اخترزیست‌شناسی

از ویکی‌پدیا، دانشنامهٔ آزاد
پرش به: ناوبری، جستجو
فارسی English

اخترزیست‌شناسی یا دگرزیست‌شناسی نام رشتهٔ پژوهشی‌ای در زیست‌شناسی است که به بررسی امکان زیست فرازمینی می‌پردازد. اخترزیست‌شناسان به مطالعهٔ خاستگاه، تکامل و پراکنش زیست در کیهان می‌پردازند. این رشته برای اولین بار در ماه می ۱۹۹۸ توسط سازمان ناسا با ایجاد انیستیتوی آستروبیولوژی در مرکز تحقیقات ایمز (Ames) بنیان‌گذاری شد. در حقیقت اختر زیست‌شناسی حوزه تحقیق مشخصی ندارد، می‌توان گفت آن تلفیقی از چندین حوزه علمی می‌باشد که کاوش حیات برون زمینی و مطالعه دربارهٔ دیگر سیارات منظومه شمسی و قمرهایشان از منظر زیست‌شناسی، وضعیت حیاتی فضانوردان در شرایط خارج از زمین و نیز پی بردن به اینکه حیات روی زمین از کجا منشا گرفته است از وظایف اخترزیست‌شناسی است.

اهداف و دستاوردها[ویرایش]

اختر زیست‌شناسی تنها با تکیه بر دستاوردهای علمی اخیر بطور شایسته‌ای گام به جلو برداشته است. این دانش به ما اجازه می‌دهد تا یافته‌های مربوط به اخترشناسی و زیست‌شناسی را در کنار هم بتوانیم بررسی کنیم. یک نمونه عالی از دستاوردهای اخترزیست‌شناسی را می‌توان در ماموریت‌های مریخ نوردان دانست که توانستند داده‌های بسیاری از شرایط محیطی حاکم بر مریخ نظیر ویژگی‌های جوی، شیمیایی، دما و سایر موارد جمع آوری و به زمین مخابره نمایند. تحقیقات انجام شده بر روی شدت دوست(اکستروموفیل)ها، یعنی موجودات زنده‌ای که شرایط سخت مثل دمای بالا و پائین و فشارهای غیر متعارف برای حیات را ترجیح می‌دهند، اطلاعات تکان دهنده‌ای از میزان تنوع این موجودات به ما داده است. این اطلاعات ما را به فکر فرو می‌برد که زندگی تقریبا در تمامی مکان‌های کره زمین در جریان است. ترکیب دو علم اخترشناسی و زیست‌شناسی منجر به پی بردن به این حقیقت شده است که برخی میکروبها قطعا می‌توانند در محیط کره مریخ بقا یابند. ولی با این حال هنوز موجود دارای حیاتی روی مریخ یافت نشده است. اخترزیست‌شناسی همچنین در پی یافت مکانهایی است که حیات را در خود جای داده‌اند. این دانش سوالات مهمی مطرح می‌کند:

  • منشا حیات در زمین چیست؟
  • چرا تا کنون موجود زنده‌ای در سایر سیارات یافت نشده است؟
  • آیا حیات قبلا در سیارات نابود شده است؟
  • آیا ما در این جهان تنها هستیم؟ اگر اینگونه است، چرا؟

بخش‌های اخترزیست‌شناسی[ویرایش]

علم اخترزیست‌شناسی به چهار حوزه تقسیم می‌شود:

برون زیست‌شناسی[ویرایش]

برون زیست‌شناسی یا اگزوبیولوژی حوزه‌ای از دانش اخترزیست‌شناسی است که به مطالعه واکنش‌های حیاتی، زیست‌شناسی مولکولی و چگونگی ساز و کارهای زیستی در شرایط فضا و دیگر سیارات می‌پردازد. اینکه حیات در فضا و دیگر سیارات به چه شکلی است، چه رفتاری دارد و در چه مکان‌هایی از فضا می‌تواند شکل گیرد از سوالاتی است که برون زیست‌شناسی در جستجوی پاسخ به آن است.

نگاره الکترونی از میکرو فسیل‌هایی از باکتریهای موجود در شهاب سنگ مریخی ALH۸۴۰۰۱، احتمال می‌رود اولین ترکیبات آلی حیات توسط شهاب سنگها وارد زمین شده باشند.

زیست‌شناسی سیاره‌ای[ویرایش]

یکی از اهداف اخترزیست‌شناسی بررسی زیست‌شناسی در مقیاس سیارات است. با زیست‌شناسی سیاره‌ای می‌توان نمونه‌های اتمسفر و سنگ‌های دیگر سیارات را به منظور یافتن ترکیبات آلی و فسیل باکتری‌ها بررسی کنیم. نتایج بدست آمده از مطالعات روی کندریت‌هایی با بیش از ۵ درصد کربن این انگیزه را به ما داده است تا فرضیه مواد آلی فرازمینی را به بوته آزمایش بگذاریم. یکی از این کندریت‌ها شهاب سنگی بنام "مارکیسون" (Murchison) است که در سال ۱۹۶۹ در دهکده‌ای به همین نام در استرالیا کشف شد. این شهاب سنگ در حال حاضر مشهورترین سنگ آسمانی در روی زمین است. مارکیسون در همان مطالعات اولیه دانشمندان را در بهت و حیرت فراوان فروبرد، چرا که درون آن بیش از هشتاد نوع اسید آمینه مختلف با میزان بیش از یک قسمت در میلیون (ppm) شناسایی شد. هشت نوع از این مولکول‌ها جزو مولکول‌هایی هستند که اجزای اصلی پروتئین‌ها و آنزیم‌ها موجود در زمین را تشکیل می‌دهند. طی کنکاش لایه‌های یخی قطب جنوب کلکسیونی از قطعات شهاب سنگی یافت شده است که حاوی مولکول‌های قند و بازهای نوکلئیک بوده‌اند. این یافته‌ها نظریه حیات فرازمینی را در اذهان بشدت تقویت کرد. نکته حائز اهمیت تر خرده شهاب‌های یافت شده در قطب جنوب اینست که بسیاری از قطعات با اندازه بین ۱۰۰ تا ۵۰۰ میکرومتر کندریت‌های ذوب نشده هستند. یعنی توانستند بدون دریافت فشار و شوک حرارتی از جو زمین عبور کنند. دانشمندان احتمال می‌دهند این سنگها زمانی وارد سیاره ما شده‌اند که زمین همچنان فاقد اتمسفر بوده است. در فوریه ۲۰۰۶ فضاپیمای Stardust متعلق به ناسا نمونه‌هایی از غبار مربوط به دنباله دارها را از آنسوی مدار ماه به زمین آورد. دانشمندان توانستند به حقایق ارزشمندی از ترکیب این سنگ‌های سرگردان دست یابند. تخمین زده می‌شود طی ۶۰۰ میلیون سال گذشته ۱۰۲۰ گرم کربن از فضا وارد زمین شده است، این مقدار از کل میزان کربن توده زنده کره زمین بیشتر است. اکنون ما می دانیم منبع اصلی مواد آلی که امروزه در پیکره جانداران وجود دارد نه بطن کره زمین بلکه فضای ماورای اتمسفر آن می‌باشد. اما سوالی که پدید می‌آید اینست که اگر شهاب سنگها می‌توانند این همه مولکول آلی را وارد زمین کنند، چرا نتوانند خود موجودات زنده را به زمین آورند. البته بایستی خاطر نشان کرد اکثر اجرام فضایی تا هنگام ورود به زمین شرایط بسیار رنج آوری را تجربه می‌کنند. پی بردن به اینکه موجودات دارای حیات چگونه می‌توانند در این شرایط دشوار زنده بمانند اولین گام برای بحث در مورد انتقال بین سیاره‌ای ارگانیسم هاست. شرایط زندگی در فضا و کرات دیگر به مراتب دشوارتر از هر زیستگاه بحرانی است که در روی زمین می‌توان سراغ داشت. ازاینرو باید آزمایش‌ها مداومی برای سنجیدن میزان انعطاف و تحمل پذیری اشکال حیاتی زمین در محیط‌های مشابه سایر سیارات انجام گیرد تا به یک روشنگری کلی در مورد میزان قابلیت بقا در شرایط فرازمینی دست پیدا کنیم. راه دیگر انتقال حیات از سیارات مادری به سایر مکان‌های فضایی موجودات هوشمندی هستند که از فن آوری‌های پیشرفته مسافرت‌های بین سیاره‌ای برخوردارند، چیزی که ما آنرا سفینه‌های سرنشین دار می‌نامیم. تقریباً تمام زیستگاه‌های کره زمین با موجودات زنده اشغال شده‌اند. شاید در میان این موجودات انواعی باشند که قادرند برای یافتن هدف غائی خود و شکوفایی بیشتر راه فضا و دنیاهای دیگر را در پیش گیرند.

