisols Udands Hapludands Oxic Paaiki

Inceptisols Udepts Dystrudepts Oxic Alonso, Hihimanu

Ustepts Dystrustepts Oxic Haliimaile, Kahana, Kolekole, Kunia

Haplustepts Oxic Dandan, Hoolehua, Pakala, Pohakupu

Oxisols Aquox Haplaquox Plinthic Sabana Seca

Perox Acroperox Anionic Halii, Umpump

Typic Ngardok. Ofu, Rakied

Plinthic Wahrekdam

Eutroperox Typic Yap

Haploperox Typic Gagil, Ngatpang, Palau

Kandiperox Typic Aimeliik, Babelthuap

Aquic Tabecheding

Torrox Eutrotorrox Typic Holomua, Molokai

Haplotorrox Typic Uwala

Udox Acrudox Rhodic Kaneohe

Anionic Kapaa, Makapili, Pooku

Typic Nipe

Hapludox Inceptic Adjuntas, Daguey, Rosario

Plinthic Almirante

Typic Bayamon, Catalina, Kunuweia, Lawai

Xanthic Consejo

Rhodic Delicias

Humic Los Guineos, Yunque

Kandiudox Humic Hanamaulu

Typic Limones

Humic Rhodic Paaloa

Ustox Acrustox Eutric Yigo

Eutrustox Lithic Cotito, Matanzas

Typic Coto

Rhodic Helemano, Lahaina, Lihue, Niu

Kandiustalfic Kagman, Laolao, Saipan

Haplustox Inceptic Akina, Mahana

Rhodic Wahiawa

Kandiustox Humic Puhi

positions. The oxic horizon is more developed on basic and ultrabasic materials
than in tuffs or limestone; however, many Oxisols in Brazil occur on ferruginized
sandstone materials. Oxisols appear to be generally of pre-Quaternary age,
and many soils with an oxic horizon occur on landforms of Tertiary age. Many
Oxisols are polygenetic and have undergone substantial climate change over
geologic time (Muggler and Buurman 2000 ;Quesadaetal. 2011 )(Tables 19.2
and 19.3 ).