Ecological variations in diatom assemblages in the Paleo-Kathmandu Lake linked with global and Indian monsoon climate changes for the last 600,000 years

Tatsuya Hayashi, Yoshihiro Tanimura, Yoshihiro Kuwahara, Masao Ohno, Mami Mampuku, Rie Fujii, Harutaka Sakai, Toshiro Yamanaka, Takeshi Maki, Masao Uchida, Wataru Yahagi, Hideo Sakai

Research output: Contribution to journalArticle

11 Citations (Scopus)

Abstract

Variations in fossil diatom assemblages and their relationship with global and Indian monsoon climate changes for the last 600,000 yr were investigated using a core of ancient lake (Paleo-Kathmandu Lake) sediments drilled at the Kathmandu Basin, Nepal Himalaya. Chronological scales of the core were constructed by tuning pollen wet and dry index records to the SPECMAP δ18O stack record. Examinations of biogenic silica contents and fossil diatom assemblages revealed that variations in productivity and compositions of diatom assemblages were closely linked with global and Indian monsoon climate changes on glacial and interglacial time scales. When summer monsoonal rainfall increased during interglacials (interstadials), diatom productivity increased because of increased inputs of terrestrial nutrients into the lake. When summer monsoonal rainfall reduced and/or winter monsoonal aridification enhanced during glacials (stadials), productivity of the diatoms decreased and lake-level falling brought about changes in compositions of diatom assemblages. Monospecific assemblages by unique Cyclotella kathmanduensis and Puncticulata versiformis appeared during about 590 to 390 ka. This might be attributed to evolutionary fine-tuning of diatom assemblages to specific lake environmental conditions. Additionally, low-amplitude precessional variations in monsoon climate and less lake-level changes may have also allowed both species to dominate over the long periods.

Original languageEnglish
Pages (from-to)377-387
Number of pages11
JournalQuaternary Research
Volume72
Issue number3
DOIs
Publication statusPublished - Nov 1 2009

Fingerprint

monsoon
diatom
climate change
lake
lake level
productivity
fossil
aridification
rainfall
interstadial
summer
Diatoms
Climate Change
Assemblages
interglacial
lacustrine deposit
pollen
silica
environmental conditions
timescale

All Science Journal Classification (ASJC) codes

  • Arts and Humanities (miscellaneous)
  • Earth-Surface Processes
  • Earth and Planetary Sciences(all)

Cite this

Ecological variations in diatom assemblages in the Paleo-Kathmandu Lake linked with global and Indian monsoon climate changes for the last 600,000 years. / Hayashi, Tatsuya; Tanimura, Yoshihiro; Kuwahara, Yoshihiro; Ohno, Masao; Mampuku, Mami; Fujii, Rie; Sakai, Harutaka; Yamanaka, Toshiro; Maki, Takeshi; Uchida, Masao; Yahagi, Wataru; Sakai, Hideo.

In: Quaternary Research, Vol. 72, No. 3, 01.11.2009, p. 377-387.

Research output: Contribution to journalArticle

Hayashi, Tatsuya ; Tanimura, Yoshihiro ; Kuwahara, Yoshihiro ; Ohno, Masao ; Mampuku, Mami ; Fujii, Rie ; Sakai, Harutaka ; Yamanaka, Toshiro ; Maki, Takeshi ; Uchida, Masao ; Yahagi, Wataru ; Sakai, Hideo. / Ecological variations in diatom assemblages in the Paleo-Kathmandu Lake linked with global and Indian monsoon climate changes for the last 600,000 years. In: Quaternary Research. 2009 ; Vol. 72, No. 3. pp. 377-387.
@article{69179f5b816546028c02e036073c2a17,
title = "Ecological variations in diatom assemblages in the Paleo-Kathmandu Lake linked with global and Indian monsoon climate changes for the last 600,000 years",
abstract = "Variations in fossil diatom assemblages and their relationship with global and Indian monsoon climate changes for the last 600,000 yr were investigated using a core of ancient lake (Paleo-Kathmandu Lake) sediments drilled at the Kathmandu Basin, Nepal Himalaya. Chronological scales of the core were constructed by tuning pollen wet and dry index records to the SPECMAP δ18O stack record. Examinations of biogenic silica contents and fossil diatom assemblages revealed that variations in productivity and compositions of diatom assemblages were closely linked with global and Indian monsoon climate changes on glacial and interglacial time scales. When summer monsoonal rainfall increased during interglacials (interstadials), diatom productivity increased because of increased inputs of terrestrial nutrients into the lake. When summer monsoonal rainfall reduced and/or winter monsoonal aridification enhanced during glacials (stadials), productivity of the diatoms decreased and lake-level falling brought about changes in compositions of diatom assemblages. Monospecific assemblages by unique Cyclotella kathmanduensis and Puncticulata versiformis appeared during about 590 to 390 ka. This might be attributed to evolutionary fine-tuning of diatom assemblages to specific lake environmental conditions. Additionally, low-amplitude precessional variations in monsoon climate and less lake-level changes may have also allowed both species to dominate over the long periods.",
author = "Tatsuya Hayashi and Yoshihiro Tanimura and Yoshihiro Kuwahara and Masao Ohno and Mami Mampuku and Rie Fujii and Harutaka Sakai and Toshiro Yamanaka and Takeshi Maki and Masao Uchida and Wataru Yahagi and Hideo Sakai",
year = "2009",
month = "11",
day = "1",
doi = "10.1016/j.yqres.2009.07.003",
language = "English",
volume = "72",
pages = "377--387",
journal = "Quaternary Research",
issn = "0033-5894",
publisher = "Academic Press Inc.",
number = "3",