منشاء حیات[ویرایش]

فرضیه‌ای تحت عنوان پان اسپرمیا ادعا می‌کند بذرهای حیات برای اولین بار از فضا و دیگر سیارات توسط شهاب سنگها به زمین آورده شده است. یکی دیگر از وظایف اخترزیست‌شناسی بررسی این موضوع می‌باشد. ایده امکان تشکیل حیات در روی زمین بواسطه ورود مولکول‌های آلی از آنسوی فضا بسیار جالب توجه است. تجزیه و تحلیل قطعات بدست آمده از شهاب سنگ‌های کربن دار این نظر را اثبات می‌کند که برخی مولکول‌های عالی نظیر آمینو اسیدها در محیط خارج از کره زمین تشکیل شده‌اند. طبق مشاهدات نجومی این مولکول‌های آلی بسیار پیش تر از آنکه منظومه شمسی شروع به تشکیل کند درون اجرام فضایی کوچکتر مثل سیارکها و دنباله دارها بوجود آمده‌اند. با وجود دمای بالای سیارات در ادوار شکل گیری آنها مولکول‌های اساسی حیات نمی‌توانستند تشکیل شوند یا از شرایط دشوار حاکم برآن جان سالم بدر برند. بنابراین این مولکول‌های مهم یا بعدها در اتمسفر سرد شده آنها متولد شده‌اند یا توسط سیارکها، شهاب سنگها و غبار بین سیاره‌ای وارد زمین گشته‌اند.

آینده انسان در فضا[ویرایش]

بطور کلی ترسیم آینده‌ای از جایگاه انسان در فضا بستگی به موفقیت‌هایی است که در حوزه اخترشناسی و اخترزیست‌شناسی بدست می‌آیند. آموزش فلسفه حقیقی کاوش‌های فضایی و آماده نمودن انسان‌ها برای رویارویی با هر کشف جدید از ضروریات علم اخترزیست‌شناسی است. در صورت کشف تمدن هوشمند فرازمینی، انسانها چگونه واکنش خواهند داد.

راهبردهای کشف حیات[ویرایش]

وقتی صحبت از کاوش حیات فرازمینی می‌شود دو حوزه بیش از همه جلب توجه می‌کند:

تلسکوپ فضایی کپلر ناسا در مارس سال ۲۰۰۹ با موفقیت به فضا پرتاب شد. این تلسکوپ سیارههای فرا خورشیدی را با دقت تحت نظر خواهد داشت.

داخل منظومه شمسی[ویرایش]

برای کاوش درون منظومه شمسی می‌توان فضاپیماهایی مجهز به دستگاه‌های پردازشگر که قابلیت اندازه‌گیری و آزمایش در سیاره مقصد را دارند راهی فضا کرد. گزینه دیگر سنجش از دور است، مثلاً نقشه برداری از توزیع گاز متان در اتمسفر مریخ که بوسیله سفینه‌های مدارگرد انجام می‌گیرد. این شیوه به ما امکان می‌دهد فقط بیوسفر فعال سطح سیاره هدف را با استفاده از سنجش گازها مطالعه کنیم. در مقابل رهیافت سنجش در محل (In Situ) امکان بررسی بیوسیگناتورهایی نظیر مولکول‌های خاص یا ایزوتوپ عناصر سازنده مولکول‌ها که لزوماً متعلق به سیستم‌های در حال حیات نیستند را نیز فراهم می‌کند و نیز از آنجایی که تشخیص یک بیومارکر به تنهایی نمی‌تواند دلیلی برای حضور حیات در حال یا گذشته سیاره‌ای باشد، بایستی مجموعه‌ای از این بیومارکرها بطور همزمان بررسی گردند. البته دانشمندان بر سر اینکه باید دنبال مواد آلی تشکیل دهنده حیات زمینی یا حداقل چیزی شبیه به آن باشیم یا نه، هنوز به توافق چندانی نرسیده‌اند. بسیاری از آنان اعتقاد دارند حیات سیارات دیگر الزامی برای شباهت داشتن به الگوهای آشنای زمینی ندارند و باید از این قید و بند رها شد. برخی دیگر معتقدند در حال حاضر ناچاریم تحقیقات خود را بر روی جستجوی سیارات و حیات زمین مانند متمرکز کنیم. - ماورای منظومه شمسی: به خاطر فاصله زیاد زمین تا مرز منظومه شمسی در حال حاضر نمی‌توان از گزینه ارسال سفینه برای بررسی وضعیت آنسوی منظومه شمسی استفاده کرد. بنابراین ناچاریم به اطلاعات بدست آمده از مشاهدات از راه دور بسنده کنیم. تا کنون بیش از ۲۰۰ سیاره خارج منظومه شمسی شناسایی شده است ولی اغلب آنها متفاوت از ان چیزی هستند که بتوان انتظار حضور حیات در آنها را داشت. ماموریت فضایی "داروین" نام پروژه‌ای است که توسط آژانس فضایی اروپا (ESA) با هدف تحقیق دربارهٔ اتمسفر سیارات خارج منظومه شمسی مثل میزان گاز ازن و پراکسی راه اندازی شده است. وظیفه اصلی داروین جستجوی منابع بزرگ اکسیژن مولکولی، ازن، آب، دی اکسید کربن و متان در این سیارات است. به نظر می‌رسد این پروژه با چالش‌های جدی مواجه خواهد شد. می دانیم درخشش یک ستاره بسیار بیشتر از درخشش سیاره اش است. این مطالعات می‌تواند با بکار گیری ابزار آلات حساس طیف‌سنجی که بتواند نور منحرف شده توسط سیاره دور را طوری آنالیز کند تا به ترکیب گازهای تشکیل دهنده اتمسفر پی ببرد به نتایج قابل قبولی نایل گردد. نکته کلیدی در اینجا اینست که این گازها در صورتی می‌توانند به مقادیر قابل تشخیص برسند که بطور مستمر توسط سیستم‌های زیستی باز تولید شوند. هر مخلوط گازی که در اتمسفر سیاره‌ای شروع به گسترش می‌کند نمی‌تواند بوسیله واکنش‌های غیر زنده تولید شوند بلکه حاکی از فعالیت‌های زیستی روی آن سیاره است. اگر گازها توسط این فعالیت‌ها بطور مستمری بازتولید نشوند بصورت معدنی جذب کانی‌های سیاره شده و از غلظت آن کاسته می‌شود

اختر زیست شناختی منظومه شمسی[ویرایش]

در حال حاضر منظومه شمسی جدی‌ترین حوزه کاوش برای حیات فرازمینی است. کما اینکه اطلاعات ارزشمندی از سیارات همسایه خود داریم. این مسئله مرهون فاصله نسبتاً نزدیک ما با این سیارات است که می‌توانیم با شیوه‌های کنونی کاوش در فضا، نمونه‌هایی از این سیارات را به زمین آورده یا آزمایشگاه‌های سیار خود را به آنجا اعزام کنیم. با اینکه ۴۰ سال از اولین قدم انسان بر روی ماه می‌گذرد، اما هنوز نتوانسته‌ایم پای بر روی مریخ بگذاریم. به نظر می‌رسد وقوع این رویداد دست کم ۳۰ سال دیگر خواهد بود. بیشتر اجرام منظومه شمسی در منطقه خارج از کمربند حیات قرار گرفته‌اند (کمربند حیات منطقه‌ای از منظومه شمسی است که بدلیل فاصله مناسب با خورشید دمای متعادلی داشته و آب در آنجا می‌تواند به شکل مایع باقی بماند. از اینرو حیات در این مناطق می‌تواند تشکیل و تداوم یابد. زمین و مریخ در کمربند حیات قرار دارند.). مثلاً عطارد آنقدر به خورشید نزدیک است که بیشتر به یک سیب زمینی برشته شده می‌ماند تا سیاره‌ای قابل زندگی. دمای سطح عطارد از ۱۸۰- درجه سانتیگراد در کف دهانه‌های آتشفشانی در قطب‌ها، تا حدود ۴۰۰ درجه در استوا متغیر است. همچنین این سیاره هیچ اتمسفری ندارد به این دلایل انتظار وجود حیات در آن کاملاً بیهوده خواهد بود.

زهره (ونوس)[ویرایش]

زهره شبیه‌ترین سیاره به زمین در منظومه شمسی است. این سیاره را خواهر زمین نام نهاده‌اند، دست کم به خاطر اندازه یکسان آن دو. در گذشته‌های دور شرایطی در سطح این سیاره برقرار بوده که شباهت زیادی به محیط امروزی زمین داشته است. ولی اکنون این سیاره به علت شرایط گلخانه‌ای زیادی که در اتمسفرش دارد وضعیت دشواری برای زندگی پدید آورده. طوری که دیگر گرمای سوزان ۴۶۰ درجه‌ای، باران‌های اسید سولفوریک، طوفان‌های غبار آلود و متراکم وجود هر گونه حیات سطح این سیاره را غیر محتمل می‌سازد.

