古生物学报
古生物學報
고생물학보
ATCA PALAEONTOLOGICA SINICA
2001年
1期
101-115
,共15页
杨式溥%邓希光%郑祥身%刘小汉
楊式溥%鄧希光%鄭祥身%劉小漢
양식부%산희광%정상신%류소한
遗迹化石晚三叠世复理石相利文斯顿岛南极
遺跡化石晚三疊世複理石相利文斯頓島南極
유적화석만삼첩세복리석상리문사돈도남겁
南极利文斯顿岛赫德半岛中的迈尔斯陡崖组主要是浅变质的石英长石杂砂岩、粉砂岩、泥岩和粉砂岩
与泥岩互层等组成的复理石,厚度可能超过3 000 m,形成于浊积扇的上扇和下扇部分,时代可能为晚三叠世。在
复理石相岩石中发育一套深水的遗迹化石,共有15个遗迹属、16个遗迹种,其中有10个可以鉴定到遗迹种、两个
比较种,4个只鉴定到遗迹属,未鉴定到遗迹种;建立1个新遗迹属及新遗迹种,除新遗迹属种外,其余14个遗迹
属,15个遗迹种都曾经在深海复理石相浊积岩内发现过,其中
Belorhaphe, Glockerichnus, Lophoctenium, Rhabdo
glyphus, Paleodictyon , Sublorenzinia , Spirophycus , Strobilorhaphe, Tuberculichnus , Cochlichnus
等,属于浊流前产
生在复理石相泥岩内的高度分异的雕画迹(Graphoglyptida),它们产于泥岩却保存为上覆砂岩底面的铸型凸起。另
外Fucusopsis和Neonereites却产生在砂岩内代表浊流后形成的沉积后遗迹组合。文内还描述3种浊流常见的无机
构造,并与上述遗迹化石进行比较。
南極利文斯頓島赫德半島中的邁爾斯陡崖組主要是淺變質的石英長石雜砂巖、粉砂巖、泥巖和粉砂巖
與泥巖互層等組成的複理石,厚度可能超過3 000 m,形成于濁積扇的上扇和下扇部分,時代可能為晚三疊世。在
複理石相巖石中髮育一套深水的遺跡化石,共有15箇遺跡屬、16箇遺跡種,其中有10箇可以鑒定到遺跡種、兩箇
比較種,4箇隻鑒定到遺跡屬,未鑒定到遺跡種;建立1箇新遺跡屬及新遺跡種,除新遺跡屬種外,其餘14箇遺跡
屬,15箇遺跡種都曾經在深海複理石相濁積巖內髮現過,其中
Belorhaphe, Glockerichnus, Lophoctenium, Rhabdo
glyphus, Paleodictyon , Sublorenzinia , Spirophycus , Strobilorhaphe, Tuberculichnus , Cochlichnus
等,屬于濁流前產
生在複理石相泥巖內的高度分異的彫畫跡(Graphoglyptida),它們產于泥巖卻保存為上覆砂巖底麵的鑄型凸起。另
外Fucusopsis和Neonereites卻產生在砂巖內代錶濁流後形成的沉積後遺跡組閤。文內還描述3種濁流常見的無機
構造,併與上述遺跡化石進行比較。
남겁리문사돈도혁덕반도중적매이사두애조주요시천변질적석영장석잡사암、분사암、니암화분사암
여니암호층등조성적복리석,후도가능초과3 000 m,형성우탁적선적상선화하선부분,시대가능위만삼첩세。재
복리석상암석중발육일투심수적유적화석,공유15개유적속、16개유적충,기중유10개가이감정도유적충、량개
비교충,4개지감정도유적속,미감정도유적충;건립1개신유적속급신유적충,제신유적속충외,기여14개유적
속,15개유적충도증경재심해복리석상탁적암내발현과,기중
Belorhaphe, Glockerichnus, Lophoctenium, Rhabdo
glyphus, Paleodictyon , Sublorenzinia , Spirophycus , Strobilorhaphe, Tuberculichnus , Cochlichnus
등,속우탁류전산
생재복리석상니암내적고도분이적조화적(Graphoglyptida),타문산우니암각보존위상복사암저면적주형철기。령
외Fucusopsis화Neonereites각산생재사암내대표탁류후형성적침적후유적조합。문내환묘술3충탁류상견적무궤
구조,병여상술유적화석진행비교。
The Miers Bluff Formation on Hurd Peninsula, Liv
ingston Island, West Antarctica, contains low-grade
metamorphic grey-wacke, arkose sandstone, shales, con
glomerate, pebbly mudstone and breccias and has been in
terpreted to be a sequence of turbidites. It may represent
sedimentation of upper and lower mid-fan settings. Its
thick is more than 3 000 meters (base unknown). Its de
positional age has been palynologically dated as Late Trias
sic (Ouyang et al., 2000). Many trace fossils of the
whole succession were found in the turbidites of the Miers
Bluff Formation. All these are deep sea ichnofossils. Fif
teen ichnogenus and sixteen ichnospecies are recongnized.
They are Belorhaphe ichnosp., Cochlichnus ichonosp. ,
Fucusopsis annulata Palibin, Glockerichnus ichnosp.,
Halyminidium sublumbricoides ( Azpeitia ), Lophocteni
um comosum Richter, Neonereites uniserialis Seilacher,
Paleodictyon ichnosp. , Paleaichnus antarctics ichnogen.
et ichnosp. nov., Planolites montanus Richter, Rhabdo
glyphus grossheimi Vassoevich, Spirophycus bicornis
Heer, Strobilorhaphe ichnosp. , Sublorenzinia cf. plana
Ksiazkiewicz, Tuberculichnus meandrinus Ksiazkiewicz
and Tuberculichnus bulbosus Ksiazkiewicz. We found a
new trace fossil and propose a new ichnogenus and new
ichnospecies-Paleaichnus antarcticus ichnogen. et ich
nosp. nov. Except the new ichnogenus and ichnospecies,
others had been found in deep-sea flysch turbidites. Some
are in mudstone and preserved in the cast convex of over
lying sandstone sole. They formed before turbidity flows
and belong to the high-different Graphoglyptidas of flysch
mudstone, for example Belorhaphe, Glockerichnus,
Lophoctenium , Rhabdoglyphus , Paleodictyon ,
Sublorenzinia , Spirophycus , Strobilorhaphe , Tuber
culichnus and Cochlichnus et al. Others as Fucusopsis and
Neonereites are preserved in sandstones and stand for trace
assemblages after turbidity sedimentation. In addition, the
paper also discussed three common inorganic structures in
turbidity flow and compared with the above-mentioned
trace fossils.