gǔ diǎn qī（
yuē gōng yuán 250
～ 900）
mǎ yǎ wén huà jìn rù shèng qī，
gè dì jiào dà guī mó de chéng shì hé jū mín diǎn shù yǐ bǎi jì，
dōushì jù dì zì lì de chéng bāng xiǎo guó，
shàng wèi xíng chéng tǒng yī guó jiā。
gè bāng shǐ yòng gòng tóng de xiàng xíng wén zì hé lì fǎ，
chéng shì guī huá、
jiàn zhù fēng gé、
shēng chǎn shuǐ píng yě dà tǐ yī zhì。
zhù yào yí zhǐ dà duō fēn bù zài zhōng bù rè dài yǔ lín qū ,
dì kǎ '
ěr、
wǎ hā kè tōng、
bǐ dé lā sī nèi gé lā sī、
pà lún kè、
kē pān、
jī lǐ guā děng jì sì zhōng xīn yǐ xíng chéng guī mó hóng dà de jiàn zhù qún。
dì kǎ '
ěr yí zhǐ yóu shù yǐ bǎi jì de dà xiǎo jīn zì tǎ shì tái miào zǔ chéng，
qì xiàng hóng wěi，
chéng qū miàn jī dá 50
píng fāng gōng lǐ，
gū jì jū mín yòu 4
wàn zuǒ yòu。
cǐ shí chū xiàn dà liàng kè jì nián bēi míng de shí zhù，
yī bān měi gé 5
nián、 10
nián huò 20
nián jiàn lì yī zuò，
chéng wéi dú tè de jì shí zhù。 800～ 900
nián zuǒ yòu，
zhè xiē jì sì zhōng xīn tū rán fèi qì，
mǎ yǎ wén míng jí jù shuāi luò。 11
shì jì yǐ hòu，
mǎ yǎ wén míng zhōng xīn kāi shǐ zhú jiàn yí xiàng běi bù de shí huī yán dī dì píng yuán。
Early Classic
The Classic period is marked by the rise and dominance of several polities. The traditional distinction between the Early and Late Classic are marked by their changing fortune and their ability to maintain regional primacy. Of paramount importance are Teotihuacán in central Mexico and Tikal in Guatemala – indeed, the Early Classic’s temporal limits generally correlate to the main periods of these sites. Monte Alban in Oaxaca is another Classic period polity that expanded and flourished during this period, but the Zapotec capital exerted less interregional influence than the other two sites.
During the Early Classic, Teotihuacan participated in and perhaps dominated a far-reaching macro-regional interaction network. Architectural and artifact styles (talud-tablero, tripod slab-footed ceramic vessels) epitomized at Teotihuacan were mimicked and adopted at many distant settlements. Pachuca obsidian, whose trade and distribution is argued to have been economically controlled by Teotihuacan, is found throughout Mesoamerica.
Tikal came to politically, economically, and militarily dominate much of the southern Maya lowlands during the Early Classic. An exchange network centered at Tikal distributed a variety of goods and commodities throughout southeast Mesoamerica, such as obsidian imported from central Mexico (e.g., Pachuca) and highland Guatemala (e.g., El Chayal, which was predominantly used by the Maya during the Early Classic), and jade from the Motagua valley in Guatemala. Carved inscriptions at the site attest to direct interaction with individuals adorned in Teotihuacan-styled dress ca 400 AD.[citation needed] However, Tikal was often in conflict with other polities in the Petén Basin, as well as with others outside of it, including Uaxactun, Caracol, Dos Pilas, Naranjo, and Calakmul. Towards the end of the Early Classic, this conflict would lead to Tikal’s military defeat at the hands of Caracol in 562 and a period commonly known as the Tikal Hiatus.
Late Classic
The Late Classic period (beginning ca. AD 600 until AD 800/850 [varies]) is characterized as a period of interregional competition and factionalization among the numerous regional polities in the Maya area. This largely resulted from the decrease in Tikal’s socio-political and economic power at the beginning. It was during this time that a number of other sites, therefore, rose to regional prominence and were able to exert greater interregional influence, including Caracol, Copán, Palenque, and Calakmul (who was allied with Caracol and may have assisted in the defeat of Tikal), and Dos Pilas Aguateca and Cancuén in the Petexbatún region of Guatemala. Around 710 DC, Tikal arises again and started to build strong alliances and defeating its worst enemies. In the Maya area, the Late Classic ended with the so-called Maya "collapse," a transitional period coupling the general depopulation of the southern lowlands and development and fluorescence of centers in the northern lowlands.
Terminal Classic
Generally applied to the Maya area, the Terminal Classic roughly spans the time between AD 800/850 and ca. AD 1000. Overall, it generally correlates the rise to prominence of Puuc settlements in the northern Maya lowlands, so named after the hills in which they are mainly found. Puuc settlements are specifically associated with a unique architectural style (the "Puuc architectural style") that represents a technological departure from previous construction techniques. Major Puuc sites include Uxmal, Sayil, Labna, Kabah, and Oxkintok. While generally concentrating within the area in and around the Puuc hills, the style has been documented as far away as at Chichen Itza to the east and Edzna to the south.
Chichén Itzá was originally thought to have been a Postclassic site in the northern Maya lowlands. Research over the past few decades has established that it was first settled during the Early/Late Classic transition but rose to prominence during the Terminal Classic and Early Postclassic. During its apogee, this widely known site economically and politically dominated the northern lowlands. Its participation in the circum-peninsular exchange route, possible through its port site of Isla Cerritos, allowed Chichén Itzá to remain highly connected to areas such as central Mexico and Central America. The apparent “Mexicanization” of architecture at Chichén Itzá led past researchers to believe that Chichén Itzá existed under the control of a Toltec empire. Chronological data refutes this early interpretation, and it is now known that Chichén Itzá predated the Toltec; Mexican architectural styles are now used as an indicator of strong economic and ideological ties between the two regions.