ماه[ویرایش]

تصویر بر این است که ماه در نتیجه برخوردی میان یک زمین اولیه نیمه مذاب و یک جرم سیاره مانند به اندازه مریخ به وجود آمده باشد. نمونه‌های بدست آمده از ماموریت‌های فضایی آپولو و لونا(Luna) هیچ اثری از زندگی و ترکیبی آلی در سطح ماه نشان نمی‌دهند. برخورد UVخشک و تشعشعات یونیزان خورشیدی به سطح عریان و بدون محافظ کره ماه امکان تشکیل مولکول هلی آلی که زیر بنای حیات اند را نمی‌دهد. به هرحال وجود ماه در نزدیکی زمین و چرخش انتقالی آن در طول سالیان نقش مهمی در توسعه حیات در روی زمین داشته است. زمین تنها سیاره منظومه شمسی است که قمری به این بزرگی دارد (نسبت به اندازه زمین). این نسبت بزرگی باعث می‌شود محور چرخش وضعی زمین در انحراف ۵ر۲۳ درجه نسبتاً پایدار باشد که باعث بوجود آمدن آب و هوا ثابت و جریان‌های هوایی و آب اقیانوس‌ها در طول میلیون‌ها سال شده است.

مریخ[ویرایش]

این سیاره سرخ رنگ هدف اصلی ما برای یافتن حیات فرازمینی و آثار آن در منظومه شمسی است. به یاری دانشمندان و کاوشگران مستقر در مریخ شواهد قانع کننده‌ای بدست آمده مبنی بر اینکه مقادیر قابل توجهی آب بر روی این سیاره در دوران‌های گذشته وجود داشته است. ولی ما هنوز بطور دقیق نمی دانیم آب چه مدت در سطح این سیاره وجو داشته. یا اینکه احتمال دارد هنوز در زیر لایه‌های سطحی آب مایع در جریان باشد. بر اساس شواهد ریخت‌شناسی در دوران اولیه، مریخ اتمسفر متراکمی داشته است. ولی به علت اندازه کوچکترش در مقایسه با زمین و گرانش ضعیف تر، بادهای خورشیدی گازهای آن را به فضا پراکنده و فقط جو رقیقی از CO۲ غنی شده برجای مانده است. دوسفینه وایکینگ (Viking) که در سال ۱۹۷۶ روی ماه فرود آمدند مجهز به ابزار شناسایی حیات و طیف‌سنج گازی بودند. این تجهیزات برای تحلیل خاک پیرامون سفینه‌ها مورد استفاده قرار گرفتند اما در شناسایی مواد آلی دچار مشکل شدند. این یافته‌ها شواهدی از نبود حیات در سطح این سیاره بود. ولی با کشف منطقه حاوی حیات در ۱۰۰ متری زیر زمین در معادن طلای آفریقای جنوبی گمانه زنی‌هایی دربارهٔ امکان وجود چنین جایگاه‌های رشد میکروبی در لایه‌های زیرین آغاز شده است.

از سوی دیگر دانشمندان نگرانند که کاوشهای انسانی در سیاره مریخ برای کشف حیات خود موجب اختلال در طبیعت این سیاره شود. برای مثال مریخ‌نورد کیوریاسیتی که در سال ۲۰۱۱ به سوی مریخ پرتاب شد، به محض فرود آمدن بر سطح این سیاره شروع به حرکت خواهد کرد. حرکت سریع این مریخ‌نورد می‌تواند آلودگی‌های زیستی احتمالی مانند انواع باکتری، ویروس یا میکروب که به چرخ‌های آن چسبیده‌اند را به سطح مریخ منتقل و با گذر چرخ‌های عقبی از روی آنها، به اعماق خاک مریخ نفوذ کنند و آغازی شود برای یک نوع خاص از زندگی مریخی.

وجود اقیانوس در گذشته مریخ[ویرایش]

جدیدترین تحقیقات نشان می‌دهد که تغییرات ارتفاع خطوط ساحلی مریخ در اثر جابه‌جایی محور چرخش مریخ است. به این صورت که احتمالا این قطب‌ها بین ۲ تا ۳ میلیارد سال پیش حدود ۳۰۰۰ کیلومتر روی سطح این سیاره جابه‌جا شده‌اند. این جابه‌جایی قطب‌ها موجب شده است که خطوط ساحلی ارتفاعی متغیر داشته باشند.

حتی اگر از زمین به مریخ نگاه کنید دشتی که قطب شمال آن را احاطه کرده است همانند ناحیه‌ای انباشته از رسوبات ته‌نشین شده در بستر یک اقیانوس است. در دههٔ ۱۹۸۰ تصاویر فضاپیمای وایکینگ چیزی شبیه دو خط ساحلی بسیار قدیمی را در نزدیکی قطب شمال مریخ نشان داد که طول آن‌ها چند هزار کیلومتربود و عوارضی مشابه با عوارض نواحی ساحلی زمین داشتند. این خطوط ساحلی با نام‌های عربستان(Arabia) و دوترونیلوس(Deuteronilus) مربوط به ۲ تا ۴ میلیارد سال قبل هستند.

در دههٔ ۱۹۹۰ نقشه بردار سراسری مریخ متعلق به ناسا سطح مریخ را با دقت ۳۰۰ متر نقشه برداری کرد و متوجه شد که ارتفاع این خطوط ساحلی در نقاط مختلف تا چندین کیلومتر تغییر می‌کند و آن‌ها همانند موجی‌هایی با طول چند هزار کیلومتر هستند. در زمین ارتفاع این خطوط ساحلی تقریبا ثابت است، به همین دلیل بسیاری از کارشناسان نظریه وجود اقیانوس‌ها در مریخ را رد کردند.

دانشمندان دانشگاه برکلی به تازگی متوجه شده‌اند که تغییرات ارتفاع خطوط ساحلی مریخ در اثر جابه‌جایی محور چرخش مریخ است. به این صورت که احتمالا این قطب‌ها بین ۲ تا ۳ میلیارد سال پیش حدود ۳۰۰۰ کیلومتر روی سطح این سیاره جابه‌جا شده‌اند. این جابه‌جایی قطب‌ها موجب شده است که خطوط ساحلی ارتفاعی متغییر داشته باشند.

«میکائیل مانگا» (Michael Manga) استاد دانشگاه برکلی و یکی از رهبران این تحقیق می‌گوید: `جابه جایی محور چرخش مریخ باعث تغییر شکل سطح سیاره و به وجود آمدن پستی و بلندی در خطوط ساحلی شده است`. «تیلور پرون» (Taylor Perron) محقق اصلی این تحقیق می‌گوید: `در سیاراتی مانند زمین و مریخ که پوستهٔ خارجی انعطاف‌پذیری دارند، سطح جامد رفتاری متفاوت با سطح اقیانوس دارد که باعث تغییرات غیریکسان سطح می‌شود`.

محاسبات پرون نشان می‌دهد که مقاومت پوستهٔ ارتجاعی مریخ باعث تغییرات ارتفاع این خطوط ساحلی شده است. پستی و بلندی‌های عربستان و دوترونیلوس به ترتیب ۲٫۵ و ۰٫۷ کیلومتر تغییرات ارتفاع دارند.

«مارک ریچاردز»(Mark Richards) یکی از محققان می‌گوید: `نتیجهٔ تیلور بسیار زیباست. توضیح دادن سبب وجود این پستی و بلندی‌ها با یک مدل ساده هیجان انگیز است. من هرگز نمی‌توانستم چنین چیزی را از قبل پیش بینی کنم`.

وی می‌افزاید:` این مدل تایید می‌کند که مریخ در گذشته اقیانوس داشته است`.

محاسبات پرون، مانگا، ریچاردز و همکارانشان نشان داد که دو خط ساحلی عربستان و دوترونیلوس در اثر جابه جایی‌های ۵۰ و ۲۰ درجه‌ای قطبین سیاره به وجود آمده‌اند. فرضیه مانگا می‌گوید که علت جابه جایی ۵۰ درجه‌ای، وجود اقیانوسی بزرگ در یکی از قطبین مریخ است. اگر جاری شدن آب باعث پر شدن قطب شمال سیاره شده باشد، جرم این مقدار آب قادر بوده است محور چرخش را ۵۰ درجه به سمت جنوب حرکت دهد و سپس با ناپدید شدن آب، محور دوباره به جای اصلی خود بازگشته است.

مانگا می‌گوید که منبع ناشناختهٔ آب احتمالا سیل بسیار عظیمی در این سیاره به وجود آورده است که گواه آن وجود دره‌های بسیار بزرگ در دشت «تارسیس» مریخ است. سپس یا آب بخار شده یا به لایه‌های زیرین نفوذ کرده است و نزدیکی سطح به صورت یخ زده و در اعماق به صورت مایع وجود دارد.

وجود چنین اقیانوسی در گذشتهٔ مریخ هدف مناسبی برای مطالعات بعدی کاوش گرهای مریخی است.

منابع: www.spaceflightnow.com

www.spaceref.com[۱]

مشتری و زحل[ویرایش]

جو سیارات غول پیکر یعنی مشتری و زحل (و نیز اورانوس) در اصل مرکب از هیدروژن، هلیوم به همراه متان و مقدار کمتری از آمونیاک است. از نظر اخترزیست‌شناسی این سیارات اهمیت چندانی برای ما ندارند چرا که فاقد سطوج جامد هستند. ولی در عوض قمرهای آنان در کانون توجه اخترزیست شناسان قرار دارد.

قمرهای مشتری[ویرایش]

قمرهای بزرگترین سیاره منظومه شمسی به دقت توسط فضاپیمای گالیله مورد بررسی قرار گرفته است. داده‌های مغناطیس سنجی حاکی از احتمال وجود اقیانوس آب مایع در زیر قشر منجمد قمر اروپا است. حالت مشابه آن ممکن است در قمرهای گانیمد(Ganymede) و کالیستو(Callisto) نیز وجود داشته باشد. اگر چه فواصل زیاد آنها از خورشید دریافت پرتوهای کافی از خورشید را ناممکن می‌سازد و آب نمی‌تواند در سطح آن به شکل مایع یافت شود، ولی نیروهای حاصل از چرخش وضعی و جاذبه مشتری منابع گرمایی اندکی ایجاد می‌کند که می‌تواند برای ذوب برخی یخها کافی باشد. البته با فرض اینکه آب مایع در قمر اروپا وجود داشته باشد، شانس تشکیل حیات و توسعه آن در این اقیانوس‌های زیرین بسیار اندک است زیرا هیچ منبع ترکیبات آلی در آن شناخته نشده است. با وجود اینکه احتمال می‌رود برخی مواد آلی در تماس با سطح قمر متراکم شوند ولی نقل و انتقال این مواد توسط صفحات یخی بسیار بعید بنظر می‌رسد. البته به رغم این تردیدهای ماٌیوس کننده قمر اروپا هنوز در فهرست تحقیقات آتی حیات فرازمینی قرار دارد. گزینه‌هایی مثل رصدهای راداری از روی زمین و اعزام کاوشگرها برای مطالعه این قمر مطرح است.

قمرهای زحل[ویرایش]

از زمانی که Gerhard Kuiper در سال ۱۹۴۴ گاز متان را در اتمسفر تایتان مشاهده کرد تصور بر این بوده که این قمر برای زندگی مناسب باشد. چرا که متان یکی از اصلی‌ترین محصول فرایندهای زیستی محسوب می‌شود. تایتان اتمسفر متراکمی از نیتروژن و سرشار از مواد آلی در فاز گازی خود دارد. این قمر لابراتواری طبیعی برای بررسی تشکیل مولکول‌های آلی پیچیده در مقیاس بزرگ در طول دوره‌های طولانی زمین‌شناسی بوده است. با وجود دمای پائین سطح تایتان که بسیار کمتر از دمای زمین می‌باشد آب مایع اصلاً در آن وجود ندارد. ولی این قمر شرایط نسبتاً متعادل و پایداری را برای تولیدات فرآیندهای حیاتی و فیزیکوشیمیایی که تشکیل دهنده شیمی آلی سیاره‌ای است فراهم می‌سازد. اما هیچ کدام از کاوشگران کاسینی و هایژن (Huygen) اثری از حیات بر روی این قمر پیدا نکرده‌اند. اخیراً قمر دیگری از زحل بنام انکلادوس (Enceladus) توجه دانشمندان را به خود جلب کرده است. این قمر از هنگامی مورد توجه قرار گرفته است که ناسا از کشف آبفشان‌های عظیمی بر روی این قمر توسط فضاپیمای کاسینی خبر داد. فوران‌های بزرگ مواد یخی در بالای قطب جنوب این قمر کیلومترها امتداد یافته است. عقیده بر این است که جریان‌های حاصل از آبفشان‌ها از منابع انباشته شده زیرین طغیان نموده‌اند و احتمال دارد در زیر آنها آب مایع در جریان باشد. این در حالی است که دمای پوشش یخی در سطح این قمر به ۲۰۰- درجه سانتیگراد می‌رسد.

سیارات حاشیه نشین منظومه شمسی[ویرایش]

غول‌های یخی، اورانوس و نپتون به همراه پلوتو و کایپر(Kuiper) از خورشید بسیار دورند. دمای بسیار پائین آنها هیچ شانسی برای وجود آب مایع و حیات باقی نمی‌گذارد. ولی کاوش این سیارات برای افزایس دانسته هایمان از چگونگی تشکیل منظومه‌های سیاره‌ای بسیار حائز اهمیت است.

دنباله دارها[ویرایش]

دنباله دارها جزو اجرام کایپر یا قطعات غبارOort هستند که نیروی جاذبه سیارات خارجی آنها را به درون منظومه شمسی می کشاند و مدار آنها را دچار تغییر و تحول می‌سازند. دنباله دارها حاوی مقادیر زیادی آب هستند، اکنون ما می دانیم دو سوم هسته دنباله دار هالی از آب منجمد تشکیل شده است. بقیه آن موادی متشکل از سیلیکات‌ها و مواد آلی مثل فرمالدهید، متانول و... است. فناوری‌های اخیر وجود مواد آلی دیگر مثل مثل آمونیاک، متان، استیلن حتی مولکول‌های پیچیده نظیر سینواستیلن را در هسته دنباله دارها اثبات کرده‌اند. با این حال ما تاکنون نتوانستیم ارزیابی مستقیمی از ترکیب هسته ستارگان دنباله دار انجام دهیم. ماٌموریت فضاپیمایRosetta متعلق به سازمان فضایی اروپا با سفینه Philae یکی از راهبردهایی است که با مطالعه دنباله دار ۶۷P/Churyumov-Gerosimenko در راه پرده برداشتن از اسرار این تکه یخ‌های سرگردان گام خواهد گذاشت. جستجوی برای یافتن دنیاهای جدید همواره از اساسی‌ترین کوشش‌های بشر بوده است. اختر زیست‌شناسی چیزی غیر از تداوم این تلاش در قالب‌های جدید و علم گرایانه نیست که مطمئناً می‌تواند ما را با ابعاد عمیق مفهوم زندگی روی سیاره منحصر بفردمان «زمین» بیش از پیش آشنا ساخته و ما را در کسب آگاهی از ارزش واقعی حیات در کائنات کمک کند نا از این سیاره زیبا و موجودات زنده آن بیشتر محافظت کنیم.

جستارهای وابسته[ویرایش]

منابع[ویرایش]

  • مجله آستروبیولوژی

منابع[ویرایش]

  • مشارکت‌کنندگان ویکی‌پدیا، «اخترزیست‌شناسی»، ویکی‌پدیای انگلیسی، دانشنامهٔ آزاد (بازیابی در ۲۰ ژانویه ۲۰۰۸).
جستجو در ویکی‌انبار در ویکی‌انبار پرونده‌هایی دربارهٔ اخترزیست‌شناسی موجود است.

Nucleic acids may not be the only biomolecules in the Universe capable of coding for life processes.[1]

Astrobiology is the study of the origin, evolution, distribution, and future of life in the universe: extraterrestrial life and life on Earth. This interdisciplinary field encompasses the search for habitable environments in our Solar System and habitable planets outside our Solar System, the search for evidence of prebiotic chemistry, laboratory and field research into the origins and early evolution of life on Earth, and studies of the potential for life to adapt to challenges on Earth and in outer space.[2] Astrobiology addresses the question of whether life exists beyond Earth, and how humans can detect it if it does.[3] (The term exobiology is similar but more specific — it covers the search for life beyond Earth, and the effects of extraterrestrial environments on living things.)[4]

Astrobiology makes use of physics, chemistry, astronomy, biology, molecular biology, ecology, planetary science, geography, and geology to investigate the possibility of life on other worlds and help recognize biospheres that might be different from the biosphere on Earth.[5][6] Astrobiology concerns itself with interpretation of existing scientific data; given more detailed and reliable data from other parts of the universe, the roots of astrobiology itself—physics, chemistry and biology—may have their theoretical bases challenged. Although speculation is entertained to give context, astrobiology concerns itself primarily with hypotheses that fit firmly into existing scientific theories.

Earth is the only place in the universe known to harbor life.[7][8] However, recent advances in planetary science have changed fundamental assumptions about the possibility of life in the universe, raising the estimates of habitable zones around other stars,[9][10] along with the discovery of hundreds of extrasolar planets and new insights into the extreme habitats here on Earth, suggesting that there may be many more habitable places in the universe than science considered possible until very recently. On 4 November 2013, astronomers reported, based on Kepler space mission data, that there could be as many as 40 billion Earth-sized planets orbiting in the habitable zones of sun-like stars and red dwarf stars within the Milky Way Galaxy.[11][12] 11 billion of these estimated planets may be orbiting sun-like stars.[13] The nearest such planet may be 12 light-years away, according to the scientists.[11][12]

It has been proposed that viruses are likely to be encountered on other life-bearing planets.[14] Efforts to discover current or past life on Mars, is an active area of research. On 24 January 2014, NASA reported that current studies on the planet Mars by the Curiosity and Opportunity rovers will now be searching for evidence of ancient life, including a biosphere based on autotrophic, chemotrophic and/or chemolithoautotrophic microorganisms, as well as ancient water, including fluvio-lacustrine environments (plains related to ancient rivers or lakes) that may have been habitable.[15][16][17][18] The search for evidence of habitability, taphonomy (related to fossils), and organic carbon on the planet Mars is now a primary NASA objective.[15]

Overview

It is not known whether life elsewhere in the universe would utilize cell structures like those found on Earth. (Chloroplasts within plant cells shown here.)[19]
The Martian meteorite ALH84001 shows microscopic formations that may have been created by life.

Astrobiology is etymologically derived from the Greek ἄστρον, astron, "constellation, star"; βίος, bios, "life"; and -λογία, -logia, study. The synonyms of astrobiology are diverse; however, the synonyms were structured in relation to the most important sciences implied in its development: astronomy and biology. A close synonym is exobiology from the Greek Έξω, "external"; Βίος, bios, "life"; and λογία, -logia, study. The term exobiology was first coined by molecular biologist Joshua Lederberg. Exobiology is considered to have a narrow scope limited to search of life external to earth, whereas subject area of astrobiology is wider and investigates the link between life and the universe, which includes the search for extraterrestrial life, but also includes the study of life on earth, its origin, evolution and limits. Exobiology as a term has tended to be replaced by astrobiology.

Another term used in the past is xenobiology, ("biology of the foreigners") a word used in 1954 by science fiction writer Robert Heinlein in his work The Star Beast.[20] The term xenobiology is now used in a more specialized sense, to mean "biology based on foreign chemistry", whether of extraterrestrial or terrestrial (possibly synthetic) origin. Since alternate chemistry analogs to some life-processes have been created in the laboratory, xenobiology is now considered as an extant subject.[21]

While it is an emerging and developing field, the question of whether life exists elsewhere in the universe is a verifiable hypothesis and thus a valid line of scientific inquiry. Though once considered outside the mainstream of scientific inquiry, astrobiology has become a formalized field of study. Planetary scientist David Grinspoon calls astrobiology a field of natural philosophy, grounding speculation on the unknown, in known scientific theory.[22] NASA's interest in exobiology first began with the development of the U.S. Space Program. In 1959, NASA funded its first exobiology project, and in 1960, NASA founded an Exobiology Program; Exobiology research is now one of four elements of NASA's current Astrobiology Program.[3][23] In 1971, NASA funded the Search for Extra-Terrestrial Intelligence (SETI) to search radio frequencies of the electromagnetic spectrum for signals being transmitted by extraterrestrial life outside the Solar System. NASA's Viking missions to Mars, launched in 1976, included three biology experiments designed to look for possible signs of present life on Mars. The Mars Pathfinder lander in 1997 carried a scientific payload intended for exopaleontology in the hopes of finding microbial fossils entombed in the rocks.[24]

In the 21st century, astrobiology is a focus of a growing number of NASA and European Space Agency Solar System exploration missions. The first European workshop on astrobiology took place in May 2001 in Italy,[25] and the outcome was the Aurora programme.[26] Currently, NASA hosts the NASA Astrobiology Institute and a growing number of universities in the United States (e.g., University of Arizona, Penn State University, Montana State University – Bozeman, University of Washington, and Arizona State University),[27] Britain (e.g., The University of Glamorgan, Buckingham University),[28] Canada, Ireland, and Australia (e.g., The University of New South Wales)[29] now offer graduate degree programs in astrobiology. The International Astronomical Union regularly organizes international conferences through its Bioastronomy Commission.[30]

Advancements in the fields of astrobiology, observational astronomy and discovery of large varieties of extremophiles with extraordinary capability to thrive in the harshest environments on Earth, have led to speculation that life may possibly be thriving on many of the extraterrestrial bodies in the universe. A particular focus of current astrobiology research is the search for life on Mars due to its proximity to Earth and geological history. There is a growing body of evidence to suggest that Mars has previously had a considerable amount of water on its surface, water being considered an essential precursor to the development of carbon-based life.[31]

Missions specifically designed to search for life include the Viking program and Beagle 2 probes, both directed to Mars. The Viking results were inconclusive,[32] and Beagle 2 failed to transmit from the surface and is assumed to have crashed.[33] A future mission with a strong astrobiology role would have been the Jupiter Icy Moons Orbiter, designed to study the frozen moons of Jupiter—some of which may have liquid water—had it not been cancelled. In late 2008, the Phoenix lander probed the environment for past and present planetary habitability of microbial life on Mars, and to research the history of water there.

In November 2011, NASA launched the Mars Science Laboratory (MSL) rover, nicknamed Curiosity, which landed on Mars at Gale Crater in August 2012.[34][35][36] Curiosity rover is currently probing the environment for past and present planetary habitability of microbial life on Mars. On 9 December 2013, NASA reported that, based on evidence from Curiosity studying Aeolis Palus, Gale Crater contained an ancient freshwater lake which could have been a hospitable environment for microbial life.[37][38]

The European Space Agency is currently collaborating with the Russian Federal Space Agency (Roscosmos) and developing the ExoMars astrobiology rover, which is to be launched in 2018.[39]

Methodology

Planetary habitability

When looking for life on other planets like the earth, some simplifying assumptions are useful to reduce the size of the task of the astrobiologist. One is to assume that the vast majority of life forms in our galaxy are based on carbon chemistries, as are all life forms on Earth.[40] Carbon is well known for the unusually wide variety of molecules that can be formed around it. Carbon is the fourth most abundant element in the universe and the energy required to make or break a bond is just at an appropriate level for building molecules which are not only stable, but also reactive. The fact that carbon atoms bond readily to other carbon atoms allows for the building of arbitrarily long and complex molecules.

The presence of liquid water is a useful assumption, as it is a common molecule and provides an excellent environment for the formation of complicated carbon-based molecules that could eventually lead to the emergence of life.[41] Some researchers posit environments of ammonia, or more likely, water-ammonia mixtures.[42]

A third assumption is to focus on sun-like stars. This comes from the idea of planetary habitability.[43] Very big stars have relatively short lifetimes, meaning that life would not likely have time to evolve on planets orbiting them. Very small stars provide so little heat and warmth that only planets in very close orbits around them would not be frozen solid, and in such close orbits these planets would be tidally "locked" to the star.[44] Without a thick atmosphere, one side of the planet would be perpetually baked and the other perpetually frozen. In 2005, the question was brought back to the attention of the scientific community, as the long lifetimes of red dwarfs could allow some biology on planets with thick atmospheres. This is significant, as red dwarfs are extremely common. (See Habitability of red dwarf systems).

It is estimated that 10% of the stars in our galaxy are sun-like; there are about a thousand such stars within 100 light-years of our Sun. These stars would be useful primary targets for interstellar listening. Since Earth is the only planet known to harbor life, there is no evident way to know if any of the simplifying assumptions are correct.

Communication attempts

The illustration on the Pioneer plaque

Research on communication with extraterrestrial intelligence (CETI) focuses on composing and deciphering messages that could theoretically be understood by another technological civilization. Communication attempts by humans have included broadcasting mathematical languages, pictorial systems such as the Arecibo message and computational approaches to detecting and deciphering 'natural' language communication. The SETI program, for example, uses both radio telescopes and optical telescopes to search for deliberate signals from extraterrestrial intelligence.

While some high-profile scientists, such as Carl Sagan, have advocated the transmission of messages,[45][46] scientist Stephen Hawking has warned against it, suggesting that aliens might simply raid Earth for its resources and then move on.[47]

Elements of astrobiology

Astronomy

Artist's impression of the extrasolar planet OGLE-2005-BLG-390Lb orbiting its star 20,000 light-years from Earth; this planet was discovered with gravitational microlensing.
The NASA Kepler mission, launched in March 2009, searches for extrasolar planets.

Most astronomy-related astrobiological research falls into the category of extrasolar planet (exoplanet) detection, the hypothesis being that if life arose on Earth, then it could also arise on other planets with similar characteristics. To that end, a number of instruments designed to detect Earth-sized exoplanets have been considered, most notably NASA's Terrestrial Planet Finder (TPF) and ESA's Darwin programs, both of which have been cancelled. Additionally, NASA has launched the Kepler mission in March 2009, and the French Space Agency has launched the COROT space mission in 2006.[48][49] There are also several less ambitious ground-based efforts underway. (See exoplanet).

The goal of these missions is not only to detect Earth-sized planets, but also to directly detect light from the planet so that it may be studied spectroscopically. By examining planetary spectra, it would be possible to determine the basic composition of an extrasolar planet's atmosphere and/or surface; given this knowledge, it may be possible to assess the likelihood of life being found on that planet. A NASA research group, the Virtual Planet Laboratory,[50] is using computer modeling to generate a wide variety of virtual planets to see what they would look like if viewed by TPF or Darwin. It is hoped that once these missions come online, their spectra can be cross-checked with these virtual planetary spectra for features that might indicate the presence of life. The photometry temporal variability of extrasolar planets may also provide clues to their surface and atmospheric properties.

An estimate for the number of planets with intelligent extraterrestrial life can be gleaned from the Drake equation, essentially an equation expressing the probability of intelligent life as the product of factors such as the fraction of planets that might be habitable and the fraction of planets on which life might arise:[51]

N = R^{*} ~ \times ~ f_{p} ~ \times ~ n_{e} ~ \times ~ f_{l} ~ \times ~ f_{i} ~ \times ~ f_{c} ~ \times ~ L

where:

  • N = The number of communicative civilizations
  • R* = The rate of formation of suitable stars (stars such as our Sun)
  • fp = The fraction of those stars with planets (current evidence indicates that planetary systems may be common for stars like the Sun)
  • ne = The number of Earth-sized worlds per planetary system
  • fl = The fraction of those Earth-sized planets where life actually develops
  • fi = The fraction of life sites where intelligence develops
  • fc = The fraction of communicative planets (those on which electromagnetic communications technology develops)
  • L = The "lifetime" of communicating civilizations

However, whilst the rationale behind the equation is sound, it is unlikely that the equation will be constrained to reasonable error limits any time soon. The first term, N, Number of Stars, is generally constrained within a few orders of magnitude. The second and third terms, fp, Stars with Planets and fe, Planets with Habitable Conditions, are being evaluated for the sun's neighborhood. The problem with the formula is that it is not usable to generate or support hypotheses because it contains units that can never be verified. Drake originally formulated the equation merely as an agenda for discussion at the Green Bank conference,[52] but some applications of the formula had been taken literally and related to simplistic or pseudoscientific arguments.[53] Another associated topic is the Fermi paradox, which suggests that if intelligent life is common in the universe, then there should be obvious signs of it. This is the purpose of projects like SETI, which tries to detect signs of radio transmissions from intelligent extraterrestrial civilizations.

Another active research area in astrobiology is planetary system formation. It has been suggested that the peculiarities of our Solar System (for example, the presence of Jupiter as a protective shield)[54] may have greatly increased the probability of intelligent life arising on our planet.[55][56] No firm conclusions have been reached so far.

Biology

Hydrothermal vents are able to support extremophile bacteria on Earth and may also support life in other parts of the cosmos.

Biology and chemistry, as opposed to physics, do not admit ideological contexts: either the biological phenomena are real, or they are abstract. Biologists cannot say that a process or phenomenon, by being mathematically possible, have to exist forcibly in the real nature. For biologists, the ground of speculations is well noticeable, and biologists specify what is speculative and what is not.[53]

Until the 1970s, life was believed to be entirely dependent on energy from the Sun. Plants on Earth's surface capture energy from sunlight to photosynthesize sugars from carbon dioxide and water, releasing oxygen in the process, and are then eaten by oxygen-respiring animals, passing their energy up the food chain. Even life in the ocean depths, where sunlight cannot reach, was believed to obtain its nourishment either from consuming organic detritus rained down from the surface waters or from eating animals that did.[57] A world's ability to support life was thought to depend on its access to sunlight. However, in 1977, during an exploratory dive to the Galapagos Rift in the deep-sea exploration submersible Alvin, scientists discovered colonies of giant tube worms, clams, crustaceans, mussels, and other assorted creatures clustered around undersea volcanic features known as black smokers.[57] These creatures thrive despite having no access to sunlight, and it was soon discovered that they comprise an entirely independent food chain. Instead of plants, the basis for this food chain is a form of bacterium that derives its energy from oxidization of reactive chemicals, such as hydrogen or hydrogen sulfide, that bubble up from the Earth's interior. This chemosynthesis revolutionized the study of biology by revealing that life need not be sun-dependent; it only requires water and an energy gradient in order to exist.

Extremophiles (organisms able to survive in extreme environments) are a core research element for astrobiologists. Such organisms include biota which are able to survive several kilometers below the ocean's surface near hydrothermal vents and microbes that thrive in highly acidic environments.[58] It is now known that extremophiles thrive in ice, boiling water, acid, the water core of nuclear reactors, salt crystals, toxic waste and in a range of other extreme habitats that were previously thought to be inhospitable for life.[59] It opened up a new avenue in astrobiology by massively expanding the number of possible extraterrestrial habitats. Characterization of these organisms—their environments and their evolutionary pathways—is considered a crucial component to understanding how life might evolve elsewhere in the universe. According to astrophysicist Dr. Steinn Sigurdsson, "There are viable bacterial spores that have been found that are 40 million years old on Earth - and we know they're very hardened to radiation."[60] Some organisms able to withstand exposure to the vacuum and radiation of space include the lichen fungi Rhizocarpon geographicum and Xanthoria elegans,[61] the bacterium Bacillus safensis,[62] Deinococcus radiodurans,[62] Bacillus subtilis,[62] yeast Saccharomyces cerevisiae,[62] seeds from Arabidopsis thaliana ('mouse-ear cress'),[62] as well as the invertebrate animal Tardigrade.[62] On 29 April 2013, French scientists, funded by NASA, reported that, during spaceflight, microbes (like Pseudomonas aeruginosa) seem to adapt to the space environment in ways "not observed on Earth" and can increase in "virulence".[63] On 27 June 2011, it was reported that a new E. coli bacterium was produced from an engineered DNA in which approximately 90% of its thymine was replaced with the synthetic building block 5-chlorouracil, a substance "toxic to other organisms".[64][65]

Jupiter's moon, Europa,[59][66][67][68][69][70] and Saturn's moon, Enceladus,[71][72] are now considered the most likely locations for extant extraterrestrial life in the solar system.

The origin of life, known as abiogenesis, distinct from the evolution of life, is another ongoing field of research. Oparin and Haldane postulated that the conditions on the early Earth were conducive to the formation of organic compounds from inorganic elements and thus to the formation of many of the chemicals common to all forms of life we see today. The study of this process, known as prebiotic chemistry, has made some progress, but it is still unclear whether or not life could have formed in such a manner on Earth. The alternative hypothesis of panspermia is that the first elements of life may have formed on another planet with even more favorable conditions (or even in interstellar space, asteroids, etc.) and then have been carried over to Earth by a variety of means. Somewhat related to such a hypothesis, NIH scientists reported studies that life began 9.7±2.5 billion years ago, billions of years before the Earth was formed, based on extrapolating the "genetic complexity of organisms" [from "major phylogenetic lineages"] to earlier times.[73][74] (also see Abiogenesis#Coenzyme world)

In October 2011, scientists found that the cosmic dust permeating the universe contains complex organic matter ("amorphous organic solids with a mixed aromatic-aliphatic structure") that could be created naturally, and rapidly, by stars.[75][76][77] As one of the scientists noted, "Coal and kerogen are products of life and it took a long time for them to form ... How do stars make such complicated organics under seemingly unfavorable conditions and [do] it so rapidly?"[75] Further, the scientist suggested that these compounds may have been related to the development of life on earth and said that, "If this is the case, life on Earth may have had an easier time getting started as these organics can serve as basic ingredients for life."[75] In September 2012, NASA scientists reported that polycyclic aromatic hydrocarbons (PAHs), subjected to interstellar medium (ISM) conditions, are transformed, through hydrogenation, oxygenation and hydroxylation, to more complex organics - "a step along the path toward amino acids and nucleotides, the raw materials of proteins and DNA, respectively".[78][79] Further, as a result of these transformations, the PAHs lose their spectroscopic signature which could be one of the reasons "for the lack of PAH detection in interstellar ice grains, particularly the outer regions of cold, dense clouds or the upper molecular layers of protoplanetary disks."[78][79]

On 29 August 2012, and in a world first, astronomers at Copenhagen University reported the detection of a specific sugar molecule, glycolaldehyde, in a distant star system. The molecule was found around the protostellar binary IRAS 16293-2422, which is located 400 light years from Earth.[80][81] Glycolaldehyde is needed to form ribonucleic acid, or RNA, which is similar in function to DNA. This finding suggests that complex organic molecules may form in stellar systems prior to the formation of planets, eventually arriving on young planets early in their formation.[82]

On 21 February 2014, NASA announced a greatly upgraded database for tracking polycyclic aromatic hydrocarbons (PAHs) in the universe. According to scientists, more than 20% of the carbon in the universe may be associated with PAHs, possible starting materials for the formation of life. PAHs seem to have been formed shortly after the Big Bang, are widespread throughout the universe, and are associated with new stars and exoplanets.[83]

Astroecology

Astroecology concerns the interactions of life with space environments and resources, in planets, asteroids and comets. On a larger scale, astroecology concerns resources for life about stars in the galaxy through the cosmological future. Astroecology attempts to quantify future life in space, addressing this area of astrobiology.

Experimental astroecology investigates resources in planetary soils, using actual space materials in meteorites.[84] The results suggest that Martian and carbonaceous chondrite materials can support bacteria, algae and plant (asparagus, potato) cultures, with high soil fertilities. The results support that life could have survived in early aqueous asteroids and on similar materials imported to Earth by dust, comets and meteorites, and that such asteroid materials can be used as soil for future space colonies.[84][85]

On the largest scale, cosmoecology concerns life in the universe over cosmological times. The main sources of energy may be red giant stars and white and red dwarf stars, sustaining life for 1020 years.[84][84][86] Astroecologists suggest that their mathematical models may quantify the immense potential amounts of future life in space, allowing a comparable expansion in biodiversity, potentially leading to diverse intelligent life-forms.[87]

Astrogeology

Astrogeology is a planetary science discipline concerned with the geology of the celestial bodies such as the planets and their moons, asteroids, comets, and meteorites. The information gathered by this discipline allows the measure of a planet's or a natural satellite's potential to develop and sustain life, or planetary habitability.

An additional discipline of astrogeology is geochemistry, which involves study of the chemical composition of the Earth and other planets, chemical processes and reactions that govern the composition of rocks and soils, the cycles of matter and energy and their interaction with the hydrosphere and the atmosphere of the planet. Specializations include cosmochemistry, biochemistry and organic geochemistry.

The fossil record provides the oldest known evidence for life on Earth.[88] By examining the fossil evidence, paleontologists are able to better understand the types of organisms that arose on the early Earth. Some regions on Earth, such as the Pilbara in Western Australia and the McMurdo Dry Valleys of Antarctica, are also considered to be geological analogs to regions of Mars, and as such, might be able to provide clues on how to search for past life on Mars.

Consistent with the above, the earliest evidence for life on Earth are graphite found to be biogenic in 3.7 billion-year-old metasedimentary rocks discovered in Western Greenland[89] and microbial mat fossils found in 3.48 billion-year-old sandstone discovered in Western Australia.[90][91] Nonetheless, several studies suggest that life on Earth may have started even earlier, as early as 4.25 billion years ago according to one study.[92][93][94]

Life in the Solar System

Europa, due to the ocean that exists under its icy surface, might host some form of microbial life.

People have long speculated about the possibility of life in settings other than Earth, however, speculation on the nature of life elsewhere often has paid little heed to constraints imposed by the nature of biochemistry.[95] The likelihood that life throughout the universe is probably carbon-based is encouraged by the fact that carbon is one of the most abundant of the higher elements. Only two of the natural atoms, carbon and silicon, are known to serve as the backbones of molecules sufficiently large to carry biological information. As the structural basis for life, one of carbon's important features is that unlike silicon it can readily engage in the formation of chemical bonds with many other atoms, thereby allowing for the chemical versatility required to conduct the reactions of biological metabolism and propagation.

The various organic functional groups, composed of hydrogen, oxygen, nitrogen, phosphorus, sulfur, and a host of metals, such as iron, magnesium, and zinc, provide the enormous diversity of chemical reactions necessarily catalyzed by a living organism. Silicon, in contrast, interacts with only a few other atoms, and the large silicon molecules are monotonous compared with the combinatorial universe of organic macromolecules.[53][95] Indeed, it seems likely that the basic building blocks of life anywhere will be similar to our own, in the generality if not in the detail.[95] Although terrestrial life and life that might arise independently of Earth are expected to use many similar, if not identical, building blocks, they also are expected to have some biochemical qualities that are unique. If life has had a comparable impact elsewhere in the solar system, the relative abundances of chemicals key for its survival - whatever they may be - could betray its presence. Whatever extraterrestrial life may be, its tendency to chemically alter its environment might just give it away.[96]

Thought on where in the Solar System life might occur was limited historically by the belief that life relies ultimately on light and warmth from the Sun and, therefore, is restricted to the surfaces of planets.[95] The three most likely candidates for life in the Solar System are the planet Mars, the Jovian moon Europa, and Saturn's moon Titan.[97][98][99][100][101] More recently, Saturn's moon Enceladus may be considered a likely candidate as well.[72][102] This speculation of likely candidates of life is primarily based on the fact that (in the cases of Mars and Europa) the planetary bodies may have liquid water, a molecule essential for life as we know it, for its use as a solvent in cells.[31]

Water on Mars is found in its polar ice caps, and newly carved gullies recently observed on Mars suggest that liquid water may exist, at least transiently, on the planet's surface.[103][104] At the Martian low temperatures and low pressure, liquid water is likely to be highly saline.[105] As for Europa, liquid water likely exists beneath the moon's icy outer crust.[67][97][98] This water may be warmed to a liquid state by volcanic vents on the ocean floor (an especially intriguing theory considering the various types of extremophiles that live near Earth's volcanic vents), but the primary source of heat is probably tidal heating.[106] On 11 December 2013, NASA reported the detection of "clay-like minerals" (specifically, phyllosilicates), often associated with organic materials, on the icy crust of Europa.[107] The presence of the minerals may have been the result of a collision with an asteroid or comet according to the scientists.[107]

Another planetary body that could potentially sustain extraterrestrial life is Saturn's largest moon, Titan.[101] Titan has been described as having conditions similar to those of early Earth.[108] On its surface, scientists have discovered the first liquid lakes outside Earth, but they seem to be composed of ethane and/or methane, not water.[109] After Cassini data was studied, it was reported on March 2008 that Titan may also have an underground ocean composed of liquid water and ammonia.[110] Additionally, Saturn's moon Enceladus may have an ocean below its icy surface[111] and, according to NASA scientists in May 2011, "is emerging as the most habitable spot beyond Earth in the Solar System for life as we know it".[72][102]

On 26 April 2012, scientists reported that lichen survived and showed remarkable results on the adaptation capacity of photosynthetic activity within the simulation time of 34 days under Martian conditions in the Mars Simulation Laboratory (MSL) maintained by the German Aerospace Center (DLR).[112][113] In June, 2012, scientists reported that measuring the ratio of hydrogen and methane levels on Mars may help determine the likelihood of life on Mars.[114][115] According to the scientists, "...low H2/CH4 ratios (less than approximately 40) indicate that life is likely present and active."[114] Other scientists have recently reported methods of detecting hydrogen and methane in extraterrestrial atmospheres.[116][117]

Rare Earth hypothesis

This hypothesis states that based on astrobiological findings, multi-cellular life forms found on Earth may actually be more of a rarity than scientists initially assumed. It provides a possible answer to the Fermi paradox which suggests, "If extraterrestrial aliens are common, why aren't they obvious?" It is apparently in opposition to the principle of mediocrity, assumed by famed astronomers Frank Drake, Carl Sagan, and others. The Principle of Mediocrity suggests that life on Earth is not exceptional, but rather that life is more than likely to be found on innumerable other worlds.

The anthropic principle states that fundamental laws of the universe work specifically in a way that life would be possible. The anthropic principle supports the Rare Earth Hypothesis by arguing the overall elements that are needed to support life on Earth are so fine-tuned that it is nearly impossible for another just like it to exist by random chance (note that these terms are used by scientists in a different way from the vernacular conception of them). However, Stephen Jay Gould compared the claim that the universe is fine-tuned for the benefit of our kind of life to saying that sausages were made long and narrow so that they could fit into modern hot dog buns, or saying that ships had been invented to house barnacles.[118][119]

Research

The systematic search for possible life outside Earth is a valid multidisciplinary scientific endeavor.[120] The University of Glamorgan, UK, started just such a degree in 2006,[28] and the American government funds the NASA Astrobiology Institute. However, characterization of non-Earth life is unsettled; hypotheses and predictions as to its existence and origin vary widely, but at the present, the development of theories to inform and support the exploratory search for life may be considered astrobiology's most concrete practical application.