}

TY - JOUR

T1 - Ecological variations in diatom assemblages in the Paleo-Kathmandu Lake linked with global and Indian monsoon climate changes for the last 600,000 years

AU - Hayashi, Tatsuya

AU - Tanimura, Yoshihiro

AU - Kuwahara, Yoshihiro

AU - Ohno, Masao

AU - Mampuku, Mami

AU - Fujii, Rie

AU - Sakai, Harutaka

AU - Yamanaka, Toshiro

AU - Maki, Takeshi

AU - Uchida, Masao

AU - Yahagi, Wataru

AU - Sakai, Hideo

PY - 2009/11/1

Y1 - 2009/11/1

N2 - Variations in fossil diatom assemblages and their relationship with global and Indian monsoon climate changes for the last 600,000 yr were investigated using a core of ancient lake (Paleo-Kathmandu Lake) sediments drilled at the Kathmandu Basin, Nepal Himalaya. Chronological scales of the core were constructed by tuning pollen wet and dry index records to the SPECMAP δ18O stack record. Examinations of biogenic silica contents and fossil diatom assemblages revealed that variations in productivity and compositions of diatom assemblages were closely linked with global and Indian monsoon climate changes on glacial and interglacial time scales. When summer monsoonal rainfall increased during interglacials (interstadials), diatom productivity increased because of increased inputs of terrestrial nutrients into the lake. When summer monsoonal rainfall reduced and/or winter monsoonal aridification enhanced during glacials (stadials), productivity of the diatoms decreased and lake-level falling brought about changes in compositions of diatom assemblages. Monospecific assemblages by unique Cyclotella kathmanduensis and Puncticulata versiformis appeared during about 590 to 390 ka. This might be attributed to evolutionary fine-tuning of diatom assemblages to specific lake environmental conditions. Additionally, low-amplitude precessional variations in monsoon climate and less lake-level changes may have also allowed both species to dominate over the long periods.

AB - Variations in fossil diatom assemblages and their relationship with global and Indian monsoon climate changes for the last 600,000 yr were investigated using a core of ancient lake (Paleo-Kathmandu Lake) sediments drilled at the Kathmandu Basin, Nepal Himalaya. Chronological scales of the core were constructed by tuning pollen wet and dry index records to the SPECMAP δ18O stack record. Examinations of biogenic silica contents and fossil diatom assemblages revealed that variations in productivity and compositions of diatom assemblages were closely linked with global and Indian monsoon climate changes on glacial and interglacial time scales. When summer monsoonal rainfall increased during interglacials (interstadials), diatom productivity increased because of increased inputs of terrestrial nutrients into the lake. When summer monsoonal rainfall reduced and/or winter monsoonal aridification enhanced during glacials (stadials), productivity of the diatoms decreased and lake-level falling brought about changes in compositions of diatom assemblages. Monospecific assemblages by unique Cyclotella kathmanduensis and Puncticulata versiformis appeared during about 590 to 390 ka. This might be attributed to evolutionary fine-tuning of diatom assemblages to specific lake environmental conditions. Additionally, low-amplitude precessional variations in monsoon climate and less lake-level changes may have also allowed both species to dominate over the long periods.

UR - http://www.scopus.com/inward/record.url?scp=70349973701&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=70349973701&partnerID=8YFLogxK

U2 - 10.1016/j.yqres.2009.07.003

DO - 10.1016/j.yqres.2009.07.003

M3 - Article

VL - 72

SP - 377

EP - 387

JO - Quaternary Research

JF - Quaternary Research

SN - 0033-5894

IS - 3

ER -