Biologist Jack Cohen and mathematician Ian Stewart, amongst others, consider xenobiology separate from astrobiology. Cohen and Stewart stipulate that astrobiology is the search for Earth-like life outside our solar system and say that xenobiologists are concerned with the possibilities open to us once we consider that life need not be carbon-based or oxygen-breathing, so long as it has the defining characteristics of life. (See carbon chauvinism).

Research outcomes

Asteroid(s) may have transported life to Earth.

As of 2014, no evidence of extraterrestrial life has been identified. Examination of the Allan Hills 84001 meteorite, which was recovered in Antarctica in 1984 and believed to have originated from Mars, is thought by David McKay, Chief Scientist for Astrobiology at NASA's Johnson Space Center, as well as other scientists, to contain microfossils of extraterrestrial origin; this interpretation is controversial.[121][122][123]

Yamato 000593 is the second largest meteorite from Mars, and was found on Earth in 2000. At a microscopic level, spheres are found in the meteorite that are rich in carbon compared to surrounding areas that lack such spheres. The carbon-rich spheres may have been formed by biotic activity according to NASA scientists.[124][125][126]

On 5 March 2011, Richard B. Hoover, a scientist with the Marshall Space Flight Center, speculated on the finding of alleged microfossils similar to cyanobacteria in CI1 carbonaceous meteorites.[127][128] However, NASA formally distanced itself from Hoover's claim.[129][130][131] According to American astrophysicist Neil deGrasse Tyson: "At the moment, life on Earth is the only known life in the Universe, but there are compelling arguments to suggest we are not alone."[132]

Extreme environments on the Earth

On 17 March 2013, researchers reported data that suggested microbial life forms thrive in the Mariana Trench, the deepest spot on the Earth.[133][134] Other researchers reported related studies that microbes thrive inside rocks up to 1900 feet below the sea floor under 8500 feet of ocean off the coast of the northwestern United States.[133][135] According to one of the researchers,"You can find microbes everywhere — they're extremely adaptable to conditions, and survive wherever they are."[133]

Methane

In 2004, the spectral signature of methane was detected in the Martian atmosphere by both Earth-based telescopes as well as by the Mars Express probe. Because of solar radiation and cosmic radiation, methane is predicted to disappear from the Martian atmosphere within several years, so the gas must be actively replenished in order to maintain the present concentration.[136][137] The Mars Science Laboratory rover will perform precision measurements of oxygen and carbon isotope ratios in carbon dioxide (CO2) and methane (CH4) in the atmosphere of Mars in order to distinguish between a geochemical and a biological origin.[138][139][140]

Planetary systems

It is possible that some planets, like the gas giant Jupiter in our solar system, may have moons with solid surfaces or liquid oceans that are more hospitable. Most of the planets so far discovered outside our solar system are hot gas giants thought to be inhospitable to life, so it is not yet known whether our solar system, with a warm, rocky, metal-rich inner planet such as Earth, is of an aberrant composition. Improved detection methods and increased observing time will undoubtedly discover more planetary systems, and possibly some more like ours. For example, NASA's Kepler Mission seeks to discover Earth-sized planets around other stars by measuring minute changes in the star's light curve as the planet passes between the star and the spacecraft. Progress in infrared astronomy and submillimeter astronomy has revealed the constituents of other star systems. Infrared searches have detected belts of dust and asteroids around distant stars, underpinning the formation of planets.

Planetary habitability

Efforts to answer questions such as the abundance of potentially habitable planets in habitable zones and chemical precursors have had much success. Numerous extrasolar planets have been detected using the wobble method and transit method, showing that planets around other stars are more numerous than previously postulated. The first Earth-sized extrasolar planet to be discovered within its star's habitable zone is Gliese 581 c, which was found using radial velocity.[141]

Missions

Research into the environmental limits of life and the workings of extreme ecosystems is ongoing, enabling researchers to better predict what planetary environments might be most likely to harbor life. Missions such as the Phoenix lander, Mars Science Laboratory, ExoMars to Mars, and the Cassini probe to Saturn's moon Titan hope to further explore the possibilities of life on other planets in our solar system.

Viking program

Carl Sagan posing with a model of the Viking Lander.

The two Viking spacecraft each carried four types of biological experiments to the surface of Mars in the late 1970s. These were the only Mars landers to carry out experiments to look specifically for biosignatures of life on Mars. The landers used a robotic arm to put soil samples into sealed test containers on the craft. The two landers were identical, so the same tests were carried out at two places on Mars' surface; Viking 1 near the equator and Viking 2 further north.[142] The result was inconclusive,[143] and is still disputed by some scientists.[144][145][146][147]

Beagle 2

Replica of the 33.2 kg Beagle-2 lander
Mars Science Laboratory rover concept artwork

Beagle 2 was an unsuccessful British Mars lander that formed part of the European Space Agency's 2003 Mars Express mission. Its primary purpose was to search for signs of life on Mars, past or present. All contact with it was lost upon its entry into the atmosphere.[148]

EXPOSE

EXPOSE was a multi-user facility mounted in 2008 outside the International Space Station dedicated to astrobiology.[149][150] EXPOSE was developed by the European Space Agency (ESA) for long-term spaceflights that allowed to expose organic chemicals and biological samples to outer space for one and a half years in low Earth orbit.[151]

Mars Science Laboratory

The Mars Science Laboratory (MSL) mission landed a rover that is currently in operation on Mars.[152] It was launched 26 November 2011, and landed at Gale Crater on 6 August 2012.[36] Mission objectives are to help assess Mars' habitability and in doing so, determine whether Mars is or has ever been able to support life,[153] collect data for a future manned mission, study Martian geology, its climate, and further assess the role that water, an essential ingredient for life as we know it, played in forming minerals on Mars.

ExoMars

ExoMars rover model

ExoMars is a robotic mission to Mars to search for possible biosignatures of Martian life, past or present. This astrobiological mission is currently under development by the European Space Agency (ESA) with likely collaboration by the Russian Federal Space Agency (Roscosmos); it is planned for a 2018 launch.[154][155][156]

Mars 2020 rover mission

The 'Mars 2020 rover mission' is a concept under study by NASA with a possible launch in 2020. It is intended to investigate astrobiologically relevant environments on Mars, investigate its surface geological processes and history, including the assessment of its past habitability and potential for preservation of biosignatures within accessible geological materials.[157] The Science Definition Team is proposing the rover collect and package as many as 31 samples of rock cores and soil for a later mission to bring back for more definitive analysis in laboratories on Earth. The rover could make measurements and technology demonstrations to help designers of a human expedition understand any hazards posed by Martian dust and demonstrate how to collect carbon dioxide (CO2), which could be a resource for making oxygen (O2) and rocket fuel. Improved precision landing technology that enhances the scientific value of robotic missions also will be critical for eventual human exploration on the surface.[158][159]

Red Dragon

Red Dragon is a proposed concept for a low-cost Mars lander mission that would utilize a SpaceX Falcon Heavy launch vehicle, and a modified Dragon capsule to enter the Martian atmosphere. The lander's primary mission would be to search for evidence of life on Mars (biosignatures), past or present. The concept had been scheduled to propose for funding on 2012/2013 as a NASA Discovery mission, for launch in 2018.[160][161]

Icebreaker Life

Icebreaker Life is a lander mission that is being proposed for NASA's Discovery Program for the 2018 launch opportunity.[162] If selected and funded, the stationary lander would be a near copy of the successful 2008 Phoenix and it would carry an upgraded astrobiology scientific payload, including a 1 meter-long drill to sample ice-cemented ground in the northern plains to conduct a search for organic molecules and evidence of current or past life on Mars.[163][164] One of the key goals of the Icebreaker Life mission is to test the hypothesis that the ice-rich ground in the polar regions has significant concentrations of organics due to protection by the ice from oxidants and radiation.

Europa Clipper

Europa Clipper is a mission concept under study by NASA that would conduct detailed reconnaissance of Jupiter's moon Europa and would investigate whether the icy moon could harbor conditions suitable for life.[165][166] It would also aid in the selection of future landing sites.[167][168]

See also


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Bibliography

External links

Further reading

  • The Search For Life In The Universe, D. Goldsmith, T. Owen. Second edition. ISBN 0-201-56949-3 Addison-Wesley Publishing